Multi Pattern Condenser
Multi Pattern Condenser
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 Yeti Blue Microphone  US $99.00
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 Shure SLX24 Beta87 Handheld Wireless System US $675.00
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 AKG C441B XLS Professional Condenser Microphone C 441B Mic Recording Vocal Drum US $451.00
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 Soundelux E47 Condensor Microphone Bock U47 Low Serial US $3,800.00
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 AKG C414 B XLII Matched Stereo Pair US $1,195.00
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 Blue Mouse Condenser Microphone with Blue Shockmount US $899.00
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 NEW Blue Mouse Microphone US $900.00
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 Sennheiser EW112P G3 Wireless Lav Camera System G Band Zoom H4n Recorder US $699.00
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 CAD Audio 6000 Condenser Cable Professional Microphone US $125.00
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 CAD Trion 8000 Multi Pattern Studio Tube Condenser Mic w Shockmount Case US $149.99
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 SAMSON C03 MULTI PATTERN CONDENSER MICROPHONE MIC with CASE AND CABLE NR US $34.95
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 MXL STUDIO 1 USB MICROPHONE MIC NEW NR US $49.95
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 Samson C01U Pro USB Studio Condenser Microphone Plus FREE BONUS unique offer US $99.99
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 Sennheiser EW112P G3 Wireless Lav Camera System A Band Zoom H4n Recorder US $699.00
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 NEW CAD Trion 8000 Mic Power Supply Cable Case US $399.99
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 NR47 tube microphoneTelefunkenMullard similar U47 US $1,485.16
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 M Audio Solaris Condenser Cable Professional Microphone US $.99
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 NEW Behringer T 47 Studio Vacuum Tube Condenser Mic BUY IT NOW FREE SHIPPING US $169.88
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 Blue Yeti Pro USB condenser Microphone US $56.00
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 Samson Wireless Airline 77 Aerobics Headset System N5 US $215.99
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 ADK A 51TC TUBE CONDENSER MICROPHONE W WINDSCREEN DJ 8 POWER SUPPLY CASE US $99.00
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 AKG C414 XL II ST Stereo Matched Pair C 414 XL2 XLIIST PROAUDIOSTAR US $1,475.00
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 CAD GXL1200 GXL 1200 SMALL DIAPHRAGM CONDENSER PAIR BARELY USED US $74.99
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 Behringer T47 STUDIO CONDENSER MICROPHONE T 47 NEW US $129.99
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 CAD GXL3000 GXL 3000 STUDIO CONDENSER MICROPHONES PAIR BARELY USED US $129.99
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 AUDIO TECHNICA AE3000 INSTRUMENT CONDENSER MICROPHONE EXCELLENT US $149.95
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 KAM MC3 multi capsule studio condenser mic with 3 capsules case shock mount US $79.00
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 Audio Technica AT4050CM5 Condenser Cable Professional Microphone US $500.00
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 SE Electronics SE4400A Condenser Cable Microphone US $620.00
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 Sennheiser MKH 416 Short Shotgun Interference Tube Mic w Zoom H4n XLR Cable US $999.95
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 CAD e300 Multi Pattern Condenser Microphone Mic 300 US $199.00
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 Audio Technica Artist Elite AE3000 Condenser Professional Microphone US $140.00
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 Shure SLX14 HS 06 6 Pack Wireless Microphone Earset System US $3,299.99
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 NEW Audio Technica AT2050 Multi Pattern Condenser Microphone US $159.00
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 Carvin CM87S condenser Microphone US $50.00
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 Samson Airline Micro Wireless Camera Lav Mic SystemN6 Band Zoom H4n Recorder US $449.00
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 DELUXE Samson CO3U Podcast PAK KIT USB C03U Mic NEW US $169.95
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 ADK TC Tube Microphone Condenser Large Diaphragm Fixed Cardiod Open Box US $400.00
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 Neumann TLM170R Cable Professional Microphone US $2,500.00
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 APEX 460 apex460 authorized dealer PROAUDIOSTAR US $209.00
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 Shure PGX24 SM86 H6 Wireless Mic System US $399.00
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 Rode Stereo VideoMic Pro Camera Microphone for Video Canon and Nikon DSLR US $299.00
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 AKG C414 XLS Large Diaphragm Condenser Recording C414 Studio Microphone New US $999.00
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 Audio Technica AT4050 AT 4050 Condenser Mic w Auralex Mudguard US $699.01
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 Audio Technica AT2050 Condenser Microphone w Mic Stand XLR Cable Pop Filter US $229.00
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 Sennheiser EW122P G3 EW122 P Wireless Lav Mic G Band w Zoom H4n US $699.00
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 822B630 UHF Dual Mini Earhook Headset Wireless Microphone System US $289.00
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 Samson Airline 77 Wireless Aerobics Headset Mic N6 FREE NEXT DAY AIR US $299.00
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 TASCAM TM ST1 Stereo Condenser Microphone US $29.99
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 Behringer T 47 Vacuum Tube Condenser Studio Mic Large Diaphragm Condenser Mic US $138.75
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Blue Reactor Multi Pattern Condenser Microphone $499 The Blue multi-pattern Reactor pushes the envelope of modern microphone design and performance while making multiple mic setups more accessible. Reactor fuses an innovative pattern selection method with a swiveling capsule head for perfect positioning, and features Blue's premium condenser capsule, fully discreet Class A solid state components, and proprietary preamp for simple live switching between patterns (Cardioid, Omni or Figure-8). To facilitate use in multiple mic setups (like Mid/Side, X-Y), Reactor's capsule head rotates a range of 90 degrees for perfect positioning in tight spaces and easy pattern adjustability. Reactor's recording pattern selection is both intuitive and stylish, featuring LED backlighting on the pattern indicators and a magnifying element that compliments its forward-looking design.Large-diaphragm premium condenser capsuleThree recording patterns: cardioid, omnidirectional, bidirectional (figure-8)Swivel head allows flexible placement and multi-mic positioning (like mid/side, X-Y)Unique selection method with magnifier for easy toggleFully discreet, Class A solid stste componentsLED backlit pattern selectionSimple pop filter selectionIncludes: custom metal case, shockmount, and pop filter |
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Used Blue Reactor Multi Pattern Condenser Microphone $454.09 The Blue multi-pattern Reactor pushes the envelope of modern microphone design and performance while making multiple mic setups more accessible. Reactor fuses an innovative pattern selection method with a swiveling capsule head for perfect positioning, and features Blue's premium condenser capsule, fully discreet Class A solid state components, and proprietary preamp for simple live switching between patterns (Cardioid, Omni or Figure-8). To facilitate use in multiple mic setups (like Mid/Side, X-Y), Reactor's capsule head rotates a range of 90 degrees for perfect positioning in tight spaces and easy pattern adjustability. Reactor's recording pattern selection is both intuitive and stylish, featuring LED backlighting on the pattern indicators and a magnifying element that compliments its forward-looking design.Large-diaphragm premium condenser capsuleThree recording patterns: cardioid, omnidirectional, bidirectional (figure-8)Swivel head allows flexible placement and multi-mic positioning (like mid/side, X-Y)Unique selection method with magnifier for easy toggleFully discreet, Class A solid stste componentsLED backlit pattern selectionSimple pop filter selectionIncludes: custom metal case, shockmount, and pop filter |
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Blue Reactor Multi Pattern Condenser Mic $499 The Blue multi-pattern Reactor pushes the envelope of modern microphone design and performance while making multiple mic setups more accessible. Reactor fuses an innovative pattern selection method with a swiveling capsule head for perfect positioning, and features Blue's premium condenser capsule, fully discreet Class A solid state components, and proprietary preamp for simple live switching between patterns (Cardioid, Omni or Figure-8). To facilitate use in multiple mic setups (like Mid/Side, X-Y), Reactor's capsule head rotates a range of 90 degrees for perfect positioning in tight spaces and easy pattern adjustability. Reactor's recording pattern selection is both intuitive and stylish, featuring LED backlighting on the pattern indicators and a magnifying element that compliments its forward-looking design. |
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Cad E300 Multi-Pattern Condenser Microphone $299.99 The CAD e300 is a Multi-Pattern Condenser Microphone that captures transparent, airy uppers and mids, coupled with a rich, silky smooth low end. Combining lightning-fast transient response and pinpoint precision with an enormous upfront presence, the e300 offers uparalleled performance from critical studio tracking scenarios to live reinforcement. The 1.1" 24K gold-sputtered dual-diaphragm condenser capsule is hand dampened for consistent frequency response. A hi-pass filter features 6dB octave @ 80Hz, and a 20dB non-capacitive pad. The stainless/brass triple stage pop/EMI filter delivers unmatched ballistic stability, with high SPL characteristics and plosives control. Sophisticated laser trimmed op-amp circuitry provides increased management of fast transient response. Frequency response of 10Hz-20 kHz. Requires phantom power.Multi-pattern condenser microphone 1.1" 24K gold-sputtered dual-diaphragm capsule Selectable patterns include cardioid, omni, and figure 8 Hi-pass filter features 6dB octave @ 80Hz 20dB non-capacitive pad Transparent, airy uppers and mids Rich, smooth low end |
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CAD e300 Multi-Pattern Condenser Microphone $224.99 The CAD e300 is a Multi-Pattern Condenser Microphone that captures transparent, airy uppers and mids, coupled with a rich, silky smooth low end. Combining lightning-fast transient response and pinpoint precision with an enormous upfront presence, the e300 offers uparalleled performance from critical studio tracking scenarios to live reinforcement. The 1.1" 24K gold-sputtered dual-diaphragm condenser capsule is hand dampened for consistent frequency response. A hi-pass filter features 6dB octave @ 80Hz, and a 20dB non-capacitive pad. The stainless/brass triple stage pop/EMI filter delivers unmatched ballistic stability, with high SPL characteristics and plosives control. Sophisticated laser trimmed op-amp circuitry provides increased management of fast transient response. Frequency response of 10Hz-20 kHz. Requires phantom power. |
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Audio-Technica At4050 Multi-Pattern Condenser Microphone $699 Meet the Audio-Technica AT4050, a multi-pattern studio condenser microphone that captures every nuance. With 3 switchable polar patterns, the large-diaphragm Audio-Technica AT4050 exhibits a remarkable combination of qualities: high-SPL capability with transparent and airy uppers/mids complemented by rich low-end qualities. Its dual large diaphragms are gold-vaporized and aged for consistent, outstanding performance. A precision-machined, nickel-plated brass acoustic element baffle provides rock-solid element stability and exceptional sensitivity. The AT4050 is an ideal microphone for studio use and live sound productions with vocals, piano, strings, drum overheads, guitar amps, and more. Transparent uppers/mids balanced by rich low-end qualities combine with advanced acoustic engineering for extensive performance capabilities and highest quality Dual-diaphragm capsule design maintains precise polar pattern definition across the full frequency range of the microphone The 2-micron-thick, vapor-deposited gold diaphragms undergo a 5-step aging process so that the optimum characteristics achieved remain constant over years of use Transformerless circuitry virtually eliminates low-frequency distortion and provides superior correlation of high-speed transients Open acoustical environment of the symmetrical housing assembly minimizes unwanted internal reflections State-of-the-art surface-mount electronics ensure compliance with A-T's stringent consistency and reliability standards Requires phantom power.Dual large gold diaphram capsule 3 switchable polar patterns: omni, cardioid, figure-8 Transformerless circuitry virtually eliminates low-frequency distortion and provides superior correlation of high-speed transients State-of-the-art surface-mount electronics ensure compliance with A-T's stringent consistency and reliability standards Switchable 80Hz hi-pass filter and 10dB pad Custom shock mount provides superior isolation |
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Audio-Technica At4047mp Multi-Pattern Condenser Microphone $849 The multi-pattern Audio-Technica AT4047MP Condenser Microphone delivers vintage sound while offering selectable omnidirectional, cardioid, and figure-8 polar patterns. The AT4047MP microphone's transformer-coupled output and specially tuned element provide sonic characteristics reminiscent of early F.E.T. studio microphone designs. With a wide dynamic range, incredibly low self-noise and high SPL capability, the versatile Audio Technica AT4047MP microphone excels on vocals, strings, acoustic guitar, instrument ensembles, small vocal groups, and voiceovers.Three switchable polar patterns: cardioid, omnidirectional, figure-of-eight Engineered to meet the critical acoustic requirements of professional recording, broadcast, and sound reinforcement Transformer-coupled output and specially tuned element provide sonic characteristics reminiscent of early F.E.T. studio microphone designs Exceptionally low self-noise, wide dynamic range and high SPL capability Dual-diaphragm capsule design maintains precise polar pattern definition across the full frequency range of the microphone Precision-machined, nickel-plated brass, acoustic element baffle provides enhanced element stability and optimal sensitivity Vintage silver-matte finish on microphone and shock mount Open acoustical environment of the symmetrical housing assembly minimizes unwanted internal reflections Custom shock mount provides superior isolation Integral 80Hz high-pass filter switch and 10dB pad switch Certified by the METAlliance (Music Engineering and Technology Alliance) |
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MXL 4000XL Multi-Pattern FET Studio Condenser Microphone $399.99 The MXL 4000XL is a multi-pattern condenser microphone with a large 32mm dual diaphragm capsule. The latest incarnation of the MXL 4000, its large-sized capsule brings a bolder, brighter, and more open sound. The 4000XL uses hand-selected internal components to create a sound that enhances both vocal and instrument performances. This microphone includes a shockmount and wooden storage case. |
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Mxl 4000Xl Multi-Pattern Fet Studio Condenser Microphone $249.99 The MXL 4000XL is a multi-pattern condenser microphone with a large 32mm dual diaphragm capsule. The latest incarnation of the MXL 4000, its large-sized capsule brings a bolder, brighter, and more open sound. The 4000XL uses hand-selected internal components to create a sound that enhances both vocal and instrument performances. This microphone includes a shockmount and wooden storage case.Enhances both vocal and instrumentLarge capsule condensers reveal very subtle sonic details Multiple polar patterns: cardioid, figure 8, omni-directional Includes a shockmount and wooden storage case. |
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Used Mxl 4000Xl Multi-Pattern Fet Studio Condenser Microphone $227.49 The MXL 4000XL is a multi-pattern condenser microphone with a large 32mm dual diaphragm capsule. The latest incarnation of the MXL 4000, its large-sized capsule brings a bolder, brighter, and more open sound. The 4000XL uses hand-selected internal components to create a sound that enhances both vocal and instrument performances. This microphone includes a shockmount and wooden storage case.Enhances both vocal and instrumentLarge capsule condensers reveal very subtle sonic details Multiple polar patterns: cardioid, figure 8, omni-directional Includes a shockmount and wooden storage case. |
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Audio-Technica At2050 Multi-Pattern Large Diaphragm Condenser Microphone $229 The versatile Audio-Technica AT2050 is a multi-pattern large diaphragm condenser microphone that provides consistent, superior performance. The AT2020 mic offers you switchable cardioid, omnidirectional and figure-eight polar pattern settings. The AT2050 mic's dual large diaphragms are gold-vaporized and aged to achieve optimum characteristics over years of use. Equipped with a switchable 80 Hz high-pass filter and 10 dB pad, the Audio-Technica AT2050 microphone is ideal for studio and live sound use on vocals, piano, strings, drum overheads, guitar amps, and more.Three switchable polar patterns: omni, cardioid, figure-of-eight Switchable 80 Hz high-pass filter and 10 dB pad Large diaphragm for smooth, natural sound and low noise State-of-the-art surface-mount electronics ensure compliance with A-T's stringent consistency and reliability standards Includes shock mount & protective pouch |
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Mojave Audio Ma-300 Large-Diaphragm Multi-Pattern Tube Condenser Microphone $1295 The MA-300 is a multi-pattern large diaphragm, vacuum tube condenser microphone. Based upon the widely accepted MA-200 designed by David Royer, the MA-300 adds a continuously variable pickup pattern selector, 15dB pad and a switchable bass roll-off. The MA-300 gives warm, full-bodied reproductions of vocals and instruments, with none of the shrillness and high frequency distortion artifacts that are often encountered with modern condenser microphones. Utilizing hand-selected, double diaphragm 3-micron capsules, high-quality Jensen audio transformers and military-grade JAN 5840 vacuum tubes, the MA-300 performs at a level reminiscent of some of the best loved classic condenser microphones. The MA-300 power supply can be set for 115V and 230V, 50 or 60 Hz, through an internal switch (100V is also available). Each MA-300 microphone, power supply and cable set is burned in for 24 hours, carefully tested and evaluated, then packaged in its protective case-within-a-case.Remotely controlled, continuously variable polar pattern selectorSwitchable 15dB padSwitchable Bass Roll-offHand-selected 3-micron double diaphragm capsuleJensen audio transformerMilitary grade JAN 5840 vacuum tubeInternal switchable power supply voltageUltra clean signal pathIncludes an aluminum case, AC power supply and cable, 16-foot microphone cable with 5-pin male and female connectors, and shock mountRecommended applications: Use anywhere you would use an expensive, large diaphragm tube microphone.VocalsVoice Over and BroadcastAcoustic InstrumentsPianoDrum Overheads, Drum RoomsOrchestral RecordingChoral Recording |
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Audix Cx212b Large Diaphragm Condenser Microphone Multi-Pattern $399 The CX-212B multi-pattern, dual diaphragm condenser microphone is an exceptional tool for professional audio production, project studios and live stage performances. Delivering a smooth, uniform frequency response from 20 Hz - 20 kHz, the CX-212B offers a choice of three polar patterns: cardioid, omnidirectional, and figure 8. Additionally, the CX-212B is equipped with a bass roll-off filter to help eliminate rumble in the lower frequencies.The CX-212B, for use in sound pressure levels up to 133 dB, is ideal for a wide variety of acoustic instruments, vocals, string sections, ensembles and ambient room miking. The CX-212B, which is designed with discreet low noise preamp circuitry, operates on 48 volts phantom power. For optimum results use the CX-212B with a high quality mic preamplifier and microphone cable.Multi-pattern: cardioid, omni, figure-8Resistant to touch noise and vibration35 mm (1.37) Capsule27.5 mm (1.08) Gold vapor dual diaphragmLow noise electronicsRich, warm tones ideal for digital recordingHeavy duty isolation shockmount includedRoad case for mic and shockmount3 year warrantySupplied accessories:Isolation shockmount (SMT-CX112)Aluminum carrying case (CASE-CX)Applications:Studio vocals, lead and backingVoice overChoirAmbient room micDrum overheadsOrchestraBells, chimes, marimba, vibesAcoustic instrumentsElectric guitar cabs |
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CAD GXL3000BP Multi-Pattern Condenser Microphone Black Pearl Chrome $139.99 The CAD GXL3000BP is a large diaphragm multi-pattern condenser that is borne of precious metal and pure electricity. Tune two golden membranes intimately across polished bass and inject electrons with oscillatory high tension. Drive emotion across copper and iron by field-effect detection. Wrap it in Faraday's cage to conceive the GXL3000. Live all three polar patterns as you align space and tone. The GXL3000BP is a great well-rounded general instrument mic for applications in the home studio, and is priced for the budget minded home studio owner. It is sonically described as having boosted upper mids and highs that provide extra air, cut and clarity. Stylishly finished in black pearl chrome. Features include hi-pass filter and attenuator. Elastic shock mount and protective pouch are included. P48 (48V) phantom power is required.Applications: studio vocals, voice-over, choir, acoustic instrument, guitar cabinets, bass cabinets, piano, and ambient drum room. |
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Cad Gxl3000bp Multi-Pattern Condenser Microphone Black Pearl Chrome $139.99 The CAD GXL3000BP is a large diaphragm multi-pattern condenser that is borne of precious metal and pure electricity. Tune two golden membranes intimately across polished bass and inject electrons with oscillatory high tension. Drive emotion across copper and iron by field-effect detection. Wrap it in Faraday's cage to conceive the GXL3000. Live all three polar patterns as you align space and tone. The GXL3000BP is a great well-rounded general instrument mic for applications in the home studio, and is priced for the budget minded home studio owner. It is sonically described as having boosted upper mids and highs that provide extra air, cut and clarity. Stylishly finished in black pearl chrome. Features include hi-pass filter and attenuator. Elastic shock mount and protective pouch are included. P48 (48V) phantom power is required.Applications: studio vocals, voice-over, choir, acoustic instrument, guitar cabinets, bass cabinets, piano, and ambient drum room. 1 dual diaphragm gold sputtered capsule Cardioid, figure-of-eight, omnidirectional polar patternsHi-pass filter 10 dB padBlack pearl chrome finishIncludes elastic shock mount and protective pouchPhantom power required |
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Used M-Audio Solaris Large-Diaphragm Multi-Pattern Condenser Microphone $318.49 The M-Audio Solaris is alarge-diaphragm condenser microphone that makes a versatile and appealing addition to your project studio's mic locker. The multi-pattern Solaris mic serves as a single or multipurpose mic for personal home studiosetups. The Solaris microphone has been painstakingly designed with features usually reserved for more expensive and exotic microphones. Its precision-designed 3-micron diaphragm, selectable polar patterns, bass roll-off filter, and switchable -10dB pad place it firmly in a class previously reserved for high-end imported studio mics. Its innovative, alluring designer look and vintage motif add appeal.Offering precision circuitry and components, low self-noise, and minimal coloration, the Solaris microphone is the ideal tool for capturing the nuances of vocals, acoustic instruments and other critical source material. With its unparalleled craftsmanship and quality construction, the Solaris delivers professional-quality recordings at an affordable price. Includes case and shock mount.Requires phantom power.Precision-designed 3-micron diaphragmSelectable polar patternsBass roll-off filterSwitchable -10dB padDesigner look with vintage motifIncludes case and shockmount |
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CAD GXL3000 Multi-Pattern Condenser Microphone List Price: $159.00 Sale Price: Too low to display  |
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Borne of precious metal and pure electricity. Tune two golden membranes intimately across polished bass and inject electrons with oscillatory high tension. Drive emotion across copper and iron by field-effect detection... |
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Audio Technica 20 Series AT2050 Multi Pattern Condenser Microphone List Price: $369.00 Sale Price: $219.99 |
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The AT2050 provides consistent, superior performance in switchable cardioid, omnidirectional and figure of eight polar pattern settings. It's dual large diaphragms are gold-vaporized and aged to achieve optimum characteristics over years of use... |
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Golden Age Project FC3 Multi-pattern Large Diaphragm Condenser Microphone List Price: $149.99 Sale Price: $149.99 |
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The FC 3 is a high quality dual capsule condenser microphone, inspired by classical microphone models. The FC 3 is a very versatile microphone with a wide frequency response and a large dynamic range... |
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Samson Multi-pattern Condenser Mic List Price: $224.99 Sale Price: $99.99 Used From: $90.99 |
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Following on the success of the C01U, Samson is proud to introduce the C03U, multi-pattern USB studio condenser microphone. Based on the extremely popular C03 studio condenser, the C03U delivers the same pristine audio quality and enhanced capabilities along with a high quality A/D converter and USB output... |
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Blue Microphones Yeti Pro USB Condenser Microphone, Multipattern. List Price: $249.00 Sale Price: Too low to display Used From: $186.75 |
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The Yeti Pro is the world’s first USB microphone combining 24 bit/192 kHz digital recording resolution with analog XLR output.Featuring three custom condenser capsules and four different pattern settings, the Yeti Pro can capture digital audio with up to fourtimes the clarity found on CDs... |
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APEX 480 Multi-Pattern Wide Diaphragm FET Condenser Microphone Sale Price: $139.00 |
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The Apex 480 wide diaphragm FET microphone offers a warmth and tone similar to that of a tube microphone without the limitations often associated with a tube mic design. The Field Effect Transistors (FETs) used in the Apex480?s deliver incredible clarity with an extremely wide dynamic range... |
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Sterling Audio ST59 Multi-pattern FET Condenser Mic List Price: $599.99 Sale Price: $299.99 |
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The Sterling Audio ST59 is an FET condenser microphone that employs a large capsule with a dual sided ultrathin 3-micron evaporated gold Mylar diaphragm. The ST59 mic is built with an exclusive process that extends high frequencies and improves details and depth on both vocal and instrument recordings... |
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CAD e300 Multi-pattern Condenser Microphone List Price: $399.00 Sale Price: $299.00 Used From: $149.00 |
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Powerful and articulate, the e300 blows away the competition with strength and precision. The externally-biased large-diaphragm capsule and high-power transformerless electronics deliver the vocal impact you deserve... |
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Sontronics SATURN multi-pattern condenser microphone Sale Price: $999.00 |
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Sontronics SATURN multi-pattern condenser microphone. The Sontronics SATURN has been developed with the help of top producers, artists and educators from around the world to set a new standard in flexible microphone performance and high-grade audio reproduction... |
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Avantone CK-7 Large Capsule Multi-Pattern FET Condenser Microphone Sale Price: $279.00 |
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The Avantone "Cabernet (C-series)" mics are designed to offer true professional performance. They will meet or surpass the performance and specifications of much higher priced mics. The design, character and performance can be compared directly to fine studio-standard FET mics... |
Offshore Black Sea an Opportunity for the Future - Evidence of Larger Structures With Improved Understanding of the Depositional Systems
International Hot Spots - The Black Sea
AAPG & AAPG European Region Energy Conference and Exhibition (November 18-21, 2007) Technical Program
I have compiled these abstracts from the AAPG conference in Athens 2007, where the Black Sea had its own sessions. Especially Bulgaria, Ukraine and Georgia were covered during the session, but also some examples from offshore and onshore Turkey were covered during these sessions. The under explored Offshore Black Sea has gained more attention the latter years since more data has been collected. Especially offshore Ukraine, several generations of 2D seismic has revealed some potential offshore until now not been discovered. However since the mid 1990’s there has been some interest due to the first generation 2D seismic and some older CCCP seismic, pre 1990’s. With this compilation we want to promote more interest for the offshore Black Sea, as we see this as an area for the future as oil and gas legislations in bounding countries mature and gets more open for international oil and gas companies, as well as investors.
Upper Jurassic Reefs of the Western Caucasus-Crimea; Hydrocarbon Implications for the Eastern Black Sea
Li Guo1, Stephen J. Vincent1, Samuel P. Rice1, and Vladimir Lavrishchev2. (1) CASP, Department of Earth Sciences, University of Cambridge, 181a Huntingdon Road, Cambridge, CB3 0DH, United Kingdom, phone: +44 1223 337068, li.guo@casp.cam.ac.uk, (2) Kavkazgeols'emka, Ul. Kislovodskaya 203, Yessentuki, Russia
Widespread Upper Jurassic reefs are important potential reservoir facies in the Eastern Black Sea Basin. Russian seismic reflection data from the northern Shatskiy Ridge indicate possible offshore reef-facies occurrences up to 1-2 km thick and 10-20 km wide. Data from excellent onshore exposures in the Russian Western Caucasus and Crimea provide a reservoir analogue for offshore targets. A model for development and distribution of the carbonate reefs is presented with reference to possible alternative tectonic settings for the Upper Jurassic north Tethyan Margin.
Outcrops of well-preserved Upper Jurassic reefs can be grouped into coral-dominated, siliceous sponge-microbial and microbial types. Patchy and massive coral-dominated reefs formed at shallow-water platform margins or in slightly restricted deeper-water mid shelf settings. Siliceous sponge-microbial and microbial reefs occur as lenses and mounds and are restricted to deeper-water mid-outer shelf environments. The development of these reefs was controlled mainly by local variations in water depth, light, and the availability of nutrients.
The reefs exhibit a complex pattern of porosity development reflecting independent diagenetic histories involving near-surface and deep-burial dissolution, dolomitization and dedolomitization. Porosity is particularly common in coral-dominated reef facies and consists of both primary and secondary types.
Coral-dominated reefs analogous to onshore outcrops in the Russian Western Caucasus are likely to occur along the northwestern margin of the Yuzhnyi-Adler carbonate platform in the Eastern Black Sea. Possible isolated deeper-water reefs imaged on the northern Shatskiy Ridge could be largely composed of siliceous sponge-microbialite and microbialite facies. Similar reef facies may be present on the Mid Black Sea High.
Lithostratigraphy of the Upper Jurassic – Cretaceous Deposits and Hydrocarbon Perspective in the Romanian Shelf of the Black Sea
Ovidiu Nicolae Dragastan, Faculty of Geology and Geophysics, Bucharest University, Bulevardul N Balcescu no. 1, Bucharest 010041 Romania, phone: 0040729610876, ovidiud@geo.edu.ro
In the Romanian shelf of the Black Sea (offshore), Petromar Co. drilled and has obtained cores of Middle and Upper Jurassic- Cretaceous deposits, as well as Paleogene and Neogene ones. The Mesozoic and Cenozoic deposits belongs to two main geological units: the North Dobrogea Orogenic Belt and the Moesian Platform. In the offshore of the North Dobrogea Orogenic Belt three cycles of sedimentation have been identified: 1. A lower transgressive cycle corresponding to the compression phase of synrift 1 (Bajocian- Callovian ?), the last stage possible corresponding to a „general” unconformity or to a break up 1 between the Middle and Upper Jurassic , with black calci- and siltic turbidites (Heraclea Formation). 2. A middle transgressive compression phase composed by mudstones, claystones and siltstones ( Pontus Formation), Upper Jurassic- Neocomian in age corresponding to the synrift 2 followed by a break up 2 to the Jurassic-Cretaceous boundary and intra Neocomian covered different times hiatuses. 3. An upper large postrift phase Albian to Senonian, continued during the Paleogene and Neogene. Many short and long time hiatuses are recorded that include the Cretaceous deposits. Three source rocks can be identified for hydrocarbon generation: - the black argillaceous, siltic to sandstones of the Heraclea Formation (Middle Jurassic in age), about 1000 m in thickness.; - the black argillites of the Pontus Formation (Neocomian) and - the Oligocene- Miocene bituminous shales, clays and marls known more or less as the Maikop beds.
Hydrocarbon Accumulation in the Permo-Triassic Reservoirs of the Moesian Platform
Pene Constantin1, Niculescu Bogdan1, and Mitru Daniela2. (1) Faculty of Geology and Geophysics, University of Bucharest, 6 Traian Vuia Street, Bucharest, RO - 020956, Romania, phone: +40 21 3181588, penec@gg.unibuc.ro, (2) T.E.I.-Kozani, T.E.I.-Kozani, 114, Ioanis, Kozani, Kozani, Greece
Romanian petroleum basins contain hydrocarbon fields in the Triassic reservoirs only in the north-west of the Moesian Platform and in its south was identified an “oil show”. This distribution of the oil and gas fields is a little enigmatic, because of their position regarding the Bals-Optasi Uplift. Well logs, cores, some seismic profiles and lithophacies maps define the depositional systems and the dispersal patterns of the reservoirs and seals of the Triassic formations. The Permo-Triassic deposits consist of three lithostratigraphic formations: Lower Red Detrital (LRD Fm) (Lower Triassic), Carbonatic-Evaporitic (C-E Fm) (Middle Triassic) and Upper Red Detrital (URD Fm) (Upper Triassic). The lowest part of the LRD Fm and the URD Fm consists of multiple coarsening-upward parasequences deposited in deltaic and fluviatil environments of the lowstand systems tract during a forced regression. The upper part of the LRD Fm consists of fining-upward parasequences that sugests a strong transgression. This evolution is the result of the Permo-Triassic riftogenesis. The main reservoir is a very well sorted sandstone (“Bradesti sandstone”). The seals consist of marls associated with evaporitic rocks. The reservoirs of the C-E Fm consist of limestones and dolomites, especially in the lower part of this formation and the seals are composed by evaporitic rocks. Analysis of the main Triassic reservoirs (Bradesti sandstone as well as dolomite and limestone in the C-E Fm) suggests that there are others prospective areas for hydrocarbon accumulations in the southern part of the Bals-Optasi Uplift.
Tectonic Style and Oil and Gas Accumulation in the Moldavian Platform
Pene Constantin1, Negulescu Rodica2, and Coltoi Octavian1. (1) Faculty of Geology and Geophysics, University of Bucharest, 6 Traian Vuia Street, Bucharest, RO - 020956, Romania, phone: +40 21 3181588, penec@gg.unibuc.ro, (2) Prospectiuni SA, Prospectiuni SA, Caransebes Street, 1, Bucharest, 020834, Romania
The Moldavian Platform represents the western part of the East European Platform. Seismic profiles, well logs, cores as well as geological cross sections and maps show that during Alpine orogeny, the western part of the platform was gradually underthrusted by the Eastern Carpathian Orogene. This structural evolution imprinted a monoclinal character of the deposits and they dip westward beneath the Carpathian Foredeep (Molasse) and Eastern Carpathian Flysch. The compressional tectonic regime accompanied by slowly strike-slip movements and interrupted by short moments of extension imprinted the main tectonic style of the Moldavian Platform. It is dominated by a fault network with two predominantly directions. A first system of major faults, almost parallel with the Eastern Carpathian Orogene is of NNW-SSE orientation (Paltinoasa Fault, West Paltinoasa Fault, and Siret Fault). The second system consists of small cross faults (E-W oriented) and it generated more tectonic block alignments that follow the longitudinal fault trace. The older deposits than the Upper Sarmatian ones plunge step by step beneath Eastern Carpathians along major faults. The tectonic blocks on every step folded and generated gently anticlines and faulted monoclines. The intense compressional regime and the high subsidence rate of the Sarmatian deposits favored the formation of the lithostratigrafic traps. The gas and gas-condensate are reservoired in Albian, Badenian and Sarmatian sandstones and marls and anhydrites seal them. The study of the tectonic evolution of the Moldavian Platform suggests new prospective areas for the gas and gas-condensate in the pre-Badenian deposits.
Paleocene carbonate platform facies distribution (northern part of the Black Sea basin, Ukrainian offshore)
Sergii Vakarchuk, Department of Complex Geology- Industrial Researches, Scientific Research Institute of Oil and Gas Industry (Naukanaftogaz), Uritskogo Str., 45, Kyiv, 03035, Ukraine, phone: +380445850219, fax: +380442487101, vakarchuk@naukanaftogaz.kiev.ua, Piter Chepil, Scientific Research Institute of Oil and Gas Industry (Naukanaftogaz), Uritskogo Str., 45, Kyiv, 03035, and Tetyana Dovzhok, Department of oil and gas geology problems, Scientific Research Institute of Oil and Gas Industry (Naukanaftogaz), Uritskogo Str., 45, Kyiv, 03035, Ukraine.
This study is aimed to detailed facies subdivision and mapping of the Paleocene carbonates that is stipulated by several oil and gas discoveries recently made in this sequence. An analysis is based on an integrated interpretation of core sets and well logs for more than 40 deep wells drilled in the different tectonic zones of the basin and regional and local seismic data. Carbonates of Paleocene occur at depth of 500-6000 m and extend over the most of structural-tectonic zones of the Black Sea basin. The thickness of these sediments changes from 50-100 m to 600-900m. The study has revealed several facies zones in the carbonate sediments of Paleocene: littoral (alternation of skeletal wackestones and packstone, lime mudstones, marls, calcareous sandstones and siltstones), intra-shelf (skeletal wackestones and packstone 60-70%, marls 10-20%, pelitomorphic limestone 5-15 %, baundstones 3-5%, sales 10%), outer-shelf, (skeletal wackestones and packstone 30-40%, marls 20-30%, pelitomorphic limestones 10 %, sales 20%), gentle slope (marls 20-30%, wackestones and packstone 10-15 %, pelitomorphic limestones 20 % sales 30-50%) and basin (sales and marls with intercalation of pelitomorphic limestones). Four gas and gas-condensate fields are discovered within the Paleocene carbonate to date. All from them are located in the intra-shelf zone. The reservoirs are represented with skeletal wackestones. The reservoirs are porous and porous-fissured types. Open porosity - from 10 to 32%, permeability – 0,0005-0,045 mcm2.
South Akcakoca Gas: A Black Sea Discovery 30 Years in the Making
Michael J. Fitzgerald, III1, Ed Ramirez1, William Moulton2, and Al Garcia3. (1) Toreador Resources Corp, 4809 Cole Ave, Suite 108, Dallas, TX 75205, phone: 214-559-3933, fax: 214-559-3945, mfitzgerald@toreador.net, (2) Independent Consultant, (3) Integral Technology Group
Six Eurasian countries surround the Black Sea. Of those six countries, the Republic of Turkey has the longest coastline, 1595 km. of any bounding country. Prior to 2004 there had been only six well drilled in the Turkish Black Sea, four in the far western Black Sea area and two in the west central area offshore from a small vacation town, Akcakoca.
The Akcakoca #1 and #2 wells had been drilled in the mid-1970's designed to test Mesozoic and Cenozoic sediments seen onshore in outcrops and the subsurface. Early seismic had indicated the presence of sizable structures formed by compressional tectonics bounded by trust faults. The Akcakoca #1 well encountered gas shows in Eocene clastics from 1000m to 1400m and tested 3.25mmcfpd during an open-hole DST. The Akcakoca #2 well encountered gas shows but no tests were run.
In 2000 Madison Oil Turkey, later merged with Toreador Resources, acquired a 962,000 acre permit that contained the Akcakoca wells. Utilizing existing seismic and the original wells Toreador explorationists determined that potential existed for a significant accumulation. A conventional 2-D seismic survey and follow-up high resolution 2-D surveys enabled geophysics to map velocity anomalies that could be tied to the 1970's wells.
In 2004 the Ayazli #1 wildcat was drilled on a thrusted anticline 3 km south of the original Akcakoca #1 well. This well tested approximately 12.0mmcfgpd from four Eocene age sands. Drilling over the next two and a half years saw the exploration group drill 12 successful well out of 14 and initiate the first gas production in the Turkish Black Sea.
This paper will review the geology and geophysics that went into this effort.
Debunking the Myths of Crimean Geology
Igor V. Popadyuk, Naukanaftogaz, Kyiv 03035 Ukraine, phone: 38 044 5852764, fax: 38 044 2487101, popadyuk@naukanaftogaz.kiev.ua
The Crimea Mountains located in the southernmost part of Crimea Peninsula in southern Ukraine hold keys to the Black Sea understanding as the coastline of Crimean Peninsula spans both Western and Eastern Black Sea.
At least two myths of the regional stratigraphy might be debunked. Myth 1: Tauric Group is not Triassic-Early Jurassic in age. Based on published palaeontological data (Ammonites) it is likely the Tauric Group to be younger, the most probably Aptian- Early-Mid Albian in age. It means that the compressive event affected basins in the Crimea region at the end of Albian, not Middle Jurassic. Myth 2: The flysch and conglomerate successions widely developed on eastern Crimea and commonly referred to the Upper Jurassic are Tertiary in age as it might be concluded based on published palaeontological (foraminifera) data. It means the volume of clastics shed from the Crimea Mountains during the Tertiary uplift seems to have been significant.
Late Jurassic to Early Cretaceous successions are incorporated in two major thrust sheets, named structurally descending as Yayla thrust and Tauric thrust. Yayla thrust is composed mostly of shallow marine carbonates of Late Jurassic-Neocomian age. Tauric thrust consists of Tauric flysch succession and equivalent siliciclastic deposits of Aptian – Early-Mid Albian age. Both of these thrust sheets were transported northward probably during the Late Albian pulse and sealed by post-tectonic cover of Cenomanian to Late Eocene sediments. The Crimea region was tectonically uplifted and eroded after Late Eocene.
The Tertiary Kamtchia Fluvio-Estuary-Fan System of Eastern Bulgaria
Rudolf Dellmour, OMV Exploration & Production GmbH, Vienna, Austria, Rudolf.Dellmour@omv.com and Gian Gabriele Ori, IRSPS, c/o Univ d'Annunzio, Viale Pindaro 42, Pescara, 65127, Italy.
OMV Bulgaria is holding the “Varna Deep Sea” Exploration license in the near offshore from the city of Varna in Eastern Bulgaria. The block covers a large Tertiary fan system sourced from the Balkanide and Carpathian mountains.
The tectonically active Hinterland provided during Eocene to Miocene a vast amount of siliciclastics from eroded crystalline and metamorphic rocks. These sediments were deposited into alluvial plains and alluvial fan aprons during relative high-stands and periods of tectonic quiescence. Relative low-stands produced massive erosion of this detritus which has been funneled through a pronounced Paleo-valley system into the deep sea. This paleovalley system spans over large parts of the Paleogene and Neogene. Two major sequence boundaries have been identified along with several minor unconformities. Today the “Paleo Kamtchia Incised Valley” forms an impressive geomorphologic feature in the landscape south of Varna.
Recent geological fieldwork over the last 3 years revealed the sedimentary history from the Eocene to the Pliocene. Field evidence for this clastic system includes fluvial, tidal and estuary sedimentary environments. This long living system of the Paleo Kamtchia came to an end when the Danube River finally broke through the Carpathians during early Quaternary. After this event the Danube captured the drainage area of the Paleo Kamtchia reducing the Kamtchia River system to a creek of minor importance.
3D seismic data acquired in 2006 reveals a pronounced and complex deepwater fan system connected to this “Paleo Kamtchia Incised Valley”. This fan system opens up a new play in the Bulgarian Black Sea similar to that which has been successfully chased by Explorationist's worldwide over the past 20 years.
The Moesian Platform: a Critical Piece in the Tectonic Puzzle of the Black Sea Region
Gabor Tari, AllyGabor Geoscience, 6719 Avenue B, Bellaire, TX 770401, phone: 832-724-1404, gabor@allygabor.com
Based on recent results on the structure of the Moesian Platform and the Bohemian Massif segments of the European continental margin, a new model of the evolution of these passive margins is outlined. The Moesian Platform is interpreted as the upper plate, conjugate margin of the Bohemian segment of the European margin, rifted and drifted away during the Middle and Late Jurassic. Moesia, as a new microplate, was separated from the European margin at about the end of the Bathonian and started to drift towards the SE. There are no constraints on the rate of the drifting but by the Aptian Moesia should have reached its present-day position, at least 600 km to the SE from its original position. The direction of drifting can be deduced from the geometry of the major faults to the NE from the present-day Moesian Platform, in the broader Tornquist-Tesseyre fault zone, for example the Peceneaga-Camena fault bounding the Dobrogea orogenic belt. To the SW, the northeastern edge of the Bohemian Spur projecting below the Pannonian Basin is mappable by reflection seismic data providing an additional geometric constraint for the separation of Moesia from Europe. The correct reconstruction of the pre-Jurassic position of the Moesian Platform has important implications for the paleogeography of the Black Sea prior to its opening. For example, the Triassic rift system of Dobrogea in Romania can be directly correlated with the Strandzha rift sequence in southernmost Bulgaria offering a much simpler paleogeographic scenario than previously thought.
The Geological History of the Istria ‘Depression’, Offshore Romania: Tectonic Controls on Second Order Sequence Architecture
David Boote, Consultant, 12 Elsynge Road, London SW18 United Kingdom, phone: 0208 871 0069, davidboote@elsyngeroad.fsnet.co.uk
The Istria ‘Depression' or trough of offshore Romania, lies at the intersection of the trans-European, Tornquist-Teisseyre ‘Zone' and the Black Sea back arc basin, just outboard of the East Carpathian orogenic welt. It experienced an extraordinary polyphase history of subsidence, sedimentation and dramatic sediment evacuation during the late Mesozoic and Tertiary, reflecting the interplay between these three tectonic domains. It first developed as a trans-tensional rift in the Triassic- Jurassic to be compressed and deformed during the (?)end-Jurassic Cimmerian orogeny. Residual topography was filled by a west-facing continental clastic-evaporite sequence during the Neocomian. This was terminated by uplift and doming associated with Apto-Albian rifting and back-arc spreading in the western Black Sea. Post break-up subsidence and tilting of the Black Sea rift margin, led to easterly evacuation of its early Cretaceous sedimentary fill by gravity-driven mass wastage. The margin was subsequently transgressed from the east with deposition first confined within the open Istria trough and later expanding out onto the bounding highs. By the end of the Cretaceous, it had been entirely buried, only to be partially evacuated once more in the early Palaeocene and again quite spectacularly during the (?)late Eocene. The deeply incised canyon formed at that time, was rapidly filled by Oligocene-Miocene sediments, but late Miocene (Messinian?) draw-down of the Black Sea basin was reflected by yet a third period of erosional incision. Continental margin outbuilding followed during the Plio-Pleistocene with deposition of several rapidly prograding wedges. This was interrupted by a major gravity slide event and several phases of shelf-margin canyon incision and late phase of shelf margin listric faulting, reflecting the final docking of the Carpathian orogen.
Oil and Gas Prospects of the Ukrainian Part of the Western Black Sea
Oxana Khriachtchevskaia, Naukanaftogaz, Uritskogo Str., 45, Kyiv, 03035, Ukraine, phone: +38(044)5852762, hryaschevska@naukanaftogaz.kiev.ua and Sergiy Stovba, Naukanaftogaz, Uritskoga Str., 45, Kiev, 03035, Ukraine.
Eight gas-condensate commercial fields have been discovered within the Odessa shelf (western part of the Ukrainian Black Sea) during last three decades. The success factor of drilling is 0.5. The productive horizons are located in Upper Cretaceous, Palaeocene, Eocene, Oligocene and Lower Miocene sequences. Present-day exploration activity is focused on inverted structural highs within shallow water area (
Hydrocarbon Bearing Area in the Eastern Part of the Ukrainian Black Sea
Sergiy Stovba, “Naukanaftogaz” - Scientific Research Institute of Oil and Gas Industry of National Joint-Stock Company “Naftogaz of Ukraine”, Kyiv, Ukraine, phone: +38 044 5852765, stovba@naukanaftogaz.kiev.ua and Oxana Khriachtchevskaia, Naukanaftogaz, Uritskogo Str., 45, Kyiv, 03035, Ukraine.
A regional investigation of the eastern part of the Ukrainian Black Sea has been carried using a vast set of regional seismic reflection profiles, including the new set of regional seismic profiles by Naftogaz of Ukraine. To the south of the Crimea peninsula 20 large structures with closures of 50-200 sq. km have been mapped within Oligocene-Miocene-Pliocene sediments. Huge structures (>350 sq. km) in Tertiary and older sediments exist further to the east within Sorokin Trough and Andrusov Ridge. In the easternmost part of the Ukrainian Black Sea a number of high-amplitude anticlines has been mapped in shallow water depth and a huge Mesozoic structure of 400 sq. km in deep water depth (150-700 m). Eocene, Oligocene and Miocene sediments are considered as source rocks with good generative potential for hydrocarbons. There are strong direct hydrocarbon indicators on seismic data. According to expert appraisal, each major lead formed within Upper Mesozoic-Cenozoic section in water depths of 100 m to 2000 m has an area of several hundred sq. km, with vertical closure of hundreds of meters, and has the potential to contain hundred million barrels of recoverable hydrocarbons. The drilling of Subbotina well up to 4300 m has confirmed the high oil and gas potential of Kerch shelf. Plenty of oil and gas reservoirs were determined along the section of the well. Some of them were tested in the lower part of Oligocene sequence with successful result and commercial oil inflow.
The Tectonic Ecology of the Black Sea
Celal Sengor, Istanbul Technical University, Istanbul, Turkey, phone: 90 212 285 6209, sengor@itu.edu.tr and Boris NatalIn.
The Black Sea formed within a complicated area. It had two orogenic collages plastered against each other and fragments of one Gondwana-Land bound continental margin orogen: the Scythides, and the two parts of the Cimmerides. It began opening as a consequence of Alpide subduction of Neo-Tethyan ocean floor in the Aptian-Albian interval and at least in its eastern part, clearly split a continental margin arc. Eastwards it clearly did not connect with the earlier Flysch trough of the Greater Caucasus and neither did it have any relation to the ongoing Cimmeride shortening as late as the Nish-Trojan trough formation. It disrupted a pre-existing fabric, but it is remarkable that the Andrusov Ridge exactly parallels the old Scythide/Cimmeride fabric of en-echelon arc segments.
It evolved as a marginal basin of Japan-Sea type and even in its history of rear-arc shortening it greatly resembles the present structure of the Japan Sea. After the Miocene Arabia/Eurasia final collision, Black Sea began shortening as far east as Zonguuldak. West of there it was extending north-south in unison with Bulgaria, Macedonia and Greece.
It is remarkable how 'continental' its behaviour is. We compare this with that of the Tarim Basin and suggest that the Tarim is perhaps a palaeo-Black Sea.
Geological History and Hydrocarbon Potential of the Eastern Black Sea Region
Anatoly M. Nikishin, Geological Faculty, Moscow State University, Moscow, 119992, Russia, phone: (495) 939 49 31, fax: (495) 939 38 65, nikishin@geol.msu.ru and Aleksandr P. Afanasenkov, YUKOS oil companie, Moscow, Russia.
The Eastern Black Sea Basin originated as a back-arc basin during the Cretaceous times. Both the Western and Eastern Black Sea basins have been opened nearly simultaneously during Cenomanian to Coniacian times. Shatsky Ridge was a carbonate platform and zone of pinnacle-type reefs during the Late Jurassic. It was a platformal area since the Cretaceous. The Tuapse, Guria and Sorokin basins originated at the Eocene-Oligocene transition as a flexural foredeep basins. Shatsky Ridge was affected by flexural tectonics also at those times. Shatsky Ridge has a Miocene river system. Since Pliocene only Shatsky ridge was subsided up to 2 km simultaneously with main folding event in the Tuaspe Basin. Hydrocarbon potential of the Shatsky Ridge, Tuapse Basin and Sorokin Basin is connected with: (1) Late Jurassic carbonate platform and system of large pinnacle-type reefs: (2) Possible Paleocene bioclastic limestones; (3) possible Eocene nummulite limestones; (4) possible Oligocene turbitites with sandstone bodies; (5) Miocene river system; (6) Miocene and Pliocene horizons of sandstones.
The Impact of Recent Data on the Interpretation of the Geologic Evolution and Petroleum System of the Eastern Black Sea Basin, Offshore Georgia
Ryan J. Wilson, Neil Mountford, Paul Maguire, and Richard Hedley. Anadarko Algeria Corporation, 1 Harefield Road, Uxbridge, UB8 1YH, United Kingdom, phone: +44 (0)1895 209400, ryan.wilson@anadarko.com
The genesis and sediment-fill history of the Eastern Black Sea Basin, offshore Georgia has been largely understudied with little new data being acquired since the Soviet Era. However, recent data acquired demonstrate the existence of a Tertiary petroleum system.
The Oligo-Miocene Maykop Formation is a widespread source rock that extends from Romania to Turkmenistan. It has been identified as the source of the hydrocarbons in the giant fields of the South Caspian and the accumulations in both the western and eastern onshore basins in Georgia. In addition, oils collected and analyzed from active seeps offshore Georgia, directly above mapped structural culminations, confirms the presence of a generative Maykop in the Eastern Black Sea Basin.
Offshore Georgia can be subdivided into three tectonic provinces, one of which is characterised by high-amplitude anticlines that strike in a southwest-northeast direction as a result of shortening from the Middle Miocene to present day. These fold and thrust anticlines range from classic box folds to overturned folds, with a common decollment within the Maykop.
The primary reservoir sands are believed to be of Middle Miocene age, and based on 3D seismic data, the sandstones were deposited in deepwater channel-levee systems that originated from the north. Late Miocene to present day depositional systems have a south-easterly provenance of volcanic/lithic origins.
In 2005, the first deepwater well in the Eastern Black Sea Basin was drilled offshore Turkey but did not penetrate the northerly-sourced reservoir system. Consequently, the offshore Georgia petroleum system, with billion barrel opportunities, remains untested.
Mud Volcanoes and Fluid Migration in the Sorokin Trough
Sebastian Krastel1, Michelle Wagner-Friedrichs1, Volkhard Spiess1, Leonid Meisner2, Gerhard Borhmann3, and Michael Ivanov4. (1) Marine Technology - Environmental Research, Bremen University, Klagenfurter Strasse, Bremen, D-24359, Germany, phone: +49-421-2184598, skrastel@uni-bremen.de, (2) Marine Geology and Hydrocarbon potential department, Okeangeofizika Research Institute, Krymskaja Str. 18, Gelendzhik, 353470, Russia, (3) Marine Geology, Bremen University, Klagenfurter Strasse, Bremen, 28359, Germany, (4) Moscow State University
The Sorokin Trough forms structural depression along the south-eastern margin of the Crimean Peninsula. Compressive deformation affects the growth of diapiric ridges and facilitates fluid flow to the seafloor and the evolution of mud volcanoes above the diapirs. The main objective of a high-resolution multi-channel seismic survey carried out by Bremen University (Germany) was to study the evolution and formation of mud volcanoes correlated to gas/fluid migration and gas hydrates occurrences. We grouped mud volcanoes in the Sorokin Trough in three areas. The different geological setting influences the evolution of the individual mud volcanoes and hence their morphology. Collapsed depressions dominate in Area 1 in the western survey area. A 2.5D seismic data set was collected across the Sevastopol Mud Volcano representing a typical collapsed depression located above a complex diapiric structure with two ridges. Bright Spots in direct vicinity of the conduit of the mud volcano probably mark the base of the gas hydrate stability zone. We postulate that overpressured fluids initiated an explosive eruption generating the collapsed depression of the Sevastopol mud volcano and subsequent mud extrusions formed cones within the depression. The homogeneous fan deposits of the Palaeo Don-Kuban Fan in the central and eastern Sorokin Trough are characterized by increased permeability resulting in quiet effusive mud extrusions in Areas 2 and 3. Mud volcanoes in the central Area 2 reach enormous dimensions with diameters up to 2000 m and heights of about 100 m where faults with large offsets allow high mud flow rates.
Geology and Petroleum Potential of the Shatsky Ridge (Black Sea)
Alexey L. Meisner, DCS, Schlumberger logelco inc, 9 Taganskaya str., Moscow, Russia, Moscow, Russia, phone: +7 916 868 61 84, ameisner@moscow.oilfield.slb.com and Leonid B. Meisner, Geological, Yuzhmorgeologiya, Krymskaya Str. 18, Gelendzhik, Russia, Gelendzhik, Russia.
The Shatsky Ridge is an anticline structure that is comprised of the Upper Mesozoic-Paleogene rocks. Anticlinels have dimensions up to 66 x 18 km. It lies mainly at water depth about 2 km and extends from the Georgia coast to the Mountain Crimea (Ukraine). The goal of this work was to research perspective of Shatsky Ridge. Seismic and magnetic data have contributed to the recognition of main geological features. There are no wells drilled within the ridge, and the analog data from the Western Georgia and Crimea were used for lithology and reservoir prediction.
The lowest sequence consists of the Low Jurassic thick black shales, deposited on the top of Paleozoic basement. Magnetic anomalies caused most likely by the Middle Jurassic gabbro intrusions. Upper Jurassic-Eocene section consists of mainly carbonate rocks. This section contains the reservoir quality rocks. Limestone porosity varies between 5 - 20 %, range of permeability is 10 - 40 md. Presence of Upper Jurassic reefs, Eocene nummulitic limestone points to a shallow marine sedimentation. These reservoirs are overlain by marine thick shale seals of the Oligocene-Quaternary ages.
A potential of source rocks belongs probably to the Jurassic and the Low Cretaceous rocks. It is also possible that hydrocarbons could migrate into Mesozoic reservoirs from sources rock of the Eocene and the Maikop succession of the adjacent troughs.
Mud volcanoes and seismic anomalies "bright spot" indicate hydrocarbon accumulations in the sedimentary cover of the Shatsky Ridge.
Reservoir prediction, sizes of anticlines and hydrocarbon seeps make conclude that the Shatsky Ridge may contains undrilled prospects and form a basis for its future exploration.
Effects of Tectonics on Deposition in the Balkans of Eastern Bulgaria
Michal Nemcok, Energy and Geoscience Institute, University of Utah, 423 Wakara Way, Suite 300, Salt Lake City, UT 84108, phone: 801-585-9829, fax: 801-585-3540, mnemcok@egi.utah.edu, Charles J. Stuart, EGI at University of Utah, 423 Wakara Way, Suite 300, Salt Lake City, UT 84108, Dian Vangelov, Department of Geology at Sofia University, bul. Tzaz. Osvoboditel 15, Sofia, 1000, Bulgaria, Eric R. Higgins, Chesapeake Energy Corporation, 6100 N. Western Avenue, Oklahoma City, OK 73118, Chelsea Welker, EGI at University of Utah, 423 Wakara Way; Suite 300, Salt Lake City, UT 84108, and David Meaux, AOA Geophysics Inc, 11200 Westheimer, Suite 850, Houston, TX 77042.
The E Balkans geometry during Paleocene-Recent was characterized by a southeastward plunge toward the Western Black Sea, caused by: 1) a combination of eastward-thinning continental crust in the west, and oceanic crust in the east; 2) post-rift thermal subsidence of the continental crust; 3) buttressing against the Moesian Platform in the west and no buttressing in the east; and 4) northeastward advance of the thrustbelt.
The eastward-fading uplift and buttressing are evidenced by: 1) eastward decreasing amount of shortening along constructed profiles, yielding 30km, 10.5km, 11km and 4km from west to east; 2) eastward trend of more complete stratigraphic sections and shallower erosional levels; and 3) eastward increase in décollement depths, being 3.7km, 3.8km, 9.5-13.5km and 12.3-14.1km. The last thrusting age is progressively older toward the east from Middle Eocene through Late Eocene to Late Eocene/Oligocene. Onshore thrustbelt, which was significantly affected by buttressing against the Moesian Platform, exhibits thrusting followed by Late Eocene gravitational collapse, Oligocene quiescence and Neogene extension. The offshore thrustbelt exhibits thrusting followed by Oligocene-Neogene extension. A Paleocene-Middle Eocene piggyback basin formed in the onshore portion of the thrustbelt, centered in the East Balkan Zone, with a southeastward plunging axis, which migrated northeastward with basin shortening and filling.
Sedimentology And Timing Of Hydrocarbon-seepage (Lower Eocene, Varna, Bulgaria)
Eva De Boever, Geologie, K.U. Leuven, Celestijnenlaan 200 E, 3001 Leuven, Belgium, phone: +32 16 32 77 98, eva.deboever@geo.kuleuven.be, Rudy Swennen, Geologie, K.U.Leuven, Celestijnenlaan 200E, 3001 Heverlee, Belgium, and Lyubomir Dimitrov, Institute of Oceanology, P.O. Box 152, 9000 Varna, Bulgaria.
In the Pobiti Kamani area (Varna, NE Bulgaria), Lower Eocene sandy sediments contain several clusters of up to 8m high calcite-cemented chimney structures. ?13C values as low as -43‰ V-PDB indicate a hydrocarbon-seepage related origin. The depositional sequence of the shallow marine platform sediments is characterized by several cemented stratal surfaces which are cross cut by chimney structures. In this contribution, the origin of the cemented surfaces is addressed based on sedimentological, petrographical and stable isotope geochemical data and the implications with respect to the timing of hydrocarbon seepage are evaluated. Grain size measurements in two continuous vertical sections allow to distinguish two depositional sequences. Transgressive (TS) and maximum flooding (MFS) surfaces are characterized by extensive calcite cementation, thus indicating a sequence stratigraphical control on cementation. Different cement-types have been recognized. The bulk stable isotope signature of these cements indicates precipitation from Lower Eocene marine pore fluids, affected by later meteoric resetting. ?13C depletions of the dominant pore cementing “mosaic” cement as low as -20.6‰ V-PDB however supports also a pre-compactional influence of hydrocarbon-seepage which decreases within m-distance from chimney clusters. The MFS near the top of the Dikilitash Formation is partly cemented by transparent poikilotopic calcite in keystone-type vugs and in interparticular porosity. Its very early diagenetic origin and ?13C depletion (-16‰ V-PDB) suggest that hydrocarbon-bearing fluids percolated through the sandy sediments near the seafloor at the end of ??the Upper Ypresian. Other coarse-grained,13C depleted (-26‰ V-PDB) concretionary horizons likely resulted from post-sedimentary lateral migration of seepage fluids.
About the Author
Stig-Arne Kristoffersen
An Explorer
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