VAMPs—Possible hydrocarbon-bearing structures in Bering Sea Basin: Geologic notes
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Abstract
Narrow (1 to 2 km) subsurface columns of concave reflection horizons are common time-base seismic profiles collected in the Bering Sea basin. The columns of recorded downflexures are thought to be velocity pulldowns and commonly are associated with one or more arched or gently domed high-amplitude reflection horizons about 100 m higher in the section. Inferred from this association is that subsurface deposits characterized by anomalously low acoustic velocity are present.
We refer to the velocity-anomaly and reflection-amplitude association as a velocity-amplitude feature, or VAMP, and speculate that VAMPs are deep-seated “bright spots” underlain by a strong velocity pulldown possibly caused by gas-charged deposits.
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | VAMPs—Possible hydrocarbon-bearing structures in Bering Sea Basin: Geologic notes |
Series title | AAPG Bulletin |
DOI | 10.1306/C1EA5530-16C9-11D7-8645000102C1865D |
Volume | 62 |
Issue | 12 |
Year Published | 1978 |
Language | English |
Publisher | AAPG |
Contributing office(s) | Pacific Coastal and Marine Science Center |
Description | 8 p. |
First page | 2481 |
Last page | 2488 |
Other Geospatial | Bering Sea Basin |
Google Analytic Metrics | Metrics page |