Evidence for gas accumulation associated with diapirism and gas hydrates at the head of the Cape Fear Slide

E.A. Schmuck; C. K. Paull

doi:10.1007/bf01593187

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Evidence for gas accumulation associated with diapirism and gas hydrates at the head of the Cape Fear Slide

E.A. Schmuck·C. K. Paull

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Abstract

Single-channel seismic reflection profiles show evidence for areas of significant gas accumulation at the head of the Cape Fear Slide on the continental rise oft North Carolina. Gas accumulation appears to occur beneath a gas hydrate seal in landward-dipping strata and in domed strata associated with diapirism. In addition, gas venting may have occurred near diapirs located at the head of the slide.

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Geo-Marine Letters Article

Source-reported bounding extent: 32.58384932565662° to 36.40359962073253° latitude; -81.474609375° to -75.772705078125° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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E.A. Schmuck, C. K. Paull. 1993. Evidence for gas accumulation associated with diapirism and gas hydrates at the head of the Cape Fear Slide. https://doi.org/10.1007/bf01593187

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