期刊
GEOPHYSICAL RESEARCH LETTERS
卷 42, 期 3, 页码 733-742出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL062474
关键词
3-D seismic; hydrates; methane seepage; tectonic stress; Vestnesa Ridge; Arctic
资金
- Norwegian Research Council through CAGE-Center for Arctic Gas Hydrate, Environment and Climate [223259]
Methane expulsion from the world ocean floor is a broadly observed phenomenon known to be episodic. Yet the processes that modulate seepage remain elusive. In the Arctic offshore west Svalbard, for instance, seepage at 200-400m water depth may be explained by ocean temperature-controlled gas hydrate instabilities at the shelf break, but additional processes are required to explain seepage in permanently cold waters at depths >1000m. We discuss the influence of tectonic stress on seepage evolution along the similar to 100km long hydrate-bearing Vestnesa Ridge in Fram Strait. High-resolution P-Cable 3-D seismic data revealed fine-scale (>10m width) near-vertical faults and fractures controlling seepage distribution. Gas chimneys record multiple seepage events coinciding with glacial intensification and active faulting. The faults document the influence of nearby tectonic stress fields in seepage evolution along this deepwater gas hydrate system for at least the last similar to 2.7Ma.
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