Surface expression of fluid venting at the toe of the Nankai wedge and implications for flow paths
Cold seeps have been observed with manned submersibles at many sites on the Tokai margin. Most sites are found on the hanging wall of major thrust faults, within 1–2 km of their outcrop. Few sites relate to purely erosional features. This relationship between thrusting and venting may be explained e...
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Veröffentlicht in: | Marine geology 2002-07, Vol.187 (1-2), p.119-143 |
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