1887

Abstract

The Nankai-Trough, which is located south of the main island of Honshu, Japan and extends 900 km offshore, is a<br>subduction zone with large amounts of deformed trench sediments with seismic activity and a good example of an<br>accretionary prism. At extreme ocean depths, water forms ice that has, in some instances, trapped methane in its crystalline<br>lattice, forming gas hydrates so that the Nankai-Trough contains a large amount of gas hydrate formations.

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/content/papers/10.3997/2214-4609-pdb.280.iptc14441_noPW
2012-02-07
2024-04-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.280.iptc14441_noPW
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