An application of rock physics modeling to quantify the seismic response of gas hydrate-bearing sediments in Makran accretionary prism, offshore, Pakistan
Accretionary wedge
Clathrate hydrate
Amplitude versus offset
Saturation (graph theory)
Continental Margin
DOI:
10.1007/s12303-015-0044-z
Publication Date:
2015-09-22T19:55:59Z
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