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