4.7 Article

Seismic quality factors across a bottom simulating reflector in the Makran Accretionary Prism, Arabian Sea

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MARINE AND PETROLEUM GEOLOGY
卷 28, 期 10, 页码 1838-1843

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ELSEVIER SCI LTD
DOI: 10.1016/j.marpetgeo.2011.03.013

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Seismic quality factor; Gas hydrates; Free-gas; Makran accretionary prism

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The hydrate-bearing sediments above the bottom simulating reflector (BSR) are associated with low attenuation or high quality factor (Q), whereas underlying gas-bearing sediments exhibit high attenuation. Hence, estimation of Q can be important for qualifying whether a BSR is related to gas hydrates and free-gas. This property is also useful for identifying gas hydrates where detection of BSR is dubious. Here, we calculate the interval Q for three submarine sedimentary layers bounded by seafloor, BSR, one reflector above and another reflector below the BSR at three locations with moderate, strong and no BSR along a seismic line in the Makran accretionary prism, Arabian Sea for studying attenuation (Q(-1)) characteristics of sediments. Interval Q for hydrate-bearing sediments (layer B) above the BSR are estimated as 191 +/- 11, 223 +/- 12, and 117 +/- 5, whereas interval Q for the underlying gas-bearing sediments (layer C) are calculated as 112 +/- 7, 107 +/- 8 and 124 +/- 11 at moderate, strong and no BSR locations, respectively. The large variation in Q is observed at strong BSR. Thus Q can be used for ascertaining whether the observed BSR is due to gas hydrates, and for identifying gas hydrates at places where detection of BSR is rather doubtful. Interval Q of 98 +/- 4, 108 +/- 5, and 102 +/- 5, respectively, at moderate, strong and no BSR locations for the layer immediately beneath the seafloor (layer A) show almost uniform attenuation. (C) 2011 Elsevier Ltd. All rights reserved.

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