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- W2015952375 abstract "Gas hydrates reported in Green Canyon Block 184/185 are associated with an acoustically amorphous mound delineated on high resolution geophysical profiles. This elliptical mound is orientated parallel to prominent fault trends and is connected at depth with a regional chaotic seismic facies. Using this structure as a model, the location of gas hydrates was predicted from geohazard data in Mississippi Canyon Block 798. Structures of similar acoustic character and geologic setting are also found in Ewing Bank Blocks 873 and 874 in water depths too shallow for hydrate formation. The presence of gassy sediments combined with the common elements in the geologic settings as defined by high resolution geophysical profiles indicates that the acoustically amorphous structures are the extrusions of gassy muds from relatively shallow depths. These structures fit into the continuum between the mud diapir and mud volcano classifications. At the seafloor these mud mounds provide the sites for the generation of authigenic carbonates and, when in a deepwater setting, the sites for gas hydrate formation." @default.
- W2015952375 created "2016-06-24" @default.
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- W2015952375 date "1989-01-01" @default.
- W2015952375 modified "2023-09-27" @default.
- W2015952375 title "Gas Hydrates and Their Association With Mud Diapir/Mud Volcanoes on the Louisiana Continental Slope" @default.
- W2015952375 doi "https://doi.org/10.4043/5941-ms" @default.
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