Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5781943 | Marine and Petroleum Geology | 2017 | 13 Pages |
Abstract
The Dongsha Basin, circling Dongsha Island that is amid the northern margin of the South China Sea, is characterized by thin (â¼0.5Â km) Cenozoic sediments veneering on thick (up to 5Â km) Mesozoic strata. Recently, several geophysical and geological surveys, including multiple channel reflection seismic, sub-bottom profiling and benthic dredging, have been conducted on the slope southwest to the Dongsha Island, where the water depth varies from 400Â m to 2000 m. A novel discovery is numerous submarine mud volcanoes of various sizes over there, typically 50-200Â m high and 0.5-5Â km wide. Geophysical profiles document their unusual features, e.g., roughly undulating seafloor, high-amplitude seabed reflectivity, foggy hyperbolic diffractions up to 50Â m in water column above seabed, and internal reflection chaos and wipe-out down to 2-3Â km level or deeper below the seabed. Benthic dredging from the mud volcanoes gives abundant faunas of high diversity, e.g., scleractinian (stony coral), gorgonian, black coral, thiophil tubeworm, glass sponge, bryozoan etc., indicating booming chemosynthetic community, among which the Lophelia pertusa-like coral and the Euretidae-like glass sponges are the first reports in the South China Sea. Concomitantly with them, there are also abundant authigenic carbonate nodules and slabs, raw, brecciated and breccias with bio-clasts congregation. Besides, there coexist massive mudflows and allogenic coarse-grained quartz, feldspar and tourmaline most likely brought out by mud volcanism. Geochemical analysis of the bottom water samples give dissolved methane concentration up to 4 times higher than the background average. These results lend comprehensive evidences for the ongoing and historical mud volcanism. The escaping methane gas is inferred to source mainly from the Mesozoic strata. Occupying a large province of the deep water slope, ca. 1000Â km2 or more, the mud volcanoes is prospective for gas hydrate and natural gas for the Dongsha Basin.
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Authors
Yan Pin, Wang Yanlin, Liu Jun, Zhong Guangjian, Liu Xingjian,