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Gas seepage on the sea floor of Okinawa Trough Miyako Section
Luan, XW; Qin, YS
2005-07-01
发表期刊CHINESE SCIENCE BULLETIN
ISSN1001-6538
卷号50期号:13页码:1358-1365
文章类型Article
摘要A marine geophysical survey was carried out, on the RN Science 1 of the Institute of Oceanography, Chinese Academy of Sciences (IOCAS), in 2000, at the Miyako Section of Okinawa Trough. Here we present seismic and acoustic evidence of a gas seep on the sea floor on the western part of the Okinawa Through, near the lower slope of the East China Sea Slope and discuss the possibility of related formation of gas hydrate. A gas column reflection was observed in echo-sounder data above a section where the sea floor reflector was missing, on both the echo-sounder and the seismic data for line H14. The seismic data also show an acoustic curtain reflection and a turbidity reflection at this section. These anomalies are the evidence of the existence of a gas seep, which occupies an area 2.2 km in diameter. Based on the acoustic curtain on line H14, we believe that the amount of gas contained in the sediments below the gas seep is larger than 1 % by volume of sediment. Tectonically, the gas seep developed in a small basin controlled by basement uplift in the north, south and east. The thickness of the sediment layer can be greater than 3.5 km. A mud diapir structure was found in layer D beneath the gas seep. Over-pressure may occur due to the large sediment thickness and also the tectonic basement uplift in the north, south, and east. The mud diapir could be the preferential pathway for methane-rich fluids. The acoustic curtain may indicate that free gas related to the gas seep can be formed on the sea floor. We also note that the layer above the acoustic curtain on profile H14 may contain gas hydrate.; A marine geophysical survey was carried out, on the RN Science 1 of the Institute of Oceanography, Chinese Academy of Sciences (IOCAS), in 2000, at the Miyako Section of Okinawa Trough. Here we present seismic and acoustic evidence of a gas seep on the sea floor on the western part of the Okinawa Through, near the lower slope of the East China Sea Slope and discuss the possibility of related formation of gas hydrate. A gas column reflection was observed in echo-sounder data above a section where the sea floor reflector was missing, on both the echo-sounder and the seismic data for line H14. The seismic data also show an acoustic curtain reflection and a turbidity reflection at this section. These anomalies are the evidence of the existence of a gas seep, which occupies an area 2.2 km in diameter. Based on the acoustic curtain on line H14, we believe that the amount of gas contained in the sediments below the gas seep is larger than 1 % by volume of sediment. Tectonically, the gas seep developed in a small basin controlled by basement uplift in the north, south and east. The thickness of the sediment layer can be greater than 3.5 km. A mud diapir structure was found in layer D beneath the gas seep. Over-pressure may occur due to the large sediment thickness and also the tectonic basement uplift in the north, south, and east. The mud diapir could be the preferential pathway for methane-rich fluids. The acoustic curtain may indicate that free gas related to the gas seep can be formed on the sea floor. We also note that the layer above the acoustic curtain on profile H14 may contain gas hydrate.
关键词Okinawa Trough Gas Seepage Evidences Formation Gas Hydrate
学科领域Multidisciplinary Sciences
DOI10.1360/04wd0257
收录类别SCI
语种英语
WOS记录号WOS:000231858000012
引用统计
被引频次:15[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/3744
专题海洋地质与环境重点实验室
作者单位Chinese Acad Sci, Inst Oceanog, Qingdao 266071, Peoples R China
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GB/T 7714
Luan, XW,Qin, YS. Gas seepage on the sea floor of Okinawa Trough Miyako Section[J]. CHINESE SCIENCE BULLETIN,2005,50(13):1358-1365.
APA Luan, XW,&Qin, YS.(2005).Gas seepage on the sea floor of Okinawa Trough Miyako Section.CHINESE SCIENCE BULLETIN,50(13),1358-1365.
MLA Luan, XW,et al."Gas seepage on the sea floor of Okinawa Trough Miyako Section".CHINESE SCIENCE BULLETIN 50.13(2005):1358-1365.
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