中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Seafloor in-situ heat flow measurements in the deep-water area of the northern slope, South China Sea

文献类型:期刊论文

作者Li, YM ; Luo, XH ; Xu, X ; Yang, XQ ; Shi, XB
刊名CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
出版日期2010
卷号53期号:9页码:2161-2170
关键词The northern slope of the South China Sea Seafloor in-situ heat flow Thermal conductivity The temperature gradient Gas hydrates
ISSN号0001-5733
通讯作者liyamin05@scsio.ac.cn ; xbshi@scsio.ac.cn
中文摘要Seafloor heat flow data is the fundamental data for studying marine geodynamics and evaluating petroleum resource. Though resource of petroleum and gas hydrate is abundant in the deepwater areas of the northern slope of the South China Sea, there are very few heat flow sites. To investigate the geothermal distribution in the deepwater areas of the northern slope, which are thought to be advantaged areas for gas hydrates, a Jianyu-1 type heat flow probe was employed and 16 heat flow data in Xisha and Shenhu sea areas were obtained successfully. The results show that the heat flow of both Xisha Trough and Baiyun Sag is high. In Xisha Trough, except for one unreliable site, the temperature gradients in surface sediment of the other two sites are 105.3 and 99.9 degrees C . km(-1) respectively, and their heat flow values are 89 +/- 1 and 87 +/- 1 mW . m(-2), respectively. The temperature gradients of the 13 heat flows sites in the middle of Baiyun Sag range from 58.5 to 100.7 degrees C . km(-1), and except for 4 heat flows which are lower than 70 mW . m(-2), their heat flow values range from 75 +/- 2 to 101 +/- 4 mW . m(-2), which are generally higher than that previously obtained from the eastern part of Baiyun Sag. Analyses suggest that the high thermal regime in Xisha Trough and Baiyun Sag is related with high thermal background, and affected by latest active faults, diapiric structure, magma intrusion and heat fluid.
学科主题Geochemistry & Geophysics
收录类别SCI
原文出处SCIENCE CHINA PRESS
WOS记录号WOS:000282294600016
公开日期2011-07-03
源URL[http://ir.scsio.ac.cn/handle/344004/4306]  
专题南海海洋研究所_中科院边缘海地质重点实验室
推荐引用方式
GB/T 7714
Li, YM,Luo, XH,Xu, X,et al. Seafloor in-situ heat flow measurements in the deep-water area of the northern slope, South China Sea[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2010,53(9):2161-2170.
APA Li, YM,Luo, XH,Xu, X,Yang, XQ,&Shi, XB.(2010).Seafloor in-situ heat flow measurements in the deep-water area of the northern slope, South China Sea.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,53(9),2161-2170.
MLA Li, YM,et al."Seafloor in-situ heat flow measurements in the deep-water area of the northern slope, South China Sea".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 53.9(2010):2161-2170.

入库方式: OAI收割

来源:南海海洋研究所

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