A preliminary study of the gas hydrate, stability zone in the South China Sea

被引:0
|
作者
Jin, CS [1 ]
Wang, JY
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
[2] Minist Land & Resources, Strateg Res Ctr Oil & Gas Resources, Beijing 100034, Peoples R China
关键词
South China Sea; gas hydrate; stability zone; geothermal gradient; sea-bottom temperature;
D O I
暂无
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Based on the analysis of sea-bottom temperature and geothermal gradient, and by means of the phase boundary curve of gas hydrate and the sea-bottom temperature versus water depth curve in the South China Sea, this paper studies the temperature and pressure conditions for gas hydrate to keep stable. In a marine environment, methane hydrate keeps stable at water depths greater than 550 m in the South China Sea. Further, the thickness of the gas hydrate stability zone in the South China Sea was calculated by using the phase boundary curve and temperature-depth equations. The result shows that gas hydrate have a better perspective in the southeast of the Dongsha Islands, the northeast of the Xisha Islands and the north of the Nansha Islands for thicker stability zones.
引用
收藏
页码:423 / 428
页数:6
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