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《Chinese Journal of Geophysics》 2011-01
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Study on the characteristics of gas hydrate stability zone in the Muli permafrost,Qinghai——comparison between the modeling and drilling results

JIN Chun-Shuang~1,QIAO De-Wu~1,LU Zhen-Quan~(2*),ZHU You-Hai~2,ZHANG Yong-Qin~3,WEN Huai-Jun~4,LI Yong-Hong~4,WANG Ping-Kang~2,HUANG Xia~2 1 Strategic Research Center for Oil and Gas Resources,Ministry of Land and Resources,Beijing 100034,China 2 Institute of Mineral Resources,CAGS,Beijing 100037,China 3 Institute of Exploration Techniques,CAGS,Lang fang of Hebei 065000,China 4 Qinghai No,105 Coal Geological Exploration Team,Xining 810007,China  
Based on gas composition and temperature measurements in the course of field drilling, the upper and lower depths of gas hydrate stability zone are calculated by modeling in the Muli permafrost,Qinghai,then the modeling results are compared with the drilling results.The modeling results show that the upper depth of gas hydrate stability zone is 148.8~122.7 m and the lower depth of gas hydrate stability zone is 324.6~354.8 m,with the thickness of gas hydrate stability zone of 175.8~232.2 m;the drilling results indicate that gas hydrate and its related indications occur at the interval of 133~396 m.These two types of results are comparable and thus are basically accordant,suggesting that the modeling can serve as a prediction of the upper and lower depths of gas hydrate stability zone.Gas composition,depth of permafrost, thermal gradients above and below the base of permafrost are sensitive factors affecting the upper and lower depths of gas hydrate stability zone in the Muli permafrost.
【Fund】: 国家重点基础研究发展计划项目(2009CB219501);; 国家自然科学基金项目(41073040);; 中国地质大调查项目(1212010818055);; 中央公益性科研院所基本科研业务费专项基金项目(K1003)联合资助
【CateGory Index】: P618.13
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