The Gas-Source Study of Gas Hydrates in Wuli and Muli Permafrost Region of Qinghai-Tibet Plateau  

作　　者：GONG Jianming ZHANG Li ZHANG Min 

机构地区：[1]Key Laboratory of Marine Hydrocarbon Resources andEnvironmental Geology, MLR, Qingdao, Shandong 266071 [2]Qingdao Institute of Marine Geology, Qingdao, Shandong 266071 [3]Guangzhou Marine Geological Survey, MLR, Guangzhou Guangdong 510760 [4]School of Earth Environment and Water Resources, Yangtze University, Wuhan Hubei 430100

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A01期443-445,共3页地质学报（英文版）

摘　　要：1 Introduction Muli permafrost region is located in the south Qilian Mountain of the northem Qinghai-Tibet Plateau, which belongs to Kunlun Mountain terrain in geo-tectonics （Fig.l）. The average elevation of the region is 4100m and the thickness of the permafrost is about 60 to 100m （ZHOU Youwu, etc, 2000; PAN Yulu, etc, 2008）.1 Introduction Muli permafrost region is located in the south Qilian Mountain of the northem Qinghai-Tibet Plateau, which belongs to Kunlun Mountain terrain in geo-tectonics （Fig.l）. The average elevation of the region is 4100m and the thickness of the permafrost is about 60 to 100m （ZHOU Youwu, etc, 2000; PAN Yulu, etc, 2008）.

分 类 号：P642.14[天文地球—工程地质学] P618.13[天文地球—地质矿产勘探]