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作 者:DONG Ji’en ZHANG Huiqing WANG Peng LI Hua YE Gaofeng YU Xiaoliang LI Jie
机构地区:[1]Qinghai Geological Survey,MNR Technology Innovation Center for Exploration and Exploitation of Strategic Mineral Resources in Plateau Desert Region,Xining 810000,China [2]School of Geophysics and Information Technology,China University of Geosciences,Beijing 100083,China
出 处:《Acta Geologica Sinica(English Edition)》2024年第S01期18-21,共4页地质学报(英文版)
基 金:supported by Qinghai Provincial Association for Science and Technology Youth Science and Technology Talent Support Project(Grant No.2023QHSKXRCTJ47);Exploration Foundation of Qinghai Province(Grant No.2023085029ky004)。
摘 要:Introduction The East Kunlun Orogenic Belt is located in the northeastern part of the Qinghai–Tibet Plateau(Li et al.,2007),stretching from the East Kunlun to the Elashan area in an east–west direction(Guo et al.,2018).It is an important part of the Central Orogenic Belt(Xiong et al.,2023).It is considered one of the important gold mineralization regions in the Tethys tectonic domain(Norbu et al.,2023)and an essential potential base for mineral resources in China.Wulonggou and Gouli gold mines have been discovered successively,earning the reputation of the"Golden Belt of Qinghai Province"(Feng et al.,2004;He et al.,2023).
关 键 词:electromagnetic method altered rock-type gold deposits Mailong mining area East Kunlun metallogenic belt
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