supported by the National Key R&D Program of China Ministry of Science and Technology(No.2018YFC0604005);the China Geological Survey through Geological Survey Project Grant(No.1212011085527).
The Wutonggou iron deposit is located in the well-known iron metallogenic belt in the eastern Tianshan,NW China,and has been regarded as a sedimentary iron deposit.Although hydrothermal overprinting could play indispe...
supported by the National Natural Science Foundation of China(91955203,91755101,41872121,41302166);the fund from the Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources(J1901-20-4);Scientific Research Fund of the Institute of Geology,Chinese Academy of Geological Sciences(S2003);the Basic Research Project of Chinese Academy of Geological Sciences(JYYWF20180903,JYYWF20182103);the project of China Geological Survey(DD20190006,DD20190060).
The Pamir Plateau comprises a series of crustal fragments that successively accreted to the Eurasian margin preceded the India-Asia collision,is an ideal place to study the Mesozoic tectonics.The authors investigate t...
supported by the Chinese Academy of Geological Sciences (CAGS) Research Fund (Nos. J1623, YYWF201708);the National Natural Science Foundation of China (Nos. 41502196, 41472198, 41872224, 41430212);the State Scholarship Fund (No. 201809110029);the China Geological Survey (No. DD20160022)
The Yardoi dome is located in the eastern end of the northwest-southeast extending North Himalayan domes (NHD). The dome exposes a granite pluton in the core and three lithologictectonic units separated by the upper d...