supported by the Young Science and Technology Leader Training Plan Project of Jiangxi Bureau of Geology(Grant No.2024JXDZKJRC01);the Key Laboratory of Ionic Rare Earth Resources and Environment,Ministry of Natural Resources of the People's Republic of China(Grant No.2022IRERE101);the National Key R&D Program of China(Grant No.2020YFA0406400);the Jiangxi Geological Survey Project(Grant Nos.20210041 and 20242001)。
The Tieshanlong ore field is an important part of the Nanling Range,which is famous worldwide for its W-Sn mineralization.Notably,the mineralization age of the Tieshanlong ore field is not well constrained,and our fie...
financially supported by the National Natural Science Foundation of China(Grant Nos.92162210,42172096 and 41773028).
There are two factors,source composition and magmatic differentiation,potentially controlling W-Sn mineralization.Which one is more important is widely debated and may need to be determined for each individual deposit...
financially supported by a Key Project of the National Nature Science Foundation of China(Grant No.41830426);a National Key R&D Program of China Grant(No.2016YFC0600205)。
South China is endowed with copious wolframite-quartz vein-type W deposits that provide a significant contribution to the world‘s tungsten production.Mineralization is spatially associated with highly evolved granite...
supported by CGS grants(Item Number: 121201053303, 1212010881305, 1212011120811 and 1212011402450)
1 Introduction Massive tungsten-tin,rare and rare earth metals ore deposits were formed with the widespread granite magmatic activity in early Yanshanian period in the eastern Nanling region.Recent studies indicate th...
supported by China Geological Survey (1212011120813; 1212011120811; 1212010881305; 1212010533003;12120114015701 and DD20160037)
1 Introduction Nanshankeng tungsten-tin polymetallic mine,which is located in the eastern Nanling metallogenic belt,is newly discovered by geological investigation and evaluation with prospecting potential(Xiao et
financially supported by the National Key Basic Research Program (Grant2012CB416704) from the Ministry of Science and Technology, China;grant No. 40772063 from the National Natural Science Foundation of China;the Program of Excellent Young Scientists from the Ministry of Land and Resources (200809);Geological Survey Program Grant 1212010561603-2 from the China Geological Survey
Previous studies have obtained some petrogenetic and metallogenic chronological data with SHRIMP (sensitive high-resolution ion microprobe) zircon U-Pb, zircon LA-ICPMS (laser-ablation-inductively coupled plasma ma...
supported by the National Key Basic Research Program(2012CB416700,2007CB411408),a special fund managed by the State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,and the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences in Wuhan
Mesozoic granitic intrusions are widely distributed in the Nanling region, South China. Yanshanian granites are closely connected with the formation of tungsten deposits. The Xihuashan granite is a typical representat...
The present study is supported by the State Key Fundamental Research Project(Grant No.G1999043209);National Natural Science Foundation of China(Grant No.40132010).
Affected by the compressive stress from the South-Central (Indo-China) Peninsula, the Indosinian orogenesis, characterized by collision, thrust and uplifting, took place inside the South China Plate during 250-230 M...
The Nanling region is an important nonferrous and rare metal metallogenic province in South China, in which most of the deposits are related to granitoids in genesis. It covers southern Hunan, southern Jiangxi, Guangx...