SKARN

作品数:58被引量:169H指数:7
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相关领域:天文地球更多>>
相关作者:成永生更多>>
相关机构:中南大学中国科学院更多>>
相关期刊:《地学前缘》《矿物学报》《Science Bulletin》《Science China Earth Sciences》更多>>
相关基金:国家自然科学基金国家重点基础研究发展计划高等学校学科创新引智计划中国博士后科学基金更多>>
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Geochemistry and geochronology of multi-generation garnet:New insights on the genesis and fluid evolution of prograde skarn formation被引量:2
《Geoscience Frontiers》2023年第1期360-371,共12页Gaobin Chu Huayong Chen Shitao Zhang Yu Zhang Jiamin Cheng 
the Guangdong Major Projects of Basic and Applied Research(2019B030302013);the National Natural Science Foundation of China(NSFC Projects Nos.42102064,42173065 and 41725009);the China Postdoctoral Science Foundation(2021M693188).
Origin of garnet in skarn(magmatic vs.hydrothermal)and the prograde skarn fluid evolution are still controversial.Two generations of garnet(Grt1,Grt2)were identified at the Tongshankou deposit:Grt1 is anisotropic with...
关键词:Multi-generation garnet Mineral chemistry LA-ICP-MS U-Pb dating Fluid evolution Prograde skarn 
Geochronology and geochemistry of the Donglufang porphyry-skarn Mo-Cu deposit in the southern Yidun Terrane and their geological significances被引量:4
《Geoscience Frontiers》2018年第5期1433-1450,共18页Wenyan He Shixiong Xie Xudong Liu Xue Gao Yanlu Xing 
financially supported by the National Basic Research Program of China (No. 2015CB452605);the Natural Science Foundation of China (No. 41602089);Fundamental Research Funds for the Central Universities (No. 20170713174019)
The newly-discovered Donglufang Moe Cu porphyry-skarn deposit is located in the southern Yidun Terrane, southeast Tibet, with more than 80 million tonnes(Mt) of reserves(grading 0.15 wt.% Mo and0.48 wt.% Cu) hosted in...
关键词:Late cretaceous Mo-Cu METALLOGENESIS MOLYBDENITE RE-OS GEOCHRONOLOGY U-Pb zircon dating Yidun TERRANE 
Structure of the Panzhihua intrusion and its Fe-Ti-V deposit,China被引量:4
《Geoscience Frontiers》2013年第5期571-581,共11页Arnaud Pecher Nicholas Arndt Alexander Jean Arthur Bauville Clement Ganino Charlotte Athurion 
supported by a Famous overseas professor project MS2011ZGDZ[BJ]019 through China University of Geosciences (Beijing)and by the USA NSF "Continental Geodynamics" program;Geologists from the Panzhihua mining company are thanked for their logistic support
The Panzhihua intrusion in southwest China is part of the Emeishan large igneous province and host of a large Fe-Ti-V ore deposit.In previous interpretations it was considered to be a layered,differentiated sill with ...
关键词:Fe-Ti-V deposit INTRUSION STRUCTURE SKARN Tectonics 
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