中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Multiple skarn generations related to composite leucogranites in the Cuonadong Sn-W-Be deposit, Himalaya

文献类型:期刊论文

作者He, Chang-Tong2,3; Qin, Ke-Zhang2,3; Zhao, Jun-Xing2; Evans, Noreen J.4; Li, Jin-Xiang5; Zhou, Qi-Feng1; Li, Guang-Ming2,3
刊名ORE GEOLOGY REVIEWS
出版日期2022-11-01
卷号150页码:15
ISSN号0169-1368
关键词Cuonadong Sn -W -Be district Composite leucogranites Multigenerational skarns titanite-monazite-columbite U-(Th)-Pb dating Tethyan Himalaya
DOI10.1016/j.oregeorev.2022.105161
英文摘要The newly discovered Cuonadong Sn-W-Be skarn deposit is related to fractionated leucogranitic intrusions hosted in the Cenozoic Himalayan gneiss dome, Tibet, however, temporal and genetic relationships between composite magmatism, skarn and mineralization remain unclear. Based on age and compositional features, three types of titanite were identified: Ttn1 and Ttn2 in the diopside-dominated skarn and adjacent greisenized granitic dike, and Ttn3 (subdivided into Ttn3a and 3b) in the Sn-mineralized garnet skarn. Ttn1 has a higher Ti content and yielded a U-Pb age of -35 Ma, consistent with the U-Pb ages of monazite from the pegmatitic granite (35.0 +/- 0.6 Ma). Younger, recrystallized Ttn2 (-28-27 Ma) is characterized by higher Al, F, Ta, Nb, Sn and Y contents and was likely formed by interaction between early Ttn1 and late fluids as indicated by the monazite U-Pb age of two-mica granite (28.8 +/- 0.3 Ma). These two types of hydrothermal titanite are confined to the Oligocene unmineralized skarn and adjacent greisenized granitic dike.Titanite from the garnet-bearing Sn-mineralized skarn (Ttn3) provides the age of mineralization (16.8 +/- 1.6 Ma), slightly younger than the emplacement age of the Miocene granite (monazite U-Pb age: 19.9 +/- 0.3 Ma and columbite: 19.0 +/- 0.4 Ma). The Sn-rich Ttn3b coexisting with garnet and interstitial cassiterite shows a deficit of Y and HREE and a high (Dy)N/(Yb)N ratio, implying that hydrothermal Sn metasomatism of Ttn3 occurred after garnet crystallization. Overall, our results shows that the Cuonadong multigenerational skarns were generated during three episodic magmatic-hydrothermal events, and mineralization occurred in the Miocene.
WOS关键词U-PB GEOCHRONOLOGY ; SOUTHERN TIBET ; TETHYAN HIMALAYA ; TRACE-ELEMENT ; CRUSTAL ANATEXIS ; GNEISS DOME ; POLYGENETIC TITANITE ; POLYMETALLIC DEPOSIT ; TECTONIC EVOLUTION ; DETACHMENT SYSTEM
资助项目Second Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0806] ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0802] ; Key Deployment Project of CAS[ZDRW-ZS-2020-4-1] ; Key Research Program of the Institute of Geology and Geophysics, CAS[IGGCAS-201902] ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology[6142A010104] ; SEG Student Research Grant[SRG 21-55] ; Society of Economic Geologists Foundation ; Chengdu Center of China Geological Survey
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
出版者ELSEVIER
WOS记录号WOS:000878182400002
资助机构Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Deployment Project of CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Key Research Program of the Institute of Geology and Geophysics, CAS ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; Pre-Research Foundation from Beijing Research Institute of Uranium Geology ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; SEG Student Research Grant ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Society of Economic Geologists Foundation ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey ; Chengdu Center of China Geological Survey
源URL[http://ir.iggcas.ac.cn/handle/132A11/107682]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Qin, Ke-Zhang
作者单位1.China Met Geol Bur, Inst Mineral Resources Res, Beijing 101300, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
4.Curtin Univ, Sch Earth & Planetary Sci, John de Laeter Ctr, Perth, WA 6845, Australia
5.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Environm, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
He, Chang-Tong,Qin, Ke-Zhang,Zhao, Jun-Xing,et al. Multiple skarn generations related to composite leucogranites in the Cuonadong Sn-W-Be deposit, Himalaya[J]. ORE GEOLOGY REVIEWS,2022,150:15.
APA He, Chang-Tong.,Qin, Ke-Zhang.,Zhao, Jun-Xing.,Evans, Noreen J..,Li, Jin-Xiang.,...&Li, Guang-Ming.(2022).Multiple skarn generations related to composite leucogranites in the Cuonadong Sn-W-Be deposit, Himalaya.ORE GEOLOGY REVIEWS,150,15.
MLA He, Chang-Tong,et al."Multiple skarn generations related to composite leucogranites in the Cuonadong Sn-W-Be deposit, Himalaya".ORE GEOLOGY REVIEWS 150(2022):15.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。