中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Revisit and comparative analysis of the typical graphite deposits in the Paleoproterozoic khondalite series, western North China Craton: Implications for genesis, depositional environment and prospecting potential

文献类型:期刊论文

作者Zhong, Yan1,2; Ma, Xu-Dong3; Li, Huai-Kun1,2; Zhai, Ming-Guo4
刊名ORE GEOLOGY REVIEWS
出版日期2019-06-01
卷号109页码:370-380
关键词Phaneritic graphite deposits Khondalite series Fengzhen Group North China Craton
ISSN号0169-1368
DOI10.1016/j.oregeorev.2019.04.023
英文摘要The phaneritic graphite deposits in the western North China Craton can be delineated into an E-W trending belt, which is consistent with the Paleoproterozoic khondalite series. To interpret why graphite is not ubiquitous among the Paleoproterozoic supracrustal rocks, we revisit and comparatively analyze the typical graphite deposits in the Paleoproterozoic khondalite series employing sequence stratigraphy, chronology, tectonic deformation and metamorphism for the khondalite series and carbon isotope analysis for graphite. Our renewed profile of the western graphite belt (WGB) reveals the following: 1) A greater abundance of organic matter was trapped within the lower part of the khondalite series than in the middle and upper parts; consequently, all the known deposits are restricted to the lower part of the khondalite series. 2) As the protolithic basin evolved from a passive continental margin into an active continental margin, subduction-related magmatism provided the influx of heat needed to transform the organic matter into amorphous graphite. 3) Continental collision-induced high-grade metamorphism and associated magmatism finally reworked the original amorphous graphite into the present-day phaneritic graphite deposits.
WOS关键词ZIRCON U-PB ; TECTONIC HISTORY ; CARBON ISOTOPES ; METASEDIMENTARY ROCKS ; COMPLEX CONSTRAINS ; HELANSHAN COMPLEX ; THERMAL EVOLUTION ; METAMORPHIC ROCKS ; MAFIC GRANULITES ; DETRITAL ZIRCONS
资助项目China Geological Survey[DD20190075] ; China Geological Survey[DD20190359] ; National Natural Science Foundation of China[41572174]
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
WOS记录号WOS:000472686500021
出版者ELSEVIER SCIENCE BV
资助机构China Geological Survey ; China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Geological Survey ; China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Geological Survey ; China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Geological Survey ; China Geological Survey ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/92687]  
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Ma, Xu-Dong
作者单位1.China Geol Survey, Tianjin Ctr, Tianjin 300170, Peoples R China
2.China Geol Survey, Precambrian Res Ctr, Tianjin 300170, Peoples R China
3.Chinese Acad Geol Sci, MNR Key Lab Metallogeny & Mineral Assessment, Inst Mineral Resources, Beijing 100037, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Zhong, Yan,Ma, Xu-Dong,Li, Huai-Kun,et al. Revisit and comparative analysis of the typical graphite deposits in the Paleoproterozoic khondalite series, western North China Craton: Implications for genesis, depositional environment and prospecting potential[J]. ORE GEOLOGY REVIEWS,2019,109:370-380.
APA Zhong, Yan,Ma, Xu-Dong,Li, Huai-Kun,&Zhai, Ming-Guo.(2019).Revisit and comparative analysis of the typical graphite deposits in the Paleoproterozoic khondalite series, western North China Craton: Implications for genesis, depositional environment and prospecting potential.ORE GEOLOGY REVIEWS,109,370-380.
MLA Zhong, Yan,et al."Revisit and comparative analysis of the typical graphite deposits in the Paleoproterozoic khondalite series, western North China Craton: Implications for genesis, depositional environment and prospecting potential".ORE GEOLOGY REVIEWS 109(2019):370-380.

入库方式: OAI收割

来源:地质与地球物理研究所

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