中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mid-Late Paleozoic metallogenesis and evolution of the Chinese Altai and East Junggar Orogenic Belt, NW China, Central Asia

文献类型:期刊论文

作者Han, Chunming1; Xiao, Wenjiao1,2; Zhao, Guochun3; Su, Benxun1,3; Sakyi, Patrick Asamoah4; Ao, Songjian1; Wan, Bo1; Zhang, Jien1; Zhang, Zhiyong1; Wang, Zhongmei1
刊名JOURNAL OF GEOSCIENCES
出版日期2014
卷号59期号:3页码:255-274
关键词Chinese Altai East Junggar Central Asian Orogenic Belt Mid-Late Paleozoic metallogenesis
ISSN号1802-6222
DOI10.3190/jgeosci.173
文献子类Review
英文摘要The Chinese Altai-East Junggar collage in southern Altaids is one of the largest and most important metallogenic provinces in China. It is composed of five major types of Middle to Late Paleozoic metal deposits: (1) VMS Cu-Pb-Zn, (2) porphyry Cu-Au, (3) magmatic Cu-Ni-sulfide, (4) skarn Cu-Mo-Fe and (5) orogenic Au. Tectonically, the development of these metal deposits was closely associated with accretionary and convergent processes that occurred along the southern margin of the Central Asian Orogenic Belt (CAOB). The formation of the deposits involved three main stages, briefly described as follows: (i) Those formed during extensional back-arc volcanism along the Paleozoic active margin of the CAOB. They are Late Devonian to Early Carboniferous polymetallic volcanogenic massive sulfide deposits, together with some broadly contemporaneous Fe-Cu skarns, located in the accreted Qiongkuer-Talate Terrane in the western Altai; (ii) Carboniferous to Permian terrane accretion and arc magmatism, resulting in widespread metalliferous ores of different types such as copper-bearing porphyries and Alaskan-type Cu-Ni-PGE zoned ultramafic bodies developed in arcs in the Buerjin-Ertai and Erqis terranes, and Cu-Fe skarns formed in the Erqis flysch basin; (iii) Continuing accretion in the Permian leading to the development of the Dulate arc in the southern Altai associated with the formation of Cu-Mo skarns and orogenic-type gold vein systems. The Chinese Altai-East Junggar collage typically demonstrates the various classic metalliferous ores formed during the processes of subduction-accretion and arc generation.
WOS关键词ZIRCON U-PB ; PHANEROZOIC CRUSTAL GROWTH ; XINJIANG AUTONOMOUS REGION ; NORTHWESTERN CHINA ; TECTONIC EVOLUTION ; NORTHERN XINJIANG ; CONTINENTAL GROWTH ; ISOTOPIC EVIDENCE ; ORE DISTRICT ; IRON DEPOSIT
WOS研究方向Geology
语种英语
WOS记录号WOS:000341694500005
出版者CESKA GEOLOGICKA SPOLECNOST
资助机构National Natural Science Foundation(41190075 ; National Natural Science Foundation(41190075 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; Chinese State 973 projects(2014CB440801 ; Chinese State 973 projects(2014CB440801 ; Hong Kong RGC(7066/07P) ; Hong Kong RGC(7066/07P) ; 41230207 ; 41230207 ; 2007CB411307) ; 2007CB411307) ; 41272107) ; 41272107) ; National Natural Science Foundation(41190075 ; National Natural Science Foundation(41190075 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; Chinese State 973 projects(2014CB440801 ; Chinese State 973 projects(2014CB440801 ; Hong Kong RGC(7066/07P) ; Hong Kong RGC(7066/07P) ; 41230207 ; 41230207 ; 2007CB411307) ; 2007CB411307) ; 41272107) ; 41272107) ; National Natural Science Foundation(41190075 ; National Natural Science Foundation(41190075 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; Chinese State 973 projects(2014CB440801 ; Chinese State 973 projects(2014CB440801 ; Hong Kong RGC(7066/07P) ; Hong Kong RGC(7066/07P) ; 41230207 ; 41230207 ; 2007CB411307) ; 2007CB411307) ; 41272107) ; 41272107) ; National Natural Science Foundation(41190075 ; National Natural Science Foundation(41190075 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; Chinese State 973 projects(2014CB440801 ; Chinese State 973 projects(2014CB440801 ; Hong Kong RGC(7066/07P) ; Hong Kong RGC(7066/07P) ; 41230207 ; 41230207 ; 2007CB411307) ; 2007CB411307) ; 41272107) ; 41272107)
源URL[http://ir.iggcas.ac.cn/handle/132A11/86538]  
专题中国科学院地质与地球物理研究所
通讯作者Han, Chunming
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Peoples R China
3.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
4.Univ Ghana, Dept Earth Sci, Legon, Ghana
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GB/T 7714
Han, Chunming,Xiao, Wenjiao,Zhao, Guochun,et al. Mid-Late Paleozoic metallogenesis and evolution of the Chinese Altai and East Junggar Orogenic Belt, NW China, Central Asia[J]. JOURNAL OF GEOSCIENCES,2014,59(3):255-274.
APA Han, Chunming.,Xiao, Wenjiao.,Zhao, Guochun.,Su, Benxun.,Sakyi, Patrick Asamoah.,...&Wang, Zhongmei.(2014).Mid-Late Paleozoic metallogenesis and evolution of the Chinese Altai and East Junggar Orogenic Belt, NW China, Central Asia.JOURNAL OF GEOSCIENCES,59(3),255-274.
MLA Han, Chunming,et al."Mid-Late Paleozoic metallogenesis and evolution of the Chinese Altai and East Junggar Orogenic Belt, NW China, Central Asia".JOURNAL OF GEOSCIENCES 59.3(2014):255-274.

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来源:地质与地球物理研究所

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