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
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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 |
DOI | 10.3190/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 |
推荐引用方式 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. |
入库方式: OAI收割
来源:地质与地球物理研究所
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