Metallogenic systems and belts developed on the late Paleozoic continental margin in Xinjiang.
文献类型：期刊论文
| 作者 | Zhang LianChang; Xia Bin; Niu HeCai; Li WenQian; Fang WeiXuan; Tang HongFeng; Wan Bo |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2006-05-01 |
| 卷号 | 22期号:5页码:1387-1398 |
| 关键词 | Late Paleozoic Continent Margin Continent Accretion Metallogenic System Metallogenic Belt Central Asia Orogenic Belt |
| ISSN号 | 1000-0569 |
| 文献子类 | Article |
| 英文摘要 | The northern Xinjiang, located in centre position of Central Asia orogenic belt (CAOB), are characterized by intense continent accretion, tectonic and magma activity, abundant mineral resources in late Paleozoic. The metallogenic processes on the continental margin in late Palcozoic have two main stages including early-middle Devonian and early Carboniferous. Based on studies of regional geology and tectonic evolution, mineralization type of metal deposits, the metallogenic systems on late Paleozoic continent margin are divided into three types: (1) marine volcanics-basin-fluids system in active continent margin; (2) are volcanic-intrusive system in active margin; (3) sediment basin-hydrothermal activity system in passive continent margin. On the basis of the metallogenic systems, metallogenic belts in northern Xinjiang are divided into: (1) volcanic massive sulfide (VMS-type) metallogenic belt in late Paleozoic active continent margin, southern Altaid; (2) porphyry copper-gold metallogenic belt in Almantai-Kalaxianer arc, southern Altaid-eastern Junggar; (3) porphyry Cu and volcanic hydrothermal Cu-Zn (Fe) metallogenic belt in active continent margin, eastern Tianshan; (4) porphyry Cu and hydrothermal Au metallogenic belt in intra-oceanic subduction, western Junggar; (5) porphyry Cu and hydrothermal. An metallogenic belt in active continent margin, western Tianshan; (6) SEDEX-type Pb-Zn-Cu metallogenic belt in passive continent margin of northwestern Tarim basin. This paper suggest that large and giant ore deposits can reflect the geologic and tectonic evolution, relations between the continent accretion and metallogenic processes are main researching contents of metallogenic system. |
| WOS关键词 | EASTERN TIANSHAN ; TECTONIC EVOLUTION ; SOUTHERN MARGIN ; COPPER-DEPOSITS ; VOLCANIC-ROCKS ; CRUSTAL GROWTH ; CENTRAL-ASIA ; NW CHINA ; GOLD ; MINERALIZATION |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000239220600027 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/66095]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Zhang LianChang |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China 3.Chinese Acad Sci, Inst Geochem, Guiyang 55002, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang LianChang,Xia Bin,Niu HeCai,et al. Metallogenic systems and belts developed on the late Paleozoic continental margin in Xinjiang.[J]. ACTA PETROLOGICA SINICA,2006,22(5):1387-1398. |
| APA | Zhang LianChang.,Xia Bin.,Niu HeCai.,Li WenQian.,Fang WeiXuan.,...&Wan Bo.(2006).Metallogenic systems and belts developed on the late Paleozoic continental margin in Xinjiang..ACTA PETROLOGICA SINICA,22(5),1387-1398. |
| MLA | Zhang LianChang,et al."Metallogenic systems and belts developed on the late Paleozoic continental margin in Xinjiang.".ACTA PETROLOGICA SINICA 22.5(2006):1387-1398. |
入库方式： OAI收割
来源：地质与地球物理研究所
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