Metallogenic background and metallogenesis of Qiaohuote copper deposit, Western Tianshan Mountains
文献类型:期刊论文
作者 | Zhang Xi1,2; Fan JunJia3,4; Gao Jun1; Dong LianHui1,5; Jiang Tuo1,2; Qian Qing1 |
刊名 | ACTA PETROLOGICA SINICA
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出版日期 | 2012-07-01 |
卷号 | 28期号:7页码:2057-2073 |
关键词 | VMS copper deposits Metallogenic background Metallogenesis Qiaohuote copper deposit Western Tianshan |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | In this study, we research the major, trace element and Sr-Nd isotopic characteristics of volcanic host rocks, mineralized rocks, and ores of Qiaohuote copper deposit located in the Southeast of Yili block, Western Tianshan Mountains. We also conducted in situ zircon U-Pb LA-ICP-MS dating of the diabase, which intruded into the volcanic host rocks of Qiaohuote copper deposit. It is inferred that the volcanic rocks which are mostly composed of calc-alkaline andesitic volcanic rocks are interpreted as the derivatives of a mantle source modified by subduction zone fluids derived from the northward subducted Southern Tianshan oceanic slab in an island back-arc extensional environment. Laser ablation-ICPMS (LA-ICPMS) U-Pb zircon ages of 281.0 +/- 1.9Ma were obtained for diabase. The data presented here in conjunction with previously published data suggest that it was an island arc environment as the northward subduction of Southern Tianshan Ocean during Ordovician or even earlier in Qiaohuote region, and I-type granodiorite formed during Late Ordovician(ca. 450Ma). The host rocks of Qiaohuote deposit formed by the persistent subduction of Southern Tianshan Ocean during Middle-Late Silurian (ca. 430Ma), and meanwhile the volcanic exhalation-sedimentation, which was contemporaneous with the submarine volcanic rocks, produced the primary mineralization of the Qiaohuote copper deposit. Afterward,the ore bodies and host rocks were reworked and overprinted intensively by structures corresponding with the overall collisional orogenic process of the Western Tianshan during Late Carboniferous and Early Permian, the island arc crashed and fitted with the Central Tianshan block as then the diabase intruded into the host volcanic rocks (281Ma). The Qiaohuote copper deposit is a volcanic exhalation and sedimentation-structural reworking and overprinting type deposit, which formed by complicated processes involving the subduction and closing of Southern Tianshan Ocean and the accretionary orogenic process of Western Tianshan. |
WOS关键词 | RARE-EARTH-ELEMENTS ; PALEOZOIC TECTONIC EVOLUTION ; HYDROTHERMALLY ALTERED ROCKS ; HIGH-FIELD-STRENGTH ; ISLAND-ARC BASALTS ; TRACE-ELEMENT ; SULFIDE DEPOSITS ; VOLCANIC-ROCKS ; ISOTOPIC EVIDENCE ; PROPAGATING-RIFT |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000306631600009 |
出版者 | SCIENCE PRESS |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/84658] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Zhang Xi |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 3.CNPC, Res Inst Petr Explorat & Dev, State Key Lab Enhanced Oil Recovery, Beijing 100083, Peoples R China 4.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China 5.Bur Geol & Mineral Resources Dev Xinjiang, Urumqi 830000, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang Xi,Fan JunJia,Gao Jun,et al. Metallogenic background and metallogenesis of Qiaohuote copper deposit, Western Tianshan Mountains[J]. ACTA PETROLOGICA SINICA,2012,28(7):2057-2073. |
APA | Zhang Xi,Fan JunJia,Gao Jun,Dong LianHui,Jiang Tuo,&Qian Qing.(2012).Metallogenic background and metallogenesis of Qiaohuote copper deposit, Western Tianshan Mountains.ACTA PETROLOGICA SINICA,28(7),2057-2073. |
MLA | Zhang Xi,et al."Metallogenic background and metallogenesis of Qiaohuote copper deposit, Western Tianshan Mountains".ACTA PETROLOGICA SINICA 28.7(2012):2057-2073. |
入库方式: OAI收割
来源:地质与地球物理研究所
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