| 兴蒙造山带中与古亚洲洋演化有关的成矿系统初步研究 |
| Received:November 03, 2021 Revised:April 14, 2022 点此下载全文 |
| 引用本文：ZHU YongFeng,ZHANG YunDi,JIANG JiuYang,LU GuoLong.2022.Study on ore-forming systems related with evolution of Paleo-Asian ocean in Xing-meng orogenic belt[J].Mineral Deposits,41(3):449~468 |
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| Author Name | Affiliation | | ZHU YongFeng | Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China | | ZHANG YunDi | Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China | | JIANG JiuYang | Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China | | LU GuoLong | Key Laboratory of Orogenic Belt and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China |
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| 基金项目:本文得到国家自然科学基金项目（编号：42072077）和国家重点研发计划（编号：2017YFC0601302）共同资助 |
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| 中文摘要:古亚洲洋演化过程中在兴蒙造山带中形成了大量金属矿床。早古生代早期，古亚洲洋向北俯冲，形成了奥陶纪多宝山-铜山斑岩Cu-Au成矿系统；早古生代晚期，古亚洲洋向南俯冲并形成了晚奥陶世白乃庙Cu-Mo-Au成矿系统和志留纪别鲁乌图海底喷流块状硫化物成矿系统。古亚洲洋在晚古生代早期向北俯冲，形成了晚泥盆世欧玉陶勒盖Cu-Au成矿系统。基本同时，古亚洲洋向南俯冲，形成了晚泥盆世哈达门沟Mo成矿系统。早石炭世，研究区构造体制从岛弧环境逐渐转变为陆内伸展环境，并在此过程中形成了豆荚状铬铁矿成矿系统和小型斑岩Mo-Cu成矿系统。 |
| 中文关键词:地质学 古亚洲洋 兴蒙造山带 斑岩矿床 多金属矿床 成矿系统 |
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| Study on ore-forming systems related with evolution of Paleo-Asian ocean in Xing-meng orogenic belt |
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| Abstract:Abundant metal deposits formed during the evolution of the Paleo-Asian ocean in the Xing-meng orogenic belt. The northward subductions of the Paleo-Asian ocean during the early Early Paleozoic formed the Ordovician Duobaoshan-Tongshan Cu-Au porphyry ore-forming system. The southward subductions of the Paleo-Asian ocean during the late Early Paleozoic formed the late Ordovician Bainaimiao Cu-Mo-Au ore-forming system and Silurian Bieluwutu VHMS ore-forming system. During the early Late Paleozoic, the northward subductions of the Paleo-Asian ocean formed the late Devonian Oyu Taolgoi porphyry Cu-Au ore-forming system. In the same period, the southward subductions of the Paleo-Asian ocean formed the late Devonian Hadamengou Mo ore-forming system. Tectonic pattern changed to extensional environment during Early Carboniferous periods, and formed podiform chromite and small porphyry Mo-Cu ore-forming systems. |
| keywords:geology Paleo-Asian ocean Xing-meng orogenic belt porphyry deposit polymetallic deposit ore-forming system |
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