Zircon LA-ICP-MS U-Pb Chronology of Magmatic Rock in the Baishantang Copper Polymetallic Deposit of Beishan Area, Northwest China
详细信息
- 责任者：Shan Liang (Faculty of Earth Science and Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Xu Rongke
- 刊名：Geology in China
- 出版年：2013
- 卷期：40(5)
- 关键词：斑岩铜矿床 ; porphyry copper deposit ; 铀—铅计时 ; U-Pb dating ; 西北地区 ; North West China
- 页码：p.1600-1611
- 图表：5 illus., 2 tables, 41 refs.
- 分类号：1001
- issnNo：ISSN1000-3657
- isbnNo：CN11-1167/P
摘要
Beishan area is an important metallogenic belt, and the Baishantang Cu polymetallic deposit is one of the representative porphyry copper deposits. Two kinds of magmatic rocks along ore belt I in the Baishantang ore district were dated by the zircon LA-ICP-MS U-Pb method, which yielded a porphyry granite diagenetic age of(275.0±3.0)Ma(MSWD =1.17), indicating early Permian. Two groups of ages were obtained for rhyolite porphyry: a magma zircon group of the rhyolite porphyry has an age of(371.1 ±2.8)Ma(MSWD =1.7), suggesting late Devonian. The other inheritance zircon group of inheritance zircon with remarkable rounded shape or enveloped in the former group has ages of(2627±35)Ma,(2598±35)Ma,(705±44)Ma,(1722±48) Ma,(1642±51)Ma,(1213±54)Ma, which can be assigned roughly to 2.6 billion years, 1.7 billion years and 1.2 billion years, indicating that the rhyolite porphyry was related to the remelting of the upper-middle crust in late Devonian, as also shown by the geochemical characteristics.
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