Zircon and apatite fission track analyses on mineralization ages and tectonic activities of Tuwu-Yandong porphyry copper deposit in northern Xinjiang, China
文献类型：期刊论文
| 作者 | Yuan, WM ; Bao ZK(保增宽); Dong JQ(董金泉); Bao, ZK; Dong, JQ; Guo, ZJ; Deng, J
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| 刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
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| 出版日期 | 2007 |
| 卷号 | 50期号:12页码:1787-1795 |
| 关键词 | mineralization age tectonic epoch fission track zircon apatite Tuwu-Yandong Xinjiang |
| 通讯作者 | China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China ; Chinese Acad Sci, Inst High Energy Phys, Lab Nucl Anal Techn, Beijing 100039, Peoples R China ; Peking Univ, Dept Geol, Beijing 100871, Peoples R China |
| 英文摘要 | The mineralization ages reported in the past in the Tuwu-Yandong copper district not only are different, but also fall into the Hercynian epoch. This study has achieved 9 zircon and 7 apatite fission track analysis results. The zircon fission track ages range from 158 Ma to 289 Ma and the apatite ages are between 64 Ma and 140 Ma. The mineralization accords with the regional tectonics in the copper district. We consider that the zircon fission track age could reveal the mineralization age based on annealing zone temperature of 140-300 degrees C and retention temperature of similar to 250 degrees C for zircon fission track, and metallogenetic temperature of 120-350 degrees C in this ore district. Total three mineralization epochs have been identified, i.e., 289-276 Ma, 232-200 Ma and 165-158 Ma, and indicate occurrence of the mineralization in the Indosinian and Yanshan epochs. Corresponding to apatite fission track ages, the three tectonic-mineralizing epochs are 140-132 Ma, 109-97 Ma and 64 Ma, which means age at about similar to 100 degrees C after the mineralization. The three epochs lasted 146 Ma, 108 Ma and about 100 Ma from similar to 250 degrees C to similar to 100 degrees C and trend decrease from early to late. It is shown by the fission track modeling that this district underwent three stages of geological thermal histories, stable in Cretaceous and cooling both before Cretaceous and after 20 Ma. |
| 学科主题 | Geology |
| 类目[WOS] | Geosciences, Multidisciplinary |
| 研究领域[WOS] | Geology |
| 原文出处 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000251020300004 |
| 源URL | [http://ir.ihep.ac.cn/handle/311005/239525]  |
| 专题 | 中国科学院高能物理研究所_人力资源处 高能物理研究所_多学科研究中心 |
| 作者单位 | 中国科学院高能物理研究所 |
| 推荐引用方式 GB/T 7714 | Yuan, WM,Bao ZK,Dong JQ,et al. Zircon and apatite fission track analyses on mineralization ages and tectonic activities of Tuwu-Yandong porphyry copper deposit in northern Xinjiang, China[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2007,50(12):1787-1795. |
| APA | Yuan, WM.,保增宽.,董金泉.,Bao, ZK.,Dong, JQ.,...&Deng, J.(2007).Zircon and apatite fission track analyses on mineralization ages and tectonic activities of Tuwu-Yandong porphyry copper deposit in northern Xinjiang, China.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,50(12),1787-1795. |
| MLA | Yuan, WM,et al."Zircon and apatite fission track analyses on mineralization ages and tectonic activities of Tuwu-Yandong porphyry copper deposit in northern Xinjiang, China".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 50.12(2007):1787-1795. |
入库方式： OAI收割
来源：高能物理研究所
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