| 西藏邦铺钼(铜)矿床辉绿玢岩脉体LA-ICP-MS锆石U-Pb定年及其地质意义 |
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| 引用本文： | 冷秋锋,王立强,应立娟,郑文宝,罗茂澄,陈伟,林彬,王艺云.西藏邦铺钼(铜)矿床辉绿玢岩脉体LA-ICP-MS锆石U-Pb定年及其地质意义[J].地球学报,2012,33(4):559-568. |
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| 作者姓名： | 冷秋锋 王立强 应立娟 郑文宝 罗茂澄 陈伟 林彬 王艺云 |
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| 作者单位： | 成都理工大学地球科学学院;中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室;中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室;成都理工大学地球科学学院;中国地质大学(北京)地球科学与资源学院;成都理工大学地球科学学院;成都理工大学地球科学学院;成都理工大学地球科学学院 |
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| 基金项目： | 国家973项目(编号: 2011CB403103);青藏专项(编号: 1212011085529) |
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| 摘 要： | 西藏邦铺斑岩型钼(铜)矿床位于冈底斯成矿带东段,地理位置上与甲玛铜多金属矿床、驱龙斑岩铜矿床毗邻.矿区岩浆活动频繁,发育不同类型、不同期次的侵入岩体,辉绿玢岩出露于矿区北部,地质研究程度相对较低.为了精确限制其成岩时代,文章通过对辉绿玢岩脉体LA-ICP-MS锆石U-Pb年龄精确测试,获得了19颗锆石206Pb/238...
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| 关 键 词： | LA-ICP-MS 锆石U-Pb定年 辉绿玢岩 邦铺 冈底斯 西藏 |
LA-ICP-MS Zircon U-Pb Dating of Allgovite in the Bangpu Molybdenum (Copper) Deposit in Tibet and Its Geological Significance |
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| LENG Qiu-feng,WANG Li-qiang,YING Li-juan,ZHENG Wen-bao,LUO Mao-cheng,CHEN Wei,LIN Bin and WANG Yi-yun.LA-ICP-MS Zircon U-Pb Dating of Allgovite in the Bangpu Molybdenum (Copper) Deposit in Tibet and Its Geological Significance[J].Acta Geoscientia Sinica,2012,33(4):559-568. |
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| Authors: | LENG Qiu-feng WANG Li-qiang YING Li-juan ZHENG Wen-bao LUO Mao-cheng CHEN Wei LIN Bin and WANG Yi-yun |
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| Institution: | College of Earth Sciences, Chengdu University of Technology;MLR Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;MLR Key Laboratory of Metallogeny and Mineral Resource Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;College of Earth Sciences, Chengdu University of Technology;School of Earth Sciences and Resources, China University of Geosciences;College of Earth Sciences, Chengdu University of Technology;College of Earth Sciences, Chengdu University of Technology;College of Earth Sciences, Chengdu University of Technology |
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| Abstract: | The Bangpu porphyry Mo (Cu) deposit is located in the eastern part of the Gangdise metallogenic belt in Tibet, near the Jiama copper polymetallic deposit and the Qulong porphyry Cu deposit. The magma invasion is of high frequency in this area, and varied kinds of intrusions were developed in different periods. Researches on the allgovite in the northern part of the Bangpu ore district are very insufficient. The age of allgovite was obtained in this deposit. According to LA-ICP-MS analysis of the zircon U-Pb age precision of the allgovite, 19 zircons from allgovite yielded the weighted average 206Pb/238U age of 15.21±0.29 Ma (MSWD=9.6, N=19), suggesting Miocene magma emplacement in Gangdise belt, and the age is consistent with that of allgovite in the Jiama porphyry deposit. Regional ore-forming regularity study shows that the Bangpu porphyry Mo (Cu) polymetallic deposit is in accord with the regional porphyry deposits such as Jiama and Qulong in the ore-forming and rock-forming age, suggesting that this deposit has the same geochemical dynamic background deep process as Jiama, Qulong and some other ore deposits. |
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| Keywords: | LA-ICP-MS zircon U-Pb dating allgovite Bangpu Gangdise Tibet |
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