| 西藏波龙斑岩铜金矿床钾长石和绢云母40Ar/39Ar年龄及其地质意义 |
| Received:September 03, 2012 Revised:June 05, 2013 点此下载全文 |
| 引用本文：ZHU XiangPing,CHEN HuaAn,MA DongFang,HUANG HanXiao,LI GuangMing,LI YuBin,LI YuChang,WEI LuJie,LIU ChaoQiang.2013.40Ar/39Ar dating of hydrothermal K-feldspar and hydrothermal sericite from Bolong porphyry Cu-Au deposit in Tibet[J].Mineral Deposits,32(5):954~962 |
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| Author Name | Affiliation | | ZHU XiangPing | Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China | | CHEN HuaAn | Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China | | MA DongFang | Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China | | HUANG HanXiao | Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China | | LI GuangMing | Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China | | LI YuBin | No. 5 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Golmud 816000, Qinghai, China | | LI YuChang | No. 5 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Golmud 816000, Qinghai, China | | WEI LuJie | No. 5 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Golmud 816000, Qinghai, China | | LIU ChaoQiang | No. 5 Geological Party, Tibet Bureau of Geology and Mineral Exploration and Development, Golmud 816000, Qinghai, China |
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| 基金项目:本文为国家973项目"青藏高原南部大陆聚合与成矿作用"(编号:2011CB403105);国家自然科学基金项目(编号: 41202049,41272091);中国地质调查局地质矿产调查评价专项(编号: 1212011086074,12120113037000)联合资助成果 |
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| 中文摘要:西藏波龙斑岩铜金矿床是新近在青藏高原中部发现的规模最大的斑岩型矿床。文章对该矿床内的蚀变钾长石和蚀变绢云母进行了40Ar/39Ar年代学测试,获得蚀变钾长石的40Ar/39Ar坪年龄为(118.33±0.60) Ma,反等时线年龄为(118.49±0.74) Ma (初始40Ar/36Ar=286.1±8.4),表明波龙斑岩铜金矿床的钾化蚀变年龄为118~119 Ma;蚀变绢云母的40Ar/39Ar坪年龄为(121.61±0.67) Ma,反等时线年龄为(121.1±2.0) Ma (初始40Ar/36Ar=279±19)。由于蚀变绢云母测试样品内可能混入了斜长石,受其影响,蚀变绢云母测年结果的下限可能代表了该矿床绢英岩化蚀变年龄。这些蚀变钾长石和蚀变绢云母40Ar/39Ar测年结果与波龙矿床的成岩年龄值和成矿年龄值在误差范围内基本一致,表明该矿床的钾化和绢英岩化与成岩、成矿同期,该矿床的岩浆-热液活动过程的时限为121~118 Ma。 |
| 中文关键词:地球化学 40Ar/39Ar年龄 钾长石化 绢英岩化 波龙斑岩铜金矿床 班公湖-怒江成矿带 西藏 |
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| 40Ar/39Ar dating of hydrothermal K-feldspar and hydrothermal sericite from Bolong porphyry Cu-Au deposit in Tibet |
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| Abstract:The Bolong porphyry copper-gold deposit is the largest porphyry copper deposit discovered recently in the middle of the Tibetan plateau. Hydrothermal K-feldspar from the potassic alteration zone and hydrothermal sericite from the phyllic alteration zone were analyzed by 40Ar/39Ar dating technique. The plateau age of secondary K-feldspar is (118.33±0.60) Ma, which, together with its reverse isochron age of (118.49±0.74) Ma (initial 40Ar/36Ar = 286.1±8.4), represents the potassic alteration age of the Bolong deposit. The plateau age of secondary sericite is (121.61±0.67) Ma, and its reverse isochron age is (121.1±2.0) Ma (initial 40Ar/36Ar=279±19). The high 37Ar/39Ar ratio of the secondary sericite sample indicates that some magmatic plagioclase was mixed in the sample, which increased the dating value. Thus, the phyllic alteration might have occurred around 119 Ma. Taking the deviation and uncertainties of geochronologic methods into account, the authors have found that the 40Ar/39Ar ages of hydrothermal K-feldspar and hydrothermal sericite are similar to the ore-forming and rock-forming ages of the Bolong deposit, suggesting that the potassic alteration and mineralization in the Bolong porphyry deposit were coeval with the intrusion of porphyries and phyllic alteration, and the magmatic-hydrothermal duration was within 121~118 Ma. |
| keywords:geochemistry 40Ar/39Ar age K-feldspathic alteration phyllic alteration Bolong porphyry Cu-Au deposit Bangong Lake-Nujiang River metallogenic belt Tibet |
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