| 巴基斯坦西俾路支省Chagai地区Saindak斑岩铜金矿床高锶低钇中酸性岩地球化学 |
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| 引用本文： | Abdul Shakoor MASTOI,DENG Jianghong,YANG Xiaoyong. 巴基斯坦西俾路支省Chagai地区Saindak斑岩铜金矿床高锶低钇中酸性岩地球化学[J]. 地质论评, 2016, 62(S1): 157-158 |
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| 作者姓名： | Abdul Shakoor MASTOI DENG Jianghong YANG Xiaoyong |
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| 作者单位： | 中国科学技术大学 中国科学院壳幔物质与环境重点实验室,Centre for Pure and Applied Geology, University of Sindh,中国科学技术大学 中国科学院壳幔物质与环境重点实验室,中国科学技术大学 中国科学院壳幔物质与环境重点实验室 |
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| 摘 要： | The Chagai arc is located in southwest of Pakistan and extends into Iran and Afghanistan (Fig.1A). The border between eastern Iran and western Pakistan roughly coincides with the transition from the collisional Zagros orogenic belt in the west to the Makran accretionary complex and Chagai magmatic arc in the east Siddiqui (2004). The Baluchistan (or Makran) magmatic arc, is an east-west trending, ~500 km long and up to 140 km wide belt of calc-alkaline plutonic, volcanic, and sedimentary rocks, which is part of the continental-scale Tethyan belt that spans eastern Europe and Asia. Activity along the arc began in the Late Cretaceous and continued through into the Quaternary.
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| 关 键 词： | 巴基斯坦 西俾路支省 斑岩铜矿 斑岩金矿；高锶低钇中酸性岩（埃达克岩） |
| 收稿时间： | 2016-07-10 |
| 修稿时间： | 2016-09-20 |
Geochemistry of Adakites from the Saindak Porphyry Cu-Au Deposits, Chagai, West Baluchistan, Pakistan |
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| Abdul Shakoor MASTOI,DENG Jianghong and YANG Xiaoyong. Geochemistry of Adakites from the Saindak Porphyry Cu-Au Deposits, Chagai, West Baluchistan, Pakistan[J]. Geological Review, 2016, 62(S1): 157-158 |
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| Authors: | Abdul Shakoor MASTOI DENG Jianghong YANG Xiaoyong |
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