| Was the Panzhihua Large Fe-Ti Oxide Deposit,SW China,Formed by Silicate Immiscibility? |
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| 作者姓名： | DING Xiangli CHEN Xuanhu SHAO Zhaogang |
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| 作者单位： | Chinese Academy of Geological Sciences |
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| 基金项目： | co-supported by the China Geological Survey (Grant Nos. DD20230229, DD20190011, DD20221643)；;the National Key Research and Development Project of China (Grant No. 2018YFC0603701)； |
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| 摘 要： | The Panzhihua mafic intrusion, which hosts a world-class Fe-Ti-V ore deposit, is in the western Emeishan region, SW China. The formation age(～260 Ma), and Sr and Nd isotopes indicate that the Panzhihua intrusion is part of the Emeishan large igneous province and has little crustal contamination. To assess ore genesis of the Panzhihua Fe-Ti-V ore deposit, two different models have been provided to explain the formation, namely silicate immiscibility and normal fractional crystallization. Silicate...
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| 收稿时间： | 2022/8/15 0:00:00 |
| 修稿时间： | 2022/9/18 0:00:00 |
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