巴基斯坦吉尼奥德矿区新元古代火山岩年代学及地质意义

徐剑南; 马昌前; 尹烁; 王连训; 顿新海

doi:10.3799/dqkx.2017.143

Volume 42 Issue 12

Dec. 2017

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Article Navigation > Earth Science > 2017 > 42(12): 2282-2298

Xu Jiannan, Ma Changqian, Yin Shuo, Wang Lianxun, Dun Xinhai, 2017. Chronology and Tectonic Implications of Neoproterozoic Volcanics from Chiniot Deposit, Pakistan. Earth Science, 42(12): 2282-2298. doi: 10.3799/dqkx.2017.143

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Xu Jiannan, Ma Changqian, Yin Shuo, Wang Lianxun, Dun Xinhai, 2017. Chronology and Tectonic Implications of Neoproterozoic Volcanics from Chiniot Deposit, Pakistan. Earth Science, 42(12): 2282-2298. doi: 10.3799/dqkx.2017.143

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Chronology and Tectonic Implications of Neoproterozoic Volcanics from Chiniot Deposit, Pakistan

doi: 10.3799/dqkx.2017.143

1.
State Key Laboratory of Geological Processes and Mineral Resources, Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Wuhan Surveying-Geotechnical Research Institute Co. Ltd. Of MCC Wuhan 430080, China

Received Date: 2017-03-24
Publish Date: 2017-12-15

Abstract

Abstract

This is a hotpoint that the study the breakup of Rodinia supercontinent and the formation of Chiniot iron oxide-apatite deposit, we report zircon U-Pb ages, Hf isotopic composition and REE contents of andesite. All the zircons are magmatic origin with the similar REE patterns which are enriched in HREE with a positive Ce anomaly and a negative Eu anomaly. The zircon U-Pb isotopic analyses yields ²⁰⁶Pb/²³⁸U ages of 947.8±4.0 Ma and 883.0±5.1 Ma, which can be interpreted as the crystallization ages of two stages of andesites. Besides, the inherited zircons with U-Pb age of 1 523.0±66 Ma may indicate a Mesoproterozoic basement. The igneous zircons have highly variable ε_Hf(t) values ranging from -4.67 to +13.10, indicating that the andesites were derived from partial melting of a mixed mantle sourse. The geochemical and isotopic variation suggest that mantle-derived basic magmas have went through some degree of crustal commination during migration through Mesoproterozoic granitoids. The formation of the andesites were induced by a series of tectono-thermal events, associated with extensional rift and mantle plume during Rodinia supercontinent. There are many similarities between Chiniotiron deposit and Khetri Copper Belt in geological setting of ore-forming processes, indicating that the metallogenetic potentiality of giant IOCG is very well. The northwest of Indian craton may have connection with North China-Congo-São Francisco craton between 960 Ma and 880 Ma.
- Pakistan,
- andesite,
- mantle-derived,
- extensional rift,
- Rodinia supercontinent,
- geochronology,
- petrology

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