Sm-Nd dating of scheelite in Luojiachong W-Sn deposit, Miaoershan area, southwestern Hunan Province: Implications for polycyclic tectonic-magmatic activities and metallogenesis in South China

DU Yun; TIAN Lei; ZHENG Zhengfu; CHEN Jianfeng; ZHANG Xiaoqiang; WANG Jingyuan; ZHOU Litong; FAN Hui; LI Chao

doi:10.12097/j.issn.1671-2552.2022.05.013

2022 Vol. 41, No. 5

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DU Yun, TIAN Lei, ZHENG Zhengfu, CHEN Jianfeng, ZHANG Xiaoqiang, WANG Jingyuan, ZHOU Litong, FAN Hui, LI Chao. Sm-Nd dating of scheelite in Luojiachong W-Sn deposit, Miaoershan area, southwestern Hunan Province: Implications for polycyclic tectonic-magmatic activities and metallogenesis in South China[J]. Geological Bulletin of China, 2022, 41(5): 886-902. doi: 10.12097/j.issn.1671-2552.2022.05.013

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DU Yun, TIAN Lei, ZHENG Zhengfu, CHEN Jianfeng, ZHANG Xiaoqiang, WANG Jingyuan, ZHOU Litong, FAN Hui, LI Chao. Sm-Nd dating of scheelite in Luojiachong W-Sn deposit, Miaoershan area, southwestern Hunan Province: Implications for polycyclic tectonic-magmatic activities and metallogenesis in South China[J]. Geological Bulletin of China, 2022, 41(5): 886-902. doi: 10.12097/j.issn.1671-2552.2022.05.013

Sm-Nd dating of scheelite in Luojiachong W-Sn deposit, Miaoershan area, southwestern Hunan Province: Implications for polycyclic tectonic-magmatic activities and metallogenesis in South China

1.
Hunan Institute of Geological Survey, Changsha 410116, Hunan, China
2.
Research Center for Petrogenesis and Mineralization of Granitoid Rocks, China Geological Survey, Wuhan 430205, Hubei, China

Received Date: 13 January 2020

Revised Date: 10 October 2020

Publish Date: 15 May 2022

Abstract

Abstract

The scheelite in the mining area has high Sm and Nd contents, low Sm/Nd ratio.Its Sm-Nd isochron age is 401.5±9.4 Ma (2σ, MSWD=0.90), and the initial ratio of ¹⁴³Nd/¹⁴⁴Nd is 0.5120214±0.0000098, indicating that the deposit was formed in the Late Caledonian period.Scheelite ε_Nd (t)value is -1.91~1.99, suggesting that the ore-forming material of the deposit mainly comes from the crust.Zircon LA-ICP-MS dating of the main ore-hosting granite in the mining area shows that its petrogenetic age is 423.7±2.7 Ma (2σ, MSWD=0.61), belonging to the first intrusive episode of Late Caledonian granites.Its major element contents and characteristic parameters vary widely.Its source rocks are mainly sand clastic rocks and mudstones from the Paleo-Mesoproterozoic basement crust, and it may have assimilated and mixed some Jinningian Ca and Mg-rich magmatic rocks.Based on the results of this study and previous data, it is considered that the tectonic-magmatic activities and metallogenesis in Miaoershan area and South China are multicyclic.The dominant petrogenetic and metallogenic time of the northern and southern sections of the Miaoershan pluton are Caledonian and Indosinian respectively, showing an overall "Caledonian for north and Indosinian for south" pattern.This study aims to provide a basis for guiding the prospecting work in the area and improving the petrogenetic and metallogenic theory in South China.
- Sm-Nd dating /
- scheelite /
- Caledonian period /
- metallogenesis /
- Luojiachong W-Sn deposit /
- Miaoershan pluton /
- Hunan Province /
- geological survey engineering

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References

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