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2021 Vol. 48, No. 5
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ZHANG Zhihui, ZHANG Da, HE Xiaolong, HU Bojie, ZHU Xinyou, DU Zezhong, JIA Wenbin, GONG Xiaodong. 2021. Biotite granodiorite age of Jiuling complex in Jiangxi Province and its limitation on the collision and splicing time of the Yangtze and Cathay plates[J]. Geology in China, 48(5): 1562-1579. doi: 10.12029/gc20210518
Citation: ZHANG Zhihui, ZHANG Da, HE Xiaolong, HU Bojie, ZHU Xinyou, DU Zezhong, JIA Wenbin, GONG Xiaodong. 2021. Biotite granodiorite age of Jiuling complex in Jiangxi Province and its limitation on the collision and splicing time of the Yangtze and Cathay plates[J]. Geology in China, 48(5): 1562-1579. doi: 10.12029/gc20210518
shu

Biotite granodiorite age of Jiuling complex in Jiangxi Province and its limitation on the collision and splicing time of the Yangtze and Cathay plates

  • 1.

    China University of Geosciences, Beijing 100083, China

  • 2.

    Development and Research Center of China Geological Survey, Beijing 100037, China

  • 3.

    Beijing institute of geology and mineral resources, Beijing 100012, China

  • 4.

    Jilin University, Changchun 130012, Jilin, China

  • 5.

    Chengdu Center, China Geological Survey, Chengdu 610081, Sichuan, China

    • Fund Project: Supported by National Natural Science Foundation of China (No.41772069) and the project of China Geological Survey (No.1212011220737, No.121201004000150015, No.DD20190570)
More Information
  • Author Bio: ZHANG Zhihui, born in 1980, male, doctor candidate, engaged in mineral deposits and mineral exploration. E-mail: zzh1102114@126.com
  • Corresponding author: ZHANG Da, male, born in 1967, doctoral supervisor, professor, engaged in regional metallogeny research; E-mail: zhangda@cugb.edu.cn 
Received Date:  11 October 2019
Revised Date:  29 November 2019
Publish Date:  25 October 2021
    Abstract

  • In order to explore the magmatic origin and tectonic setting of the Jiuling pluton in northern Jiangxi, a combined study of geochronology, geochemistry and zircon Lu-Hf isotope was carried out for the Dahutang biotite granodiorite. LA-ICP-MS zircon U-Pb dating of biotite granodiorite suggests it was formed at (835.6±1.5) Ma. Geochemistry analysis shows it belongs to the series of potassium-high potassium calcium alkaline peraluminous granite. It has the typical characteristics of S-type granite and it was derived from the melting of the Neoproterozoic Shuangqiaoshan Group. The positive zircon εHf (t) value (2.8-8.2) suggests that the magma forming the granite was originated from the recycling of Proterozoic crustal material. The Dahutang biotite granodiorite was formed in a tectonic background of transition stage from syn-collision to post-collision. Combining with previous studies, it is inferred that that the upper time limit of collision between the Yangtze and Cathaysia plate should be about 835 Ma.

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