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2021 Vol. 48, No. 6
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ZHOU Dai, HU Jun, YANG Wenqiang, CHEN Qi, WANG Xiangdong, WANG Lei, XU Deming. 2021. Formation age and petrogenesis of the Xinxing pluton in western Guangdong: Constraint on the closure of the East Paleo-Tethys Ocean[J]. Geology in China, 48(6): 1896-1923. doi: 10.12029/gc20210618
Citation: ZHOU Dai, HU Jun, YANG Wenqiang, CHEN Qi, WANG Xiangdong, WANG Lei, XU Deming. 2021. Formation age and petrogenesis of the Xinxing pluton in western Guangdong: Constraint on the closure of the East Paleo-Tethys Ocean[J]. Geology in China, 48(6): 1896-1923. doi: 10.12029/gc20210618
shu

Formation age and petrogenesis of the Xinxing pluton in western Guangdong: Constraint on the closure of the East Paleo-Tethys Ocean

  • 1.

    China Geological Survey, Wuhan Center of Geological Survey, Wuhan 430223, China

  • 2.

    Research Center for Petrogenesis and Mineralization of Granitoid Rocks, Wuhan 430223, China

  • 3.

    School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • Fund Project: Supported by the project of China Geological Survey(No.DD20160035 and DD20190047)
More Information
  • Author Bio: ZHOU Dai, male, born in 1985, senior engineer, engaged in regional geological survey and research in the Yunkai area and Hainan island; E-mail: 281045030@qq.com
Received Date:  12 May 2019
Revised Date:  11 October 2019
Publish Date:  25 December 2021
    Abstract

  • The tectonic framework on the southern margin of South China Block (SCB) between Permian and Triassic Periods has long been a controversial subject. The regional geological survey and research show that the Xinxing pluton in western Guangdong was emplaced in Late Triassic (240-224 Ma) rather than Jurassic, whose main lithology is medium-fine and fine-grained porphyritic monzonitic granite. The Xinxing granite is characterized by high potassium calc-alkaline and peraluminous-strongly peraluminous series, which is enriched in LREE, Rb, U, and depleted in HREE, Nb, Ta, Zr, Hf, Ti. It exhibits relatively low εNd(t) (-11.5- -10.5) and εHf(t) (-2.9- -10.3) values, showing the crustal source affinity. Therefore it is suggested that the start of the Indosinian tectonic-magmatic event in Western Gongdong probably took place in ~250 Ma. These new geochemical and geochronological evidence have furthermore restricted the timing of tectonic activities on the southern margin of SCB between later Permian (Darongshan pluton) and later Triassic (Xinxing pluton). Hence, the closure time of East Paleo-Tethys Ocean would be about 250 Ma, and the continental-continental collision between Indo-China Block and SCB continued till 240-224 Ma.

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