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SU Lin, DONG Guochen, TAN Changhai, PENG Chuan, Yanick Blaise Ketchaya, DONG Pengsheng, CHANG Zeguang. Geochronology, geochemical characteristics of the rhyolites of Tumugou Formation in the central part of Yidun arc, western Sichuan: Implications for their petrogenesis[J]. GEOLOGY IN CHINA, 2022, 49(5): 1673-1686. DOI: 10.12029/gc20220520
Citation: SU Lin, DONG Guochen, TAN Changhai, PENG Chuan, Yanick Blaise Ketchaya, DONG Pengsheng, CHANG Zeguang. Geochronology, geochemical characteristics of the rhyolites of Tumugou Formation in the central part of Yidun arc, western Sichuan: Implications for their petrogenesis[J]. GEOLOGY IN CHINA, 2022, 49(5): 1673-1686. DOI: 10.12029/gc20220520
shu

Geochronology, geochemical characteristics of the rhyolites of Tumugou Formation in the central part of Yidun arc, western Sichuan: Implications for their petrogenesis

  • 1.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing, 100083, China

  • 2.

    Research Center of Applied Geology of China Geological Survey, Chengdu, 610000, China

  • 3.

    Department of Earth Science, Faculty of Sciences, University of Yaounde 1, P. O. Box 812, Yaounde, Cameroon

Funds: 

National Key R & D Projects 2016YFC0600502

the project of China Geological Survey 12120115041701

the project of China Geological Survey DD20190459

More Information
  • Author Bio:

    SU Lin, male, born in 1995, master, engaged in mineralogy, petrology and mineral deposits; E-mail:874099712@qq.com

  • Corresponding author:

    DONG Guochen, male, born in 1962, professor, engaged in the study of petrology and mineral deposits; E-mail: donggc@cugb.edu.cn

  • Received Date: October 14, 2019
  • Revised Date: May 06, 2020
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • This paper is the result of the geological survey engineering

    Objetive 

    The Yidun island arc, as a key part of Sanjiang Tethys orogenic belt, has been hottly debated on granitic intrusions and the related mineralization in recent years. But few studies are concerned with the rhyolites such as the Tumugou Formation.

    Methods 

    Based on detailed field mapping, this paper has conducted research on petrology, geochemistry and chronology of the Tumugou Formation' s rhyolite.

    Results 

    LA-ICP-MS zircon U-Pb dating on one sample yield an age of 216.5 Ma, and proved that the rhyolites were formed in the Late Triassic. The rhyolites have contents of SiO2 from 73.24% to 74.72%, alkali (K2O+Na2O) of 5.26% to 6.27% as calc-alkaline rock series. All the samples are enriched in large ion lithophile elements such as Rb, Th, U, K and light rare earth elements, but depleted in the high strength filed elements such as Nb, Ta, Ti, P and heavy rare earth elements, indicative of the characteristics of island-arc volcanic rocks.

    Conclusions 

    According to the comprehensive study, it is concluded that the rhyolites were formed by partial melting of the lower continental crust during the westward subduction of the Ganzi-Litang oceanic crust in the Indo-Chinese epoch.

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