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2023 Vol. 56, No. 2
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WU Shukuan, CHEN Guochao, LI Jiqing, CHEN Xiaozhen, LI Ruibao, WEI Junqi. 2023. Geochronology, Petrogenesis and Tectonic Significance of Zhanhongshan Peraluminous Rhyolite Porphyry in Gouli Area, Eastern Section of East Kunlun. Northwestern Geology, 56(2): 92-108. doi: 10.12401/j.nwg.2022043
Citation: WU Shukuan, CHEN Guochao, LI Jiqing, CHEN Xiaozhen, LI Ruibao, WEI Junqi. 2023. Geochronology, Petrogenesis and Tectonic Significance of Zhanhongshan Peraluminous Rhyolite Porphyry in Gouli Area, Eastern Section of East Kunlun. Northwestern Geology, 56(2): 92-108. doi: 10.12401/j.nwg.2022043
shu

Geochronology, Petrogenesis and Tectonic Significance of Zhanhongshan Peraluminous Rhyolite Porphyry in Gouli Area, Eastern Section of East Kunlun

  • 1.

    No. 5 Geology Exploration of Qinghai Province, Xining 810003, Qinghai, China

  • 2.

    Key Laboratory of Western China’s Mineral Resources and Geological Engineering of Ministry of Education, Chang’an University, Xi’an 710054, Shaanxi, China

  • 3.

    Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources, Beijing 100037, China

  • 4.

    School of Civil Engineeringy, Nanyang Institutte of Technolog, Nanyang 473000, Henan, China

  • 5.

    Geology Survey Institute of Qinghai Province, Xining 810001, Qinghai, China

  • 6.

    Hubei Key Laboratory of Resources and Eco-Environment Geology, Hubei Geological Bureau, Wuhan 430034, Hubei, China

More Information
Received Date:  15 October 2021
Revised Date:  07 June 2022
Publish Date:  20 April 2023
    Abstract

  • The study of Triassic granitic rocks in East Kunlun mainly focuses on the large granite batholith with the characteristics of I−type granite, while the study of a small amount of peraluminous granite is less. The LA−ICP−MS zircon U−Pb dating of The Zhanhongshan rhyolite porphyry shows that the crystallization age of the Zhanhongshan rhyolite porphyry is 245±1 Ma. The Zhanhongshan rhyolite porphyry is characterized by high silica (SiO2=74.50%～75.59%), rich Na (Na2O=4.04%～4.06%), high Na2O/K2O ratio (1.26～1.76), and aluminum saturation index (A/CNK=1.07～1.14), which indicate weak peraluminous medium potassium and high potassium calc−alkaline series. The rocks is characterized by low REE content with obvious fractionation of LREE and HREE, slight negative and positive Eu anomalies (δEu=0.80～1.06), also enrichment of LILE and depletion of HFSE. They have enriched Hf isotopic compositions with εHf (t) isotope values of −4.7～+0.9. It is concluded that the peraluminous Zhanhongshan rhyolite porphyry has the characteristics of I−type granite, which is the result of the underplating of the subducted oceanic crust through mantle−derived magma and partial melting with the addition of foreign fluid, and has arc magmatic geochemical characteristics. Combined with the previous data, the study shows that the East Kunlun area was in the subduction stage of the Paleo−Tethys ocean in the Early Triassic.

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