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WANG Jinfang, LI Yingjie, LI Hongyang, DONG Peipei. 2021. Discovery of the Late Carboniferous adakite in the Erenhot-Hegenshan suture zone and intra-oceanic subduction of the Paleo-Asian Ocean[J]. Geology in China, 48(2): 520-535. doi: 10.12029/gc20210212
Citation: WANG Jinfang, LI Yingjie, LI Hongyang, DONG Peipei. 2021. Discovery of the Late Carboniferous adakite in the Erenhot-Hegenshan suture zone and intra-oceanic subduction of the Paleo-Asian Ocean[J]. Geology in China, 48(2): 520-535. doi: 10.12029/gc20210212
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Discovery of the Late Carboniferous adakite in the Erenhot-Hegenshan suture zone and intra-oceanic subduction of the Paleo-Asian Ocean

  • College of Earth Sciences, Hebei GeoUniversity, Shijiazhuang, 050031, Hebei, China

    • Fund Project: Funded by National Natural Science Foundation of China (No.41972061) and the projects of China Geological Survey(No.1212011120711, No.1212011120701)
More Information
  • Author Bio: WANG Jinfang, female, born in 1983, associate professor, engaged in the study of petrology and geochemistry
Received Date:  08 May 2018
Revised Date:  02 July 2020
Publish Date:  25 April 2021
    Abstract

  • The Ehenaobaotu tonalite is outcropped in the northern part of the Meilaotewula SSZ-type ophiolite of the Erenhot-Hegenshan suture zone in Xi Ujimqin Banner of Inner Mongolia. Based on the study of petrology, geochemistry and zircon LA-ICP-MS U-Pb geochronology, the genetic type and tectonic setting of the tonalite were determined, and the final closure time and subduction process of the Erenhot-Hegenshan ocean basin of the Paleo-Asian Ocean were discussed. The tonalite is characterized by high SiO2, Al2O3, Na2O, Sr and low K2O, Y contents, enrichment of Rb, Ba, Sr large ion lithophile elements and LREE, and depletion of Nb, Ta, Ti, P high field strength elements and HREE. There is no pronounced Eu anomaly. The lithological and geochemical characteristics show that the Ehenaobaotu pluton is a high Si adakite (HSA) formed in island arc, and was derived from patial melting of the intra-oceanic subductingd oceanic crust and sediment and subsequently reaction with overlying mantle wedge peridotite. Its U-Pb LA-ICP-MS dating yields (305.6±1.5) Ma and suggests that the Ehenaobaotu pluton was formed during Late Carboniferous. Combined with the study of spatio-temporal evloution of the Carboniferous ophiolites and Carboniferous-Permian island arc magmatic rocks in the Erenhot-Hegenshan suture, it is assumed that the Erenhot-Hegenshan oceanic basin of the Paleo-Asian Ocean was in the process of oceanic subduction characterized by intra-oceanic subduction during the Carboniferous-Early Permian.

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