Volume 46 Issue 8
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Cao Shengnan, Wang Bo, 2021. Age, Origin and Geological Implications of Early Paleozoic Marine Bentonites, Northern Yili Block of Central Asian Orogenic Belt. Earth Science, 46(8): 2804-2818. doi: 10.3799/dqkx.2020.279
Citation: Cao Shengnan, Wang Bo, 2021. Age, Origin and Geological Implications of Early Paleozoic Marine Bentonites, Northern Yili Block of Central Asian Orogenic Belt. Earth Science, 46(8): 2804-2818. doi: 10.3799/dqkx.2020.279
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Age, Origin and Geological Implications of Early Paleozoic Marine Bentonites, Northern Yili Block of Central Asian Orogenic Belt

doi: 10.3799/dqkx.2020.279

  • State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China

  • Received Date: 2020-06-14
    Available Online: 2021-09-14
  • Publish Date: 2021-08-15
    Abstract
  • The Yili Block,a part of the Central Asian Orogenic Belt (CAOB),is located in the northern part of Chinese western Tianshan. It is generally believed that the northern Yili Block was an active continental margin during the Late Paleozoic. However,the study of sedimentary and tectonic evolution (especially the isotopic dating) of the Early Paleozoic in the northern Yili Block is relatively weak. Several bentonite (altered tuff) horizons within the Ordovician black siliceous shale sequences in the Guozigou area were recognized. The Ordovician strata were intensively folded. Two bentonite samples were collected from the core and limb of a syncline for zircon U-Pb dating. Both samples indicate their magmatic origin. They yielded consistent and concordant apparent ages,and weighted average ages of 458±2 Ma and 460±2 Ma,respectively. The previous and newly obtained data implies that the bentonites were deposited at the end of Middle Ordovician (Darriwilian Stage). The timing of the bentonites in this study is in agreement with the age of the continental arc-type magmatism in the Wenquan area,both were likely derived from subduction of the Junggar Ocean beneath the northern Yili Block. The bentonites are also coeval with the worldwide intense volcanism,and are likely one of the main causes of the Late Ordovician global climate change and mass extinction.

     

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