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GE Xiangying, MOU Chuanlong, YU Qian, LIU Wei, MEN Xin, HE Jianglin, LU Junze, LIANG Wei. 2021. Petrology and geochemistry of the K-bentonites at the Ordovician-Silurian transition in XD2 well, Daguan, Yunnan Province[J]. Geology in China, 48(3): 911-924. doi: 10.12029/gc20210318
Citation: GE Xiangying, MOU Chuanlong, YU Qian, LIU Wei, MEN Xin, HE Jianglin, LU Junze, LIANG Wei. 2021. Petrology and geochemistry of the K-bentonites at the Ordovician-Silurian transition in XD2 well, Daguan, Yunnan Province[J]. Geology in China, 48(3): 911-924. doi: 10.12029/gc20210318
shu

Petrology and geochemistry of the K-bentonites at the Ordovician-Silurian transition in XD2 well, Daguan, Yunnan Province

  • 1.

    Chengdu Institute of China Geology and Mineral Resources, Chengdu 610081, Sichuan, China

  • 2.

    China University of Geosciences(Beijing), Beijing 100083, China

  • 3.

    Shandong University of Science and Technology, Qingdao 266590, Shandong, China

    • Fund Project: Funded by China Geological Survey Project(No.DD20160176, No.DD20190122)
More Information
  • Author Bio: GE Xiangying, female, born in 1986, master degree, an engineer, engaged in the study of sedimentology and basin analysis; E-mail: gexiangying-2006@163.com
Received Date:  09 October 2018
Revised Date:  15 April 2019
Publish Date:  25 June 2021
    Abstract

  • Many K-bentonites have been recognized from the Wufeng-Longmaxi Formations (Upper Ordovician-Lower Silurian) in the Yangtze Block,but only a few of them on the western margin of the Yangtze Block are reported. The mineralogical and geochemical studies of K-bentonites in the Wufeng-Longmaxi Formations through Xindi 2 well in Daguan area of Yunnan province were carried out to confirm the original magma type and its tectonic setting. The mineralogical characteristics show that the potassium bentonite is mainly composed of clay minerals and non-clay minerals,in which the clay minerals are composed of illite and illite-montmorillonite mixed beds. The non-clay minerals are mainly quartz,feldspar,calcite,dolomite and pyrite. It is geochemically characterized by high K2O and low TiO2,relative enrichment of Rb,Ba,Th and U and depletion of Ti and P elements. The Ti/Th values indicates acidic volcanic ash character. Compared with the chondrite,the total rare earth elements is (49.86-209.43)×10-6 with slight rich LREE and negative Eu amomaly,without Ce abnormity. In Nb/Y-Zr/TiO2 diagram,the data dots are mainly plotted in the andesite and trachy andesite range,which shows that the volcanic ash is mostly from middle-acid rocks. Various chemical discrimination diagrams and trace elements imply that K-bentonites were possibly derived from an island arc environment,and the volcanic ash was probably related to the subduction and closure of the Qinling Ocean on the northern border of Yangtze Plate in the Early Paleozoic.

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