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XU Xudong, LI Fengjie, YAN Dawei, LI Chunsen. Genesis and paleoenvironment of the iron ooids from the Ganxi prolife of the Devonian Yangmaba Formation in Beichuan County, Longmenshan Area[J]. GEOLOGY IN CHINA, 2021, 48(1): 322-331. DOI: 10.12029/gc20210122
Citation: XU Xudong, LI Fengjie, YAN Dawei, LI Chunsen. Genesis and paleoenvironment of the iron ooids from the Ganxi prolife of the Devonian Yangmaba Formation in Beichuan County, Longmenshan Area[J]. GEOLOGY IN CHINA, 2021, 48(1): 322-331. DOI: 10.12029/gc20210122

Genesis and paleoenvironment of the iron ooids from the Ganxi prolife of the Devonian Yangmaba Formation in Beichuan County, Longmenshan Area

Funds: 

National natural science foundation of China 41172100

National undergraduate innovation and entrepreneurship training program 201710616141

Sedimentary geology innovation team fund of Chengdu University of Technology KYTD201703

More Information
  • Author Bio:

    XU Xudong, male, born in 1997, bachelor's degree, engages in the study and research of sedimentology; E-mail:xuxudong949981291@163.com

  • Corresponding author:

    LI Fengjie, male, born in 1972, professor, engages in the teaching and research of sedimentology, E-mail:lifengjie72@163.com

  • Received Date: October 31, 2018
  • Revised Date: March 04, 2019
  • Available Online: September 25, 2023
  • There exist abundant iron ooids at the bottom of the Middle Devonian Yangmaba Formation in the Longmenshan area. In order to analyze the genesis of the iron ooids, their characteristics were studied by means of thin section and scanning electron microscope based on the detailed measurement of the Shiligou Profile in Ganxi village. The analysis results show that there are various types of ooids in Middle Devonian Yangmaba Formation of Longmenshan area. The ooidal cores include four types:quartz clastic particles, crinoid fragments, black hematite and calcite. The outer laminas of ooids can be divided into three types:alternate dark and bright one, uniform-colored one and chlorite-fragmented one. The iron ooids of Middle Devonian Yangmaba Formation in the Longmenshan area have an important significance to the ancient environment. The silty ooids were formed in the open environment nearshore shallow water under oxidation condition, and iron ones and chlorite ones with thin layers were deposited in the relatively closed lagoon and residual ooids beach of shallow seashore.

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