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Geoscience ›› 2019, Vol. 33 ›› Issue (03): 574-586.DOI: 10.19657/j.geoscience.1000-8527.2019.03.10

• Structural Geology and Stratigraphy • Previous Articles     Next Articles

Study of the Radiolarian Fauna from Kaduo in Zedang of Southern Tibet and the Geological Significance

MA Xuesong(), LI Guobiao()   

  1. 1. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China
    2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
  • Received:2018-12-01 Revised:2019-04-20 Online:2019-06-23 Published:2019-06-24
  • Contact: LI Guobiao

Abstract:

The Yarlung-Zangbo Ophiolite Zone has long been considered as the lithospheric residual of Neo-Tethys, jointly with the marine stratum within the Yarlung-Zangbo Suture Zone, recorded the evolution of the Neo-Tethys and the collision between India Plate and Eurasian Plate. Moderate preserved Mesozoic radiolarian fossils have been found from the Kaduo Chert, near the southwest of the Zedang of southern Tibet. And 39 radiolarian species belonging to 31 genera have been identified preliminary. Four radiolarian assemblages have been recognized as follows in ascending: Alievium longispineum-Transhsuum maxwelli assemblages (Late Bathonian-Early Callovian), Hsuum maxwelli-Triactoma mexicana assemblages (Late Callovian-Oxfordian), Holocryptocapsa hindei-Hiscocapsa grutterinki assemblages (Late Barremian-Early Aptian) and Hemicryptocapsa polyhedra-Obeliscoites giganteus assemblages (Late Albian-Cenomanian). The radiolarian assemblages in the Kaduo chert can provide an important micropaleontological evidence for the formation time constrain on the Zedang ophiolite and the evolution of the Neo-Tethys Ocean.

Key words: Yarlung-Zangbo suture, ophiolite, chert, radiolarian, Mesozoic

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