Earth Science Frontiers ›› 2020, Vol. 27 ›› Issue (4): 272-281.DOI: 10.13745/j.esf.sf.2019.8.24

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Paleoceanographic environment in Gyangzê, South Tibet during the Jurassic-Cretaceous boundary interval

GAO Lianfeng1,2(), LI Puzhuang1, ZHANG Zhenguo1,2,*(), WAN Xiaoqiao3, XIA Shiqiang1, DONG Guiyu1, WANG Zhaosheng1, LENG Chunpeng1, ZHANG Ying1, YAO Jiming1, ZHANG Linting1, YU Jiangtao1, YIN Shiyan1   

  1. 1. College of Mining Engineering, North China University of Science and Technology, Tangshan 063210, China
    2. College of Mining Engineering, Liaoning Technical University, Fuxin 123000, China
    3. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences(Beijing), Beijing 100083, China
  • Received:2018-11-21 Revised:2019-06-05 Online:2020-07-25 Published:2020-07-25
  • Contact: ZHANG Zhenguo

Abstract:

In order to investigate the evolution of marine sedimentary environments during the Jurassic-Cretaceous transition in the Gyangzê area, South Tibet, we collected samples from the Jiabulagou section, and performed major, trace and rare earth element analysis. The discrimination diagrams (Fe2O3+MgO vs. TiO2 or Al2O3/SiO2) showed that, from the Late Jurassic Weimei Formation to the Early Cretaceous Jiabula Formation, the tectonic setting in the study area is mainly oceanic island arc. The index elements of Mn, Fe, V, Co, Ni and REE, and U/Th, V/Cr, Sr/Ba, Lan/Ybn and V/(V+Ni) ratios showed that the deposition conditions evolved from the Weimei Formation environment, characterized by shallow sea, oxygen-enriched, high-salt and high deposition rate, to the Early Cretaceous Jiabula Formation environment, featuring deep sea, water stratification and decreasing sedimentation rate, with obvious characteristics of deep sea sedimentary environment. The geochemical data were consistent with tectonic discrimination diagram, i.e., shallow sea facies sediment, indicated by sandstone in the Weimei Formation, and siltstone in the lower and calcareous mudstone in the upper Jiabula Formation, experienced water changes from shallow to deep.

Key words: Jurassic-Cretaceous boundary, geochemical characteristics, paleoceanographic environment, Gyangzê aera, South Tibet

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