J4 ›› 2009, Vol. 39 ›› Issue (6): 1023-1030.

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Discussion on the Sedimentary Environment and Origin of the Microsparite Carbonates of Mesoproterozoic Gaoyuzhuang Formatioin Jixian Area,Tianjin,China

WANG De-hai1, MENG Xiang-hua2, GUO Feng2, REN Guo-xuan2, GE Ming2   

  1. 1.College of Earth Sciences, Jilin University, Changchun 130061,China;2.Institute of Sedimentary Basins, China University of Geosciences, Beijing 100083,China
  • Received:2008-12-02 Online:2009-11-26 Published:2009-11-26

Abstract:

Abundant microsparite(MT)  carbonates was found in the Mesoproterozoic Gaoyuzhuang Formation in Jixian area, Tianjin City. A new type of MT was also found in turbidites. Meter-scale cycle and sedimentary environment were analyzed by using  technologies of profile detailed measured, fischer plot, scanning electron microscope, electron probe and isotopes of Sr and C. Primary MT structures of Gaoyuzhuang Formation were mainly developed in the subtidal of carbonate mesa, midupper meter-scale cycle of deep-water asymmetric type(micrite and calcareous mudstone ) and core of the turbidites. The MT carbonates were developed during HST stage of meter-scale cycle in paleoocean sedimentary environment with the low 87Sr/86Sr value( <0.709 67) and δ13C value((0±1)‰).

Key words: Gaoyuzhuang Formation, Mesoproterozoic, microsparite(MT) carbonate, Jixian, mineralogy

CLC Number: 

  • P618.13
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