New understanding on the genetic mechanism of microsparite(molar-tooth)carbonates in the Neoproterozoic Hejiazhai Formation in Songshan area,Henan Province
Wang Zhen-Tao1, Li Xian-Gen2
1 MNR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,CAGS,Beijing 100037,China; 2 Offshore Oil Production Plant of Sinopec Shengli Oilfield Company,Shandong Dongying 257237,China
Abstract：As an international research focus on the Precambrian carbonate rocks,the microsparite(molar-tooth)carbonate (MT for short)is of great significance in the reconstruction of palaeogeography,stratigraphic correlation and palaeoclimate,but its formation mechanism has been debated for a long time. The Neoproterozoic Hejiazhai Formation in Songshan area,which is located at the southern margin of North China Craton,is characterized as a large number of MT deposits that were interpreted as the product of seismic liquefaction. In this paper,based on the MT-containing strata of the Hejiazhai Formation,detailed studies include the morphology of MT,microfacies and sedimentary environment were carried out. Results show that the Hejiazhai Formation MT formed in the carbonate ramp environment and it owes early diagenetic features. The morphology of MT has a strong relationship with the lithology of the host rocks and the sedimentary environments. Besides,the differences between the MT and “liquefied vein”triggered by earthquake were compared from several aspects. Through the above work,we clearly pointed out that the Hejiazhai Formation MT is mainly constrained by the palaeomarine conditions and sedimentary microfacies,and it is a good indicator of the ancient environment,but has no relationship with the earthquakes.
Wang Zhen-Tao,Li Xian-Gen. New understanding on the genetic mechanism of microsparite(molar-tooth)carbonates in the Neoproterozoic Hejiazhai Formation in Songshan area,Henan Province[J]. JOPC, 2020, 22(1): 56-74.
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