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.
Fund:; Co-funded by the subproject of National Key R & D Program of China(No.2017YFC0602704)and the National Natural Science Foundation of China(No.40572073)
About author: Wang Zhen-Tao,male,born in 1986,is an associate professor of the Institute of Mineral Resources,Chinese Academy of Geological Sciences,with a Ph.D. degree obtained from the China University of Geosciences(Beijing). He is currently engaged in Paleozoic-Mesozoic tectonics and sedimentary evolution of the western North China Craton and Yangtze Craton. E-mail: wangz@cags.ac.cn.
Cite this article:
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.
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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