鄂尔多斯盆地奥陶系马家沟组马五<sub>5</sub>亚段微生物岩盆地尺度分布特征及主控因素

doi:10.7605/gdlxb.2021.06.072

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Abstract

Based on the analysis of core,thin section and logging data,basin-scale microbial carbonate with stable distribution developed in the lower part of the Ma⁵₅ sub-member of the Ordovician Majiagou Formation in Ordos Basin. The rock types include argillaceous limestone,limestone,stromatolite,thrombolite,bound sand-clastic limestone,karst breccias. It contains various shaped stromatolite and thrombolite,such as laminar,wavy and columnar stromatolite,laminar,nodular and arborescent thrombolite. Vertically,four typical sedimentary sequences closely related to microbialites are identified,indicating relative sea-level fluctuations. The division and comparative analysis of the small layers with high-frequency cycles suggest that the microbialites are stably distributed laterally,and have basin-scale distribution. Based on the logging template established by core-log calibration,the lithology of 404 wells in the whole basin were interpreted.The result shows that cumulative thickness of microbialites range from 3 to 7m,and the thickness shows a decreasing trend from west to east.Furthermore,the continuous distribution area of microbialites can exceed 2.5×10⁵km²in area,demonstrating that the basin-scale microbialites developed in a relatively shorter time.Analysis of sedimentary sequence in the early depositional stage of Ma⁵₅ sub-member indicates that the relative sea level first slowly rises and then falls in a single cycle,while it shows an oscillating and slowly rising trend in a multi-cycle combination.Further research suggests that the relatively stable paleo-tectonic environment coupled with the filling of early evaporite provides relatively flat paleo-geomorphic conditions.Under the background of continuous slow transgression in the depositional stage of Ma⁵₅ sub-member,the bottom shape condition of environmental homogeneity is the fundamental reason for the development of large-scale microbial carbonate in shallow water.This paper reports the development and distribution of basin-scale microbialites in the depositional stage of Ma⁵₅ sub-member,which not only enriches the research of microbialites in the Majiagou Formation,but also helps improve the understanding of development mechanism of large-scale microbialites in carbonate platforms.

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	Articles by authors
	Yang Meng-Ying
	Tan Xiu-Cheng
	Yang Ming-Yi
	Xu Yu-Qing
	Yan Wei
	Su Wen-Jie
	Zhong Shou-Kang
	Xiong Ying
	Guo Mu-Shi

Key words： microbial carbonates basin-scale distribution dominant controlling factor Majiagou Formation Ordovician Ordos Basin

Received: 10 August 2021

ZTFLH:

P618.13

Corresponding Authors: Tan Xiu-Cheng,born in 1970,is a professorat in Southwest Petroleum University. He is engaged in researches of sedimentology and reservoir geology. E-mail: tanxiucheng70@163.com.

About author: Yang Meng-Ying,born in 1997,is an graduate studentat in Southwest Petroleum University. Her studies focus on sedimentology. E-mail: ymying22@163.com.

Cite this article:

Yang Meng-Ying,Tan Xiu-Cheng,Yang Ming-Yi et al. Basin-scale distribution and dominant controlling factors of microbialites of the Ma₅⁵ sub-member of Ordovician Majiagou Formation in Ordos Basin[J]. JOPC, 2021, 23(6): 1125-1139.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2021.06.072 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2021/V23/I6/1125

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