蒸发背景沉积序列精细刻画及沉积学解译:以鄂尔多斯盆地中部中奥陶统马五<sub>6</sub>亚段为例<sup>*</sup>

doi:10.7605/gdlxb.2021.04.047

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Abstract Assemblages of co-occurred dolomite and gypsum are controlled by chemical sedimentary differentiation,and precise characterization of sedimentary sequences is conducive to revealing sedimentary information in evaporatic environments. Based on drilling and coring data of the Ma5₆ submember of the Ordovician Majiagou Formation in the central Ordos Basin,we studied characterization of typical sedimentary sequences based on macro-and microscopic observation of rocks. The study shows that: (1)paragenetic assemblage of carbonate and evaporite rocks is widely developed in the Ma5₆ submember of the Ordovician Majiagou Formation in the central Ordos Basin,including 10 subtypes of facies;(2)five kinds of sedimentary sequences were summarized,characterized by the lithological assemblage of the lower dolomite and upper gypsum facies and exposed surfaces at the top of each sequence,which shows shallowing and salinizing upward due to gradual replenishment of superposed seawater from evaporative platforms;(3)in the restricted evaporation platform environment,there are mainly four sedimentary subfacies and 11 sedimentary microfacies: lagoon/inter-shoal marine,shoal,lime mud mound and platform flat. Furthermore,the sedimentary sequences in the study area and those in typical evaporative tidal flat are distinguished from each other in terms of lithologic association and sedimentary structures;(4)there were two cycles of sea-level rises and falls recorded in the Ma5₆ submember,and the sedimentary environments could be corresponding to dolomite lagoon,lime mud mound and carbonate shoal,gypsum lagoon,evaporite lagoon,and tidal flat. The above results can provide systematic petrological evidence for the study of sedimentary environments and sea-level change of the Ma5₆ submember in Ordos Basin.

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	Articles by authors
	Huang Dao-Jun
	Zhong Shou-Kang
	Zhang Dao-Feng
	Wang Bao-Bao
	Liao Jian-Chu
	Xie Kang
	Lu Zi-Xing
	Tan Xiu-Cheng

Key words： sedimentary sequence rock types sedimentological origin Majiagou Formation Ordos Basin

Received: 09 December 2020

ZTFLH:

P531

Fund:Financially supported by the National Science and Technology Major Project of China(No.2016ZX05004006-001-002)

Corresponding Authors: Zhong Shou-Kang,born in 1995,master,is mainly engaged in carbonate deposition and reservoir. E-mail: zhongsk95@163.com.

About author: Huang Dao-Jun,born in 1979,is mainly engaged in oil and gas geological exploration work. E-mail: hdj_cq@petroChina.com.cn.

Cite this article:

Huang Dao-Jun,Zhong Shou-Kang,Zhang Dao-Feng et al. Datailed characterization and interpretation of sedimentary sequences under evaporitic environments: a case from the Ma5₆ submember of Middle Ordovician in central Ordos Basin[J]. JOPC, 2021, 23(4): 735-755.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2021.04.047 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2021/V23/I4/735

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