中国湖相碳酸盐岩时空分布与碳氧同位素特征<sup>*</sup>

doi:10.7605/gdlxb.2017.06.082

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Abstract Lacustrine carbonate rocks have various occurrences. They commonly occur as the interbeds in clastic rocks with characteristics of multi-layers,thin individual layer and rhythm. Occasionally,they occur in mudstone and shale as thin layers of concretions or calcareous microfossils. Controlled by tectonic background,provenance and palaeoenvironment,the lacustrine carbonate rocks in China show wide spatial-temporal distribution,which were firstly reported in the Permian,but mainly found in the Paleogene. Based on carbonate and oxygen isotope analysis,different water environments during primary deposition and diagenetic process are concluded: (1)Well-related δ¹³C and δ¹⁸O with mostly positive δ¹³C values,indicating a closed saltwater or semi-saltwater lake environment;(2)Completely-unrelated δ¹³C and δ¹⁸O values with mostly negative δ¹³C values,indicating an open lake environment;(3)Seriously-positive δ¹³C values,indicating that during diagenesis,the environment was affected by the methane generation process,which was participated by archaebacteria.

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	Articles by authors
	Su Ling
	Zhu Rukai
	Cui Jingwei
	Wu Songtao
	Luo Zhong
	Mao Zhiguo
	Li Sen

Key words： carbonates rock carbon and oxygen isotope open lake closed lake fermentation methanogenesis

Received: 20 March 2017

ZTFLH:

P597+.2

Fund:Financially supported by the National Program on Key Basic Research Project(973 Program)in China“Formation mechanism and enrichment regularity of tight oil(shale oil)in China”(No.2014CB239000)

Corresponding Authors: 　Zhu Rukai,born in 1968,is engaged in research of reservoir sedimentology. E-mail: zrk@petrochina.com.cn.

About author: Su Ling,born in 1982,is engaged in research of reservoir sedimentology. E-mail: suling2200@petrochina.com.cn.

Cite this article:

Su Ling,Zhu Rukai,Cui Jingwei et al. Spatial-temporal distribution of lacustrine carbonate rocks in China and their carbon and oxygen isotopic characteristics[J]. JOPC, 2017, 19(6): 1063-1074.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2017.06.082 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2017/V19/I6/1063

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