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BAI Zhongkai, XIE Li, HAN Miao, LÜ Xiuxiang, SUN Zhichao, LI Qingyao, YANG Youxing, ZHANG Jinhu. 2018. Paleoproductivity conditions of lower member of Cambrian Xiaoerbulak Formation in Kalpin thrust belt, Tarim Basin[J]. Geology in China, 45(2): 227-236. doi: 10.12029/gc20180202
Citation: BAI Zhongkai, XIE Li, HAN Miao, LÜ Xiuxiang, SUN Zhichao, LI Qingyao, YANG Youxing, ZHANG Jinhu. 2018. Paleoproductivity conditions of lower member of Cambrian Xiaoerbulak Formation in Kalpin thrust belt, Tarim Basin[J]. Geology in China, 45(2): 227-236. doi: 10.12029/gc20180202
shu

Paleoproductivity conditions of lower member of Cambrian Xiaoerbulak Formation in Kalpin thrust belt, Tarim Basin

  • 1.

    Oil & Gas Survey, China Geological Survey, Beijing 100083, China

  • 2.

    School of Earth Science, China University of Petroleum, Beijing 102249, China

  • 3.

    Key Hydrocarbon Accumulation of Ministry of Education, China University of Petroleum, Beijing 102249, China

    • Fund Project: Supported by China Geological Survey Program (No. DD20160169, 12120115001801 and 12120115001901)
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  • Author Bio: BAI Zhongkai, male, born in 1979, doctor, senior engineer, mainly engages in the basic geological survey of oil and gas; E-mail:baizk@126.com
Received Date:  05 March 2018
Revised Date:  12 March 2018
Publish Date:  25 April 2018
    Abstract

  • Based on geological investigation of several outcrops, the analyses of 75 samples and the previous achievements, the authors studied the paleoproductivity conditions of lower member of Cambrian Xiaoerbulak Formation in Kalpin thrust belt. In order to get the reliable content of biogenic elements, the authors used the Ti element to deduce the terrigenous elemental content of Ba, Cu and Zn and obtain the corrected values of the biogenic elements Baxs, Cuxs and Znxs. According to the results, it can be concluded that the lower member of Cambrian Xiaoerbulake Formation has a high level of paleoproductivity. The values of the biogenic elements Baxs, Cuxs and Znxs of individual layers are higher, and this indicates that individual layers have higher paleoproductivity. The acritarchs microfossils such as Leiomarginata sp., Granomarginata squamacea Volkova, Dictyotidium priscum Kirjanov and Volkova and Lophosphaeridium sp. were found in the Cambrian Xiaoerbulak Formation, and all these factors provided a good material basis for the deposition of organic matter. The identifying indices such as Pr/Ph, V/(V+Ni), U/Th and δCe indicate that the lower member of Cambrian Xiaoerbulak Formation source rocks were developed under a favorable condition with an anaerobic sedimentary environment. The type of organic matter is Type Ⅰ-Ⅱ, and the organic matter has the characteristics of high maturity stage and potential of hydrocarbon generation. In summary, the lower member of Cambrian Xiaoerbulak Formation can be regarded as the potential source rock.

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