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Volume 46 Issue 1
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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2024  >  46(1): 146-157
CAI Qianru, WANG Jinduo, ZHANG Guanlong, SONG Zhihua, WANG Shengzhu, XIONG Zhengrong, NI Shengli. Research on sedimentary environment and provenance for hydrocarbon source rocks of Upper Carboniferous Batamayineishan Formation in northeastern Junggar Basin: evidences from the geochemistry of mudstones[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(1): 146-157. doi: 10.11781/sysydz202401146
Citation: CAI Qianru, WANG Jinduo, ZHANG Guanlong, SONG Zhihua, WANG Shengzhu, XIONG Zhengrong, NI Shengli. Research on sedimentary environment and provenance for hydrocarbon source rocks of Upper Carboniferous Batamayineishan Formation in northeastern Junggar Basin: evidences from the geochemistry of mudstones[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(1): 146-157. doi: 10.11781/sysydz202401146
shu

Research on sedimentary environment and provenance for hydrocarbon source rocks of Upper Carboniferous Batamayineishan Formation in northeastern Junggar Basin: evidences from the geochemistry of mudstones

doi: 10.11781/sysydz202401146
  • 1.

    Exploration and Development Research Institute of SINOPEC Shengli Oilfield Branch Company, Dongying, Shandong 257000, China

  • 2.

    Postdoctoral Research Workstation of SINOPEC Shengli Petroleum Management Bureau, Dongying, Shandong 257000, China

  • Received Date: 2023-05-29
  • Rev Recd Date: 2023-12-06
  • Publish Date: 2024-01-28
    Abstract
  • The distribution rules and hydrocarbon potential of source rocks are the major factors which determine oil and gas exploration in the northeastern Junggar Basin. Sedimentary background and environmental changes are the main factors controlling the genesis, distribution, and organic matter types of hydrocarbon source rocks. The main and trace elements and rare earth elements in sedimentary rocks are often influenced by palaeoclimate, paleo water chemical conditions, palaeoenvironment, and palaeosource during sedimentation process. Therefore, a comprehensive analysis of the distribution patterns of elements in sedimentary rocks can help to determine sedimentary environment and evolution process. The geochemical characteristics of major and trace elements and rare earth elements for mudstones of the Upper Carboniferous Batamayineishan Formation from outcrops of the north- eastern Junggar Basin were studied to reveal the sedimentary environment and the tectonic setting of the provenance, which can provide geological constraints for the origin and development conditions of hydrocarbon source rocks. According to a comprehensive analysis on chemical weathering indicators, element contents, and ratios between various major and trace elements, the mudstones of Batamayineishan Formation were deposited in a warm and humid paleoclimate background, and the deposition process was relatively stable in a shallow water with brackish-fresh features under oxidizing environment. Major and trace elements of mudstones indicate that the parent rocks are sedimentary rocks and felsic volcanic rocks and their provenance is derived from the weathering products of acidic igneous rocks of the Karamaili Island Arc, reflecting the tectonic transition from compression to extension during the post collision stage. The depositional environment and tectonic setting controlled the increased input of terrestrial higher plants, resulting in the medium abundance of organic matter with good hydrocarbon generating potential.

     

    • All authors disclose no relevant conflict of interests.
    The study was mainly organized by CAI Qianru. The experimental operation was completed by WANG Jinduo, ZHANG Guanlong, SONG Zhihua, XIONG Zhengrong and NI Shengli. The manuscript was drafted and revised by CAI Qianru, WANG Jinduo, ZHANG Guanlong and WANG Shengzhu. All the authors have read the last version of paper and consented for submission.
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