Sedimentary Environment and Model for Organic Matter Enrichment: Chang 7 Shale of Late Triassic Yanchang Formation, Southern Margin of Ordos Basin, China

Energies

Lei Li¹  Chunyu Zhang²  Jungang Lu²  Xingcheng Zhu²  Yonggang Zhao³  Shanghua Si³ 

[1] College of Geosciences, China University of Petroleum, Beijing 102249, China;Natural Gas Geology Key Laboratory of Sichuan Province, Southwest Petroleum University, Chengdu 610500, China;School of Earth Sciences and Engineering, Xi’an Shiyou University, Xi’an 710065, China;

关键词: lacustrine shale;    organic matter enrichment;    Late Triassic;    Chang 7;    southern margin of Ordos Basin;   

DOI  :  10.3390/en15082948

来源: DOAJ

【 摘 要 】

Shale oil is an unconventional oil resource that needs to be developed and utilized urgently. However, the Chang 7 shale in the Ordos Basin, as the most typical continental source rock in China, is limited by the study of organic matter (OM) enrichment factors in continental lacustrine facies, and there are still controversies about the controlling factors, which limit the progress of oil and gas exploration. This paper aims to reconstruct the paleoenvironment of Chang 7 shale in the southern margin of Ordos Basin and reveal the controlling factors of organic rich shale by organic and elemental analysis, X-ray diffraction (XRD) analysis, thin section observation, and scanning electron microscopy-energy dispersive spectrometer (SEM-EDS) analysis. The results show that during the deposition period of Chang 7 shale, the climate was warm and humid, the lake water has strong reducing, low salinity and rapid depth changes. Total organic carbon (TOC) is positively correlated with salinity and hydrothermal action and inversely proportional to terrigenous input. The high productivity, low consumption and low dilution result in high enrichment of shale OM in the southern margin of Ordos Basin.

【 授权许可】

Unknown