Paleoenvironment and origin of heavy oil of the lower Cretaceous-Oligocene: a case study

Zhou, Zengyuan; Wang, Shaochun; Yang, Dexiang; Chen, Shuguang; Wu, Jianping; Zhang, Wenjun; Liu, Jing; Wang, Huilai

doi:10.1080/15567036.2021.1936695

Cited by 1 publication

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“…The abundance, type, maturity, and distribution of organic matter in source rocks determine the potential of hydrocarbon resources in oil-bearing basins. ,− Three hydrocarbon source rocks were evaluated: Carboniferous mudstone-Carbonaceous mudstone, Permian Dishuiquan Formation dark mudstone, and Jurassic coal-mudstone-carbonaceous mudstone (Table ). More than 70% of the samples had TOC greater than 1.0% and S 1 + S 2 greater than 6.0 mg/g, and the organic matter abundance index shows that Permian and Jurassic source rocks have also reached the standard of good to excellent source rocks (Figure ).…”

Section: Resultsmentioning

confidence: 99%

Origin and Genesis of the Permain Hydrocarbon in the Northeast of the Dongdaohaizi Depression, Junggar Basin, China

Zhou

et al. 2022

ACS Omega

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Dongdaohaizi area is an important hydrocarbon-rich depression in the Junggar Basin. Early resource evaluation has revealed that it has superior hydrocarbon generation conditions. No major exploration breakthrough has been observed in the hydrocarbon from the Permian Pingdiquan Formation source rocks, which are widely distributed and have a large sedimentary thickness. The unclear recognition of the genesis, the sources, and the hydrocarbon evolution history of the formation seriously restricted further exploration and development. Sixty-four samples were acquired during the study, consisting of 30 source rocks, 13 crude oil samples, and 21 natural gas samples. Studying the geochemical characteristics of the source rock extract and the surrounding structural crude oil in the Dongdaohaizi Depression, the differences in the stable carbon isotope, the biomarker compound, and the molecular relative composition of the three sets of main source rock products in the research fields are summarized. The results reflect that the drying coefficient of natural gas in the study area is generally low, and the fractional distillation value of methane and ethane is 0.32, which is most likely due to the loss of oil and gas migration and the mixing of different types of natural gases. The carbon isotope value is relatively low, with the Pr/Ph being generally less than 3.0. The content of sterane C 29 is the highest in the relative composition of steranes, followed by the content of sterane C 28 , which together account for more than 80% of the total sterane content, and then followed by a lower content of C 27 sterane, accounting for only 5–20% of the total content, which generally conforms to the characteristics of Permian Pingdiquan Formation source rock products. The carbon isotope value of crude oil ranges from −30.94 to −28.31‰, which is different from the characteristics of typical Permian source rocks (values range from −34.49 to −28.21‰), while it is related to typical Carboniferous products (values range from −29.98 to −24.1‰), indicating that small amounts of Carboniferous source rock products were mixed in different degrees in the Dinan fault area. According to the distribution law of oil and gas, the geochemical characteristics and hydrocarbon sources were considered the oil source in the east of the Dongdaohaizi Depression, mainly from the source rocks of the Permian Pingdiquan Formation. The products of the peak period of hydrocarbon generation in the source rocks of the Pingdiquan Formation have not been transported to the high structural positions on a large scale to form reservoirs. They may still exist in the deep part of the Depression and the slope area. The low-amplitude structural and lithologic traps in the slope area of the Dongdahaizi Depression are promising targets for finding the products of the peak period of hydrocarbon generation. This is of great significance to reveal the Permain hydrocarbon evolution in the Junggar Basin ...

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