Comprehensive thermal maturity assessment in shales: a case study on the upper cretaceous Qingshankou formation (Songliao Basin, NE China)

被引:9
|
作者
Zhang, Penglin [1 ]
Misch, David [2 ]
Meng, Qingtao [1 ,3 ]
Bechtel, Achim [2 ]
Sachsenhofer, Reinhard F. [2 ]
Liu, Zhaojun [1 ,3 ]
Gao, Fuhong [1 ]
Hu, Fei [1 ,3 ]
Zhang, Shuaihua [1 ]
Tang, Baiqiang [1 ]
机构
[1] Jilin Univ, Coll Geosci, Changchun 130061, Peoples R China
[2] Univ Leoben, Dept Appl Geosci & Geophys, Peter Tunner Str 5, A-8700 Leoben, Austria
[3] Key Lab Oil Shale & Symbiot Energy Minerals, Changchun 130061, Jilin, Peoples R China
基金
中国国家自然科学基金;
关键词
Thermal maturity; Qingshankou formation; Shale; Clay minerals; Organic geochemistry;
D O I
10.1007/s00531-021-02000-4
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Songliao Basin is the largest Early Cretaceous lacustrine rift basin of northeast China and hosts tremendous conventional and unconventional petroleum resources. However, the distribution of shale oil is not well constrained, as production from source rock reservoirs requires certain thermal maturity cut-offs (vitrinite reflectance of > 0.8%Rr). In this study, the thermal maturity of the Qiangshankou Formation along the Southern Uplift and in the Central Depression of the Songliao Basin was evaluated by combining traditional and advanced petrographic and geochemical maturity proxies with clay mineralogical investigations. The Qingshankou Formation is one of the major source rocks of the region, but previous studies encountered difficulties in obtaining reliable maturity data, mainly due to strongly shifted T-max values. Equally, T-max determined during this study showed apparent shifting likely caused either by retained solid bitumen or by variations in kerogen type. In contrast, the measured vitrinite reflectance shows a reliable depth trend, meeting the shale oil cut-off maturity of 0.8%Ro at a drilling depth of similar to 2300 m, which is only reached in the Central Depression of the basin. The vitrinite reflectance trend is supported by changes in clay mineralogy, such as the progressing ordering of I/S mixed layers ("Reichweite"), increasing illitization, decreasing detrital kaolinite and correspondingly increasing authigenic chlorite contents. Maturity-related biomarker proxies are only partly valid; while the methylphenanthrene index (MPI-1) and the trimethylnaphthalene ratio (TNR-1) show reliable maturity trends even over short depth intervals, other established proxies (e.g. based on alkylbiphenyls) proved insensitive to changes from immature to peak oil mature and are, therefore, not recommended for further use in studies on Qingshankou Fm. shales. In summary, the combination of various maturity parameters improves the understanding of shale oil distribution in the central Songliao Basin, providing valuable insights for studies on similar unconventional targets in the region.
引用
收藏
页码:943 / 962
页数:20
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