An Improved Method for Evaluating Hydrocarbon Generation of Shale: A Case Study of the Lower Cretaceous Qingshankou Formation Shale in Songliao Basin

IF 3.5 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Acta Geologica Sinica ‐ English Edition Pub Date : 2023-08-10 DOI:10.1111/1755-6724.15102
Yuchen Zhang, Min Wang, Jinbu Li, Chen Zhao, Yunkui Yan, Liangye Xu, Zixiao Deng
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Abstract

Because of the influence of hydrocarbons, especially adsorbed hydrocarbons, on the detection of cracked hydrocarbon (S2) and total organic carbon (TOC), the hydrogen index (HI) based hydrocarbon generation model deviates from actual practice. In this study, the shale in the first member of the Qingshankou Formation in the central depression of the Songliao Basin was taken as the research object and a correction method for S2 and TOC was established. By correcting the experiment results of different maturity samples, the actual hydrocarbon generation model was revealed, the differences before and after correction were compared, and the evolution characteristics of the adsorbed hydrocarbon content were clarified. The results showed that the organic matter enters the hydrocarbon generation threshold at Ro–0.5% and reaches the hydrocarbon generation peak at Ro–1.0% and that the hydrocarbon generation process ends at Ro–1.3%. The hydrocarbon generation model established based on the measured values has a “lag effect” compared to actual values, which extends the hydrocarbon generation window of organic matter and delays the hydrocarbon generation peak. With the increase of maturity, adsorbed hydrocarbon content shows the characteristics of “first increasing, then stabilizing, and then decreasing”, and reaches the most abundant stage at Ro of 0.9%–1.3%.
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页岩生烃评价方法的改进——以松辽盆地下白垩统青山口组页岩为例
由于烃类尤其是吸附烃类对裂解烃(S2)和总有机碳(TOC)检测的影响,基于氢指数(HI)的生烃模型与实际存在偏差。本研究以松辽盆地中央凹陷青山口组一段页岩为研究对象,建立了S2和TOC的校正方法。通过对不同成熟度样品的实验结果进行校正,揭示了实际生烃模式,对比了校正前后的差异,明确了吸附烃含量的演化特征。结果表明,有机质在Ro-0.5%时进入生烃阈值,在Ro-1.0%时达到生烃高峰,在Ro-1.3%时结束生烃过程。根据实测值建立的生烃模型与实际值相比存在“滞后效应”,延长了有机质生烃窗口期,推迟了生烃高峰期。随着成熟度的增加,吸附烃含量呈现“先增加后稳定再降低”的特征,在Ro为0.9% ~ 1.3%时达到最富集阶段。
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来源期刊
Acta Geologica Sinica ‐ English Edition
Acta Geologica Sinica ‐ English Edition 地学-地球科学综合
CiteScore
3.00
自引率
12.10%
发文量
3039
审稿时长
6 months
期刊介绍: Acta Geologica Sinica mainly reports the latest and most important achievements in the theoretical and basic research in geological sciences, together with new technologies, in China. Papers published involve various aspects of research concerning geosciences and related disciplines, such as stratigraphy, palaeontology, origin and history of the Earth, structural geology, tectonics, mineralogy, petrology, geochemistry, geophysics, geology of mineral deposits, hydrogeology, engineering geology, environmental geology, regional geology and new theories and technologies of geological exploration.
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