孔隙演化定量分析及其在盆地模拟中的应用——以鄂尔多斯盆地合水地区长6储层为例

IF 3.6
Ting Shang , Meijuan Chu , Xiaolei Zhang , Bin Wang , Jihong Li , Huiruo Zhang , Zhongyi Zhang , Xin Liu
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引用次数: 0

摘要

近年来,随着鄂尔多斯盆地石油勘探技术的显著进步,越来越多的低渗透或超低渗透储层被发现。阐明其储层特征和形成机制已成为油气可持续开发的重要课题。以鄂尔多斯盆地合水地区上三叠统延长组长6段为研究对象,对其岩石学特征、孔渗特征、成岩作用及成岩演化序列进行了系统研究。通过岩心观察、薄片识别和物性测量相结合,对储层孔隙演化进行了综合定量评价。这些分析结果随后应用于模拟油气运移和聚集。这些研究成果将为深入定量研究特低渗透油藏孔隙演化和准确构建盆地模型提供科学依据。研究区储层岩性以粉砂岩与泥岩或泥质粉砂岩互层为主,具有低孔低渗的特点。在现有孔隙度数据约束下,通过基于成岩特征的重构,定量模拟了成岩过程中孔隙演化。模拟的孔隙演化与实际地质观测结果一致,验证了方法的可靠性。利用PetroMod软件将孔隙演化量化结果应用于油气运移模拟,发现盆地油气充注始于晚侏罗世(J3)末,早白垩世(K1)末达到生、排烃和成藏高峰期,并在晚白垩世保持较高的成藏速率,但在目前阶段明显下降。通过与实际钻井数据的对比,验证了模拟结果的可靠性和对其他类似油田的适用性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Quantitative analysis of pore evolution and its application in basin simulation:A case study of Chang 6 reservoir in Heshui area, Ordos Basin, NW China

Quantitative analysis of pore evolution and its application in basin simulation:A case study of Chang 6 reservoir in Heshui area, Ordos Basin, NW China
In recent years, fueled by significant advancements in oil exploration technologies within the Ordos Basin, an increasing number of low-permeability or ultra-low-permeability reservoirs have been identified. Elucidating their reservoir characteristics and formation mechanisms has become a critical priority for sustainable hydrocarbon development. The study focused on the Chang 6 Member of the Upper Triassic Yanchang Formation in the Heshui area of the Ordos Basin, systematically investigating its petrological features, porosity and permeability characteristics, diagenesis, and diagenetic evolution sequence. By integrating core observation, thin-section identification, and physical property measurements, a comprehensive quantitative evaluation of reservoir pore evolution was performed. These analytical outcomes were subsequently applied to simulate hydrocarbon migration and accumulation. These research results will provide a scientific basis for in-depth quantitative study of the pore evolution in ultra-low-permeability oil reservoirs and accurately constructing basin models. As indicated, the reservoir lithology in the study area predominantly comprises siltstone interbedded with mudstone or argillaceous siltstone, characterized by low porosity and permeability. Through diagenetic characteristics-based reconstruction constrained by the existing porosity data, pore evolution during diagenesis was quantitatively modeled. The simulated pore evolution aligns with actual geological observations, validating the reliability of the methodology. Furthermore, the quantified pore evolution results were applied to simulate hydrocarbon migration using PetroMod software, showing that hydrocarbon charging in the basin began at the end of the Late Jurassic (J3), peaking in hydrocarbon generation, expulsion, and accumulation by the end of the Early Cretaceous (K1) and maintaining high accumulation rates until the late Cretaceous, though significantly decreasing at the present stage. The simulation results were verified by comparison with actual drilling data, which confirms their reliability and applicability to other analogous oilfields.
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