通过整合图像和核磁共振测井,确定深层和超深层致密砂岩的孔隙结构特征并预测储层质量

IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Yang Su , Jin Lai , Wenle Dang , Kang Bie , Yidi Zhao , Xinjian Zhao , Dong Li , Fei Zhao , Guiwen Wang
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引用次数: 0

摘要

孔隙结构和裂缝决定了深层和超深层致密砂岩的储层质量,然而,由于岩心数据有限,描述孔隙-咽喉结构的复杂性和各种裂缝的特征具有挑战性。为了填补这一空白,我们开展了一项综合分析,从多个角度评估孔隙结构和裂缝。综合利用岩心、薄片、扫描电子显微镜(SEM)、高压注汞(HPMI)和核磁共振(NMR)测试,对库车凹陷白垩纪巴什吉其克地层深部和超深部致密砂岩的孔隙结构和裂缝特征进行了评价。根据核磁共振横向弛豫时间(T2)分布和 HPMI 曲线的特征,孔隙结构和储层质量类型主要分为三种。HPMI和核磁共振参数与岩石物理参数的相关性分析表明,最大孔喉尺寸(rmax)、T2对数平均值(T2gm)、不可还原水饱和度(Swi)和储层质量指数(RQI)是孔隙结构特征最敏感的参数。Ⅰ型孔隙结构由粒间孔隙和粒内孔隙组成,核磁共振 T2 谱显示的幅度最大,计算出的流动流体饱和度含量也最高。Ⅱ型和Ⅲ型孔隙结构由粘土矿物中的粒间孔隙、粒内溶解孔隙和晶间微孔组成。利用图像测井和岩心分析了断裂特征和参数,包括断裂密度、孔隙度、孔径和长度。通过核磁共振测井对孔隙结构特征进行定量和定性分析。通过图像测井和核磁共振测井对孔隙结构和裂缝进行综合分析,可用于预测优质储层和油气生产率。天然裂缝丰富的井段可获得较高的油气生产率,良好的孔隙结构也有助于提高基质孔隙度。因此,核磁共振测井和图像测井与岩心和分析数据校准后,对评估储层质量和预测生产率至关重要。将岩心数据与地球物理测井曲线结合起来进行综合分析,为预测深层和超深层致密砂岩的储层质量提供了重要依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Pore structure characterization and reservoir quality prediction in deep and ultra-deep tight sandstones by integrating image and NMR logs

Pore structure and fracture determine reservoir quality in deep and ultra-deep tight sandstones, however, the limited availability of core data makes it challenging to describe the complexity of pore-throat structure and characterize the wide range of fractures. To fill this gap, a comprehensive analysis was conducted to evaluate pore structure and fractures from multiple perspectives. Integration of core, thin sections, scanning electron microscopy (SEM), high pressure mercury injection (HPMI) and nuclear magnetic resonance (NMR) tests are used to evaluate pore structure and characterize fracture of deep and ultra-deep tight sandstones in the Cretaceous Bashijiqike Formation in the Kuqa Depression. Pore structure and reservoir quality types can be divided into dominantly three types according to characteristics of NMR transverse relaxation time (T2) distribution and HPMI curves. Correlation analysis among HPMI and NMR parameters with petrophysical parameters indicate that maximum pore throat size (rmax), logarithmic mean of T2 (T2gm), irreducible water saturation (Swi), and reservoir quality index (RQI) are the most sensitive parameters for pore structure characterization. The Type Ⅰ pore structure is composed of intergranular and intragranular pores, and NMR T2 spectrum shows the highest magnitude, with the calculated mobile fluid saturation content also being the highest. The Type II and III pore structures are composed of intergranular pores, intragranular dissolved pores and intercrystalline micropores in clay minerals. T2gm of Type II and III are smaller, with the calculated mobile fluid saturation content being the lower.

The fracture features and parameters including fracture density, porosity, aperture, and length are analyzed using image logs and core. The pore structure characteristics are quantificationally and qualitatively analyzed by NMR logs. Integration of pore structure and fractures by image logs and NMR logs are used for prediction of high quality reservoir and hydrocarbon productivity. High hydrocarbon productivity is obtained in well intervals with abundant natural fractures, and favorable pore structure will also contribute to high matrix porosity. Therefore, NMR logs and image logs are crucial for evaluating reservoir quality and predicting productivity when calibrated with core and analysis data. The comprehensive analysis integrating core data with geophysical well logs provide important insights for reservoir quality prediction of deep and ultra-deep tight sandstones.

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来源期刊
Journal of Asian Earth Sciences
Journal of Asian Earth Sciences 地学-地球科学综合
CiteScore
5.90
自引率
10.00%
发文量
324
审稿时长
71 days
期刊介绍: Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review. The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance. The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.
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