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Differential Diagenetic Evolution and the Mechanism of Low‐Porosity, Ultra‐Low‐Permeability Sandstone Reservoirs in the Jurassic Badaowan Formation, Central Depression of the Junggar Basin, China

成岩作用 地质学 构造盆地 多孔性 中国 萧条(经济学) 磁导率 地球化学 差速器(机械装置) 古生物学 岩石学 岩土工程 化学 考古 地理 经济 工程类 宏观经济学 航空航天工程 生物化学
作者
Jingyi Wang,Huixi Lin,Fujie Jiang,Qinhong Hu,Dingye Zheng,Fushun Zhang
出处
期刊:Geological Journal [Wiley]
标识
DOI:10.1002/gj.70001
摘要

ABSTRACT The aim of this study is to investigate the diagenetic processes and their impact on reservoir quality within the Jurassic Badaowan Formation of the Junggar Basin. Various experimental techniques were employed, including thin section petrography, scanning electron microscopy, x‐ray diffraction, and fluid inclusion micro‐thermometry, to characterise the rock composition, pore types, and diagenetic alterations from core samples of nine wells in the study area. The results reveal that the compaction and cementation are the dominant factors contributing to reservoir densification, with porosity significantly reduced by mechanical compaction and carbonate cementation. A total of four facies were identified based on diagenetic strength and sedimentary cycle associated with different diagenesis stages and reservoir physical‐property responses: (1) “Low‐plastic lithic weak compaction facies (LPLF)” occurred the cementation of chlorite rims at the early diagenetic stage and multiple stages of cementation and dissolution at the middle diagenesis stage; (2) “Volcanic lithic‐rich dissolution facies (VLDF)” was the characteristic of weak compaction at the early diagenetic stage and intense dissolution and weak cementation of middle diagenesis stage; and (3) “Calcareous cemented facies (CCF)” and (4) “carbonaceous‐laminated strongly compacted dense facies (CLCF)” underwent strong cementation and compaction respectively at the early diagenetic stage resulting in a tight reservoir. Dissolution processes, primarily driven by acidic fluids from coal‐bearing strata, enhance secondary porosity development, particularly in feldspar and volcanic rock fragments. However, in certain lithofacies, these improvements are offset by extensive calcite and siderite cementation, reducing permeability and hindering fluid flow. The study concludes that the diagenetic heterogeneity plays a critical role in reservoir quality variation across the Badaowan Formation, with the findings providing valuable insights into the differential diagenesis evolution of reservoir quality for improving hydrocarbon exploration strategies in similar geological settings.
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