非海相页岩沉积学研究进展与趋势——以松辽盆地大庆油田古龙页岩为例

IF 7 Q1 ENERGY & FUELS
Longde SUN , Rukai ZHU , Tianshu ZHANG , Yi CAI , Zihui FENG , Bin BAI , Hang JIANG , Bo WANG
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引用次数: 0

摘要

以松辽盆地上白垩统青山口组古龙页岩为例进行了研究。通过古湖位重建,综合分析青山口组湖盆沉积的层状类型、岩相垂直组合、沉积演化阶段及控制因素,探讨青山口组沉积时期湖水、古气候、陆相碎屑供给强度的旋回变化。研究了岩相组成/构造对含油性能的影响、储层性能与岩相组成/构造的关系、岩相力学性质的差异以及不同岩相中页岩油的赋存和可动性。研究结果对页岩油富集层/带的评价具有重要指导意义。非海相页岩沉积学有望在沉积岩石学和石油地质学的基础上发展成为一门跨学科的科学,揭示矿物、有机质、孔隙、流体和相在运移、沉积、水岩相互作用、成岩和演化过程中的物理、化学和生物作用以及分布特征和演化模式。主要从八个方面进行研究:非海相页岩层序地层格架下岩相及有机质分布预测;基于沉积正演模拟的页岩岩相古地理非海相页岩纹层成因及纹层组合测井识别页岩有机质来源及富集过程非海相页岩岩相刚性颗粒+塑性组分+孔隙裂缝体系分类页岩成岩作用多场耦合有机-无机相互作用机制页岩储层多尺度表征新方法及智能岩心技术以及页岩储层非均质性定量评价与智能分析系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Advances and trends of non-marine shale sedimentology: A case study from Gulong Shale of Daqing Oilfield, Songliao Basin, NE China
This study took the Gulong Shale in the Upper Cretaceous Qingshankou Formation of the Songliao Basin, NE China, as an example. Through paleolake-level reconstruction and comprehensive analyses on types of lamina, vertical associations of lithofacies, as well as stages and controlling factors of sedimentary evolution, the cyclic changes of waters, paleoclimate, and continental clastic supply intensity in the lake basin during the deposition of the Qingshankou Formation were discussed. The impacts of lithofacies compositions/structures on oil-bearing property, the relation between reservoir performance and lithofacies compositions/structures, the differences of lithofacies in mechanical properties, and the shale oil occurrence and movability in different lithofacies were investigated. The insights of this study provide a significant guideline for evaluation of shale oil enrichment layers/zones. The non-marine shale sedimentology is expected to evolve into an interdisciplinary science on the basis of sedimentary petrology and petroleum geology, which reveals the physical, chemical and biological actions, and the distribution characteristics and evolution patterns of minerals, organic matter, pores, fluid, and phases, in the transportation, sedimentation, water-rock interaction, diagenesis and evolution processes. Such research will focus on eight aspects: lithofacies and organic matter distribution prediction under a sequence stratigraphic framework for non-marine shale strata; lithofacies paleogeography of shale strata based on the forward modeling of sedimentation; origins of non-marine shale lamina and log-based identification of lamina combinations; source of organic matter in shale and its enrichment process; non-marine shale lithofacies classification by rigid particles + plastic components + pore-fracture system; multi-field coupling organic-inorganic interaction mechanism in shale diagenesis; new methods and intelligent core technology for shale reservoir multi-scale characterization; and quantitative evaluation and intelligent analysis system of shale reservoir heterogeneity.
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