渤中凹陷南部东二下段湖底扇储层控制因素 及孔隙定量演化

作    者:刘濮毓1,2,龚承林1,2,彭旸1,2,黄晓波3,王启明3,李东伟1,2,王海屹1,2
单    位:1 油气资源与工程全国重点实验室;2 中国石油大学(北京)地球科学学院; 3 中海石油(中国)有限公司天津分公司
基金项目:
摘    要:
渤中凹陷南部渐新统东二下段处于深水湖盆沉积环境,优质湖相烃源岩和大规模湖底扇广泛发育,是岩性 油气藏勘探的有利区。基于录测井数据、岩石粒度、显微薄片、扫描电镜、流体包裹体等资料,开展渤中凹陷南部东二 下段湖底扇储层特征与储层主控因素研究,建立孔隙定量演化模型。研究结果表明:东二下段湖底扇储层岩性以 中—细粒岩屑石英长石砂岩为主,孔隙以溶蚀孔为主;湖底扇朵叶复合体内部的朵叶核部、分支水道等有利沉积相带 是优质储层形成的基础;持续的压实作用和早晚两期胶结作用是导致孔隙不断损失的主因;有机酸溶蚀和异常高压 保孔促溶是改善储层质量的关键。在埋藏过程中储层孔隙演化经历了早成岩A期快速压实减孔、早成岩B期快速压 实-胶结减孔、中成岩A1期缓慢压实减孔-有机酸溶蚀增孔和中成岩A2期缓慢压实-胶结作用减孔等4个阶段,其中 压实减孔总量为13.64%,早期胶结减孔量为8.24%,溶蚀增孔量为9.55%,尤其是发生在中成岩A1期末油气开始充注 成藏之后的晚期胶结减孔量为7.12%,造成储层孔隙度显著降低。
关键词:湖底扇砂岩;成岩作用;储层控制因素;孔隙定量演化;渐新统;渤中凹陷南部

Control factors and quantitative pore evolution of sublacustrine fan reservoirs in lower section of the second member of Oligocene Dongying Formation in southern Bozhong Sag

Author's Name: LIU Puyu1,2, GONG Chenglin1,2, PENG Yang1,2, HUANG Xiaobo3, WANG Qiming3, LI Dongwei1,2, WANG Haiyi1,2
Institution: 
Abstract:
High-quality lacustrine source rock and extensive sublacustrine fans are developed in deep-lacustrine depositional environment in lower section of the second member of Oligocene Dongying Formation (E3d2l) in southern Bozhong Sag, providing an exploration realm of lithological reservoirs. However, the generally poor porosity and permeability of the deep reservoirs severely hampered the progress for oil and gas exploration and development. Thus, there is an urgent need to elucidate the key factors and the pore evolutionary processes controlling the sandstone reservoir quality of the sublacustrine fans. Based on comprehensive analysis of drilling and logging data, rock grain-size, thin sections, scanning electron microscopy and fluid inclusions, this study has successfully identified the key factors controlling reservoir quality, and established quantitative models of pore evolution. The results show that: The sublacustrine fan reservoir of the E3d2l is characterized by predominantly medium-fine grained lithic feldspathic quartz sandstone with mainly dissolution pores. The favorable sedimentary units such as lobe axis and distributary channels in sublacustrine fan are the basis for the formation of high-quality reservoirs. Persistent compaction and early / late cementation are the main causes of continuous porosity loss. Organic acid dissolution and abnormally high pressure are the key factors for improving reservoir quality. The sublacustrine fan sandstone undergoes four stages during the burial process: rapid compaction in the early diagenesis A phase, rapid compaction and early cementation in the early diagenesis B phase, slow compaction and organic acid dissolution in the middle diagenesis A1 phase, and slow compaction and late cementation in the middle diagenesis A2 phase. During these phases the compaction and early cementation reduce porosity by 13.64% and 8.24% respectively, and organic acid dissolution increases porosity by 9.55%. In particular, the late cementation after the oil and gas accumulation results in a severe porosity decrease of 7.12%. This study will provide a theoretical basis for the oil and gas exploration and development of sublacustrine fan reservoirs in the deep-lacustrine basin of the Bohai Sea.
Keywords: sublacustrine fan sandstone; diagenesis; controlling factors of reservoir; quantitative pore evolution; Oligo⁃ cene; southern Bozhong Sag
投稿时间: 2024-07-09  
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