首页|珠江口盆地HZ26区文昌组储层特征及成因机制

珠江口盆地HZ26区文昌组储层特征及成因机制

扫码查看
珠江口盆地惠州凹陷油气资源丰富,文昌组勘探主要受限于储层.以惠州凹陷HZ26区文昌组砂岩储层为研究对象,采用薄片鉴定、扫描电镜、包裹体测温等手段,对储层特征、增孔保孔机制、成岩成储过程展开研究.结果表明:①文昌组以岩屑砂岩、岩屑石英砂岩储层为主,粒间普遍含凝灰质杂基,文昌组储层整体表现为低孔、低渗.②早成岩A期大气淡水溶蚀作用和早成岩B期—中成岩A期有机酸溶蚀作用是储层最主要的增孔机制,早成岩阶段沉淀的嵌晶式浊沸石可以有效抵御压实作用从而保护粒间孔隙,早期油气充注也可以通过抑制胶结作用而保护粒间孔隙.③文昌组WC41、WC42、WC43砂层组的成岩成储过程具有明显差异.WC41砂层组原生孔发育带整体杂基含量少,成岩演化过程简单,油气沿断层处运移,在上覆不整合遮挡下形成油气藏;WC42砂层组广泛分布凝灰质杂基,凝灰质蚀变作用普遍发育,沉淀出可以提高岩石抗压性的致密胶结浊沸石,浊沸石被酸溶解后,提供大量粒间溶蚀孔,浊沸石溶解带是研究区油气聚集的另一有利场所;WC43砂层组远火山口端的富泥质杂基带和近火山口端的火山角砾堆积带均遭受强烈压实作用,储集性能差.本项研究成果可为HZ26区文昌组油气勘探决策提供参考.
Characteristics and genetic mechanisms of reservoirs of Wenchang Formation in the HZ26 area of Huizhou sag,Pearl River Mouth basin
Huizhou sag of the Pearl River Mouth basin is rich in oil and gas resources,and the exploration of Wenchang Formation is limited by reservoirs.Taken sand reservoirs of Wenchang Formation in the HZ26 area of Huizhou sag as research object,researches focusing on reservoir characteristics,mechanism of pore increase and preservation,process of diagenesis and reservoir-forming were conducted through applying thin section identification,scanning electron microscopy,inclusion temperature measurement,etc..The results show that:①The reservoirs of Wenchang Formation are dominated by litharenites and lithic quartz sandstones,and tuffaceous matrix is pervasively distributed among grains.②Meteoric fresh water dissolution in eodiagenesis A stage and organic acid dissolution in eodiagenesis B and mesodiagenesis A stage are the most important pore increasing mechanisms.The poikilitic laumontites deposited in eodiagenesis stage can effectively resist compaction and protect the intergranular pores,and the early hydrocarbon charging can also protect the intergranular pores by inhibiting cementation.③ The diagenesis and reservoir-forming processes of WC41,WC42,and WC43 sand groups in Wenchang Formation are remarkably different.The primary pore development zone of WC41 sand group has a low content of matrix and a simple diagenetic evolution process.Oil and gas migrated along the faults and accumulated under the overlying unconformity.Tuffaceous matrix is widely distributed within WC42 sand group and tuffaceous alteration was generally developed,with laumontites,which are able to improve the resistance to compaction of rock,precipitated.After the dissolution of laumontites by acid,a large number of intergranular dissolution pores were formed.The laumontite dissolution zone is another favorable place for oil and gas accumulation in the study area.For WC43 sand group,both the mud and matrix-rich zone proximal to crater and the volcanic breccia buildup zone distal to crater suffered from intense compaction,and the reservoir quality is poor.The research results can provide a reference for oil and gas exploration of Wenchang Formation in the HZ26 area.

Pearl River Mouth basinHuizhou saghigh-quality reservoirWenchang Formationdiagenetic evolutionpore increase and preservation

傅筱涵、李晓艳、丁琳、靳子濠、刘培、王宇辰、远光辉

展开 >

中国石油大学(华东)深层油气全国重点实验室 山东青岛 266580

中海石油(中国)有限公司深圳分公司 广东深圳 518067

海洋国家实验室海洋矿产资源评价与探测技术功能实验室 山东青岛 266071

珠江口盆地 惠州凹陷 优质储层 文昌组 成岩演化 增孔保孔

国家自然科学基金优秀青年基金崂山实验室科技创新项目

42222208LSKJ202203402

2024

中国海上油气
中海石油研究中心

中国海上油气

CSTPCD北大核心
影响因子:1.266
ISSN:1673-1506
年,卷(期):2024.36(2)
  • 24