蜀南地区东部上二叠统长兴组沉积特征及有利储层分布OA
Sedimentary characteristics and favorable reservoir distribution of the Upper Permian Changxing Formation in the eastern part of southern Sichuan Basin
基于露头、薄片及井震资料对蜀南地区东部长兴组进行层序划分与三级格架构建,综合岩相、测井相和地震相特征识别沉积相,并据此分析优质储层主控相带及其有利分布区.研究结果表明:①蜀南地区东部长兴组自下而上可划分为2个三级层序(Sq1和Sq2),早期发育碳酸盐深—浅缓坡沉积,中—晚期发育缓坡型碳酸盐台地沉积.开阔台地相的台内滩亚相主要发育于Sq1-HST和Sq2-HST沉积时期,尤以Sq2-HST沉积时期最发育.滩体在平面上侧向迁移,垂向上局部叠加.②储层岩性以生屑灰岩为主,储集空间以孔隙及裂缝-孔洞为主.储层的形成主要受到沉积相和溶蚀作用的控制,有利储层集中发育在台内滩亚相中,呈分散片状分布.③根据沉积相、滩体和储层发育特征,评价预测3个有利储层发育区和2个潜在有利储层发育区:Z207井—Z201井—Z202井一带、B28井—B61井一带和B24井—G11井一带为有利储层发育区;BH2井—BH3井一带与F7井—N49井一带为储层发育潜在有利区.蜀南地区东部上二叠统长兴组沉积相与有利储集区的系统研究为该区域礁滩领域下一步油气勘探提供了地质依据.
In recent years,driven by the reef-shoal hydrocarbon accumulation theory,it has been confirmed that the intra-platform shoals of the Changxing Formation in the eastern part of southern Sichuan Basin have good gas-bearing properties.However,the sedimentary system and reservoir distribution of the thick-bedded limestone reservoirs remain unclear,thus restricting the deployment of oil and gas exploration.Based on outcrop,thin section,and well-seismic data,this paper carries out sequence division and third-order framework construction of the Changxing Formation,identifies sedimentary facies by integrating lithofacies,logging facies,and seismic facies,and accordingly analyzes the dominant facies belts of high-quality reservoirs and their favorable distribution areas.The results show that:(1)Three sequence boundaries(SB1,SB2 and SB3)are identified in the Changxing Formation in the eastern part of southern Sichuan Basin,which can be further divided into two third-order sequences(Sq1 and Sq2)from bottom to top.In the early stage,carbonate deep-shallow ramp developed;in the middle-late stage,ramp-type carbonate platform developed.Among these,the intra-platform shoal subfacies of the open platform facies mainly developed during the Sq1-HST and Sq2-HST depositional periods,with the most extensive development occurring particularly in the Sq2-HST period.The shoal bodies exhibite a lateral migration trend in the planar distribution and are only locally superimposed vertically.(2)The reservoir lithology is predominantly bioclastic limestone,with pore spaces and fracture-vug systems serving as the main reservoir spaces.The formation of reservoirs is primarily controlled by sedimentary facies and dissolution processes,and favorable reservoir zones concentrated in the intra-platform shoal subfacies,displaying a scattered patchy distribution.(3)According to the sedimentary facies,the development location and thickness of shoal bodies,and the development thickness of reservoirs,three favorable reservoir development areas and two potentially favorable reservoir development areas are evaluated and predicted:the area around Z207-Z201-Z202 well area,the B28-B61 well area,the B24-G11 well area are classified as favorable reservoir development zones;the BH2-BH3 well area and F7-N49 well are the potential favorable reservoir development zones.The systematic study on the sedimentary facies and reservoir characteristics of the thick-bedded limestone of the Upper Permian Changxing Formation in the eastern part of southern Sichuan Basin provides strong guidance for the next step of oil and gas exploration in the reef-shoal field of this area.
王玉苗;胡忠贵;武赛军;谢武仁;陈政安;佟伟桀;赵春晖;马银银
南方复杂页岩油气地质与开发湖北省重点实验室||非常规油气地质与工程湖北省工程研究中心||长江大学地球科学学院南方复杂页岩油气地质与开发湖北省重点实验室||非常规油气地质与工程湖北省工程研究中心||长江大学地球科学学院中国石油勘探开发研究院中国石油勘探开发研究院中国石油勘探开发研究院南方复杂页岩油气地质与开发湖北省重点实验室||非常规油气地质与工程湖北省工程研究中心||长江大学地球科学学院南方复杂页岩油气地质与开发湖北省重点实验室||非常规油气地质与工程湖北省工程研究中心||长江大学地球科学学院南方复杂页岩油气地质与开发湖北省重点实验室||非常规油气地质与工程湖北省工程研究中心||长江大学地球科学学院
能源科技
沉积特征台内滩储层主控因素有利储层分布长兴组蜀南地区东部四川盆地
sedimentary characteristicsintra-platform shoalmain controlling factors of reservoirsfavorable reservoir distributionChangxing Formationeastern part of southern Sichuan BasinSichuan Basin
《海相油气地质》 2026 (2)
150-163,14
本文受新型油气勘探开发国家科技重大专项"四川盆地全油气系统与新领域勘探技术"(编号:2025ZD1400400)、中国石油基础性前瞻性重大科技专项"叠合盆地中下组合叠加地质构造与成因机制研究"(编号:2023ZZ0202)和中国石油天然气集团有限公司科技项目"中国石油重点地区风险勘探目标研究"(编号:2023YQX10101)联合资助
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