川北山前带寒武系筇竹寺组富有机质页岩发育模式  

Developmental models of organic-rich shales in the Cambrian Qiongzhusi Formation in the piedmont zone of northern Sichuan Basin

作　　者：张明何 魏祥峰[2] 高波[3] 戎佳 刘珠江[2] 燕继红[2] 杨琪航 王佳乐 刘慧萍 游浪 刘自亮[1] ZHANG Minghe;WEI Xiangfeng;GAO Bo;RONG Jia;LIU Zhujiang;YAN Jihong;YANG Qihang;WANG Jiale;LIU Huiping;YOU Lang;LIU Ziliang(College of Energy,Chengdu University of Technology,Chengdu,Sichuan 610059,China;Exploration Company,SINOPEC,Chengdu,Sichuan 610041,China;Petroleum Exploration and Production Research Institute,SINOPEC,Beijing 102206,China)

机构地区：[1]成都理工大学能源学院,四川成都610059 [2]中国石化勘探分公司,四川成都610041 [3]中国石化石油勘探开发研究院,北京102206

出　　处：《石油与天然气地质》2024年第4期992-1006,共15页Oil & Gas Geology

基　　金：国家自然科学基金面上项目(42272183);中国石化科技开发部项目(P19017-4)。

摘　　要：研究川北山前寒武系筇竹寺组富有机质页岩分布、主控因素及沉积模式,对该地区页岩气勘探具有重要意义。利用野外地质调查、钻井和岩心资料,结合岩石薄片鉴定、全岩X射线衍射分析、总有机碳含量(TOC)测定等分析测试资料,研究川北山前带筇竹寺组富有机质页岩的沉积模式、分布及主控因素。研究表明:①筇竹寺组页岩主要为强脆性硅质页岩和中等脆性硅/黏土混合质页岩,根据总有机碳含量(TOC)—沉积构造—矿物组分将其划分为16种岩相类型川北山前带寒武系筇竹寺组页岩主要为富有机质纹层状强脆性硅质页岩相、富有机质层状强脆性硅质页岩相和含有机质层状强脆性硅质页岩相。其中前两类岩相为页岩气主要勘探开发岩相;②富有机质页岩TOC普遍高于2%,富有机质页岩具南厚北薄、西厚东薄分布的特征,有机质丰度具南高北低、西高东低的特点;③拉张槽及区域内隆-凹相间的古地理格局是筇竹寺组富有机质页岩差异分布的主要原因,区内不均衡构造演化加剧了页岩的非均质性展布;繁盛发育的低等浮游生物及细菌等提供了丰富的有机质来源,早期快速海侵下缺氧的深水环境利于有机质的保存,晚期摩天岭古陆和汉南古陆的持续隆升对有机质富集起抑制作用;④海平面升降和古气候演变控制了富有机质页岩在纵向上呈旋回性分布。Investigating the distributions,dominant controlling factors,and sedimentary patterns of organic-rich shales in the Cambrian Qiongzhusi Formation in the Micang-Daba piedmont zone of the northern Sichuan Basin holds great significance for shale gas exploration within.Based on data from field geological surveys,drilling,and core observation,as well as analytical and test data derived from rock thin section observations,whole-rock X-ray diffraction(XRD)pattern,and total organic carbon(TOC)content determination,we explore the sedimentary patterns,distributions,and dominant controlling factors of organic-rich shales in the Qiongzhusi Formation,piedmont zone of the northern Sichuan Basin.The results indicate that shales in the Qiongzhusi Formation consist primarily of highly brittle siliceous shales and moderately brittle silica-clay mixed shales.In terms of their TOC content,sedimentary structures,and mineral components,these shales can be categorized into 16 lithofacies types,with the organic-rich laminated siliceous shale facies of high brittleness,organic-rich bedded siliceous shale facies of high brittleness,and the organic matter-bearing bedded siliceous shale facies of high brittleness dominating.The former two dominant shale facies are identified as the primary targets for the exploration and production of shale gas.The organic-rich shales,with TOC content typically exceeding 2%,are thicker in the south and west but thinner in the north and east,corresponding to a higher organic matter abundance in the south and west and lower abundance in the north and east;The intracratonic sag and the paleogeographic patterns exhibiting alternating uplifts and sags within are identified as the primary causes of the differential distribution of organic-rich shales in the Qiongzhusi Formation.The imbalanced structural evolution in the zone enhances the heterogeneous distribution of shales.The flourishing lower plankton and bacteria serve as substantial sources of organic matter.The anoxic deep-water environment under rapid tra

关 键 词：发育模式 控制因素 富有机质页岩 筇竹寺组 寒武系 川北山前带 

分 类 号：TE122.1[石油与天然气工程—油气勘探]