岩性油气藏 ›› 2024, Vol. 36 ›› Issue (4): 159–168.doi: 10.12108/yxyqc.20240414

• 地质勘探 • 上一篇    下一篇

川中古隆起北斜坡寒武系龙王庙组油气成藏特征及演化模式

卢科良1,2, 吴康军1,2, 李志军1,2, 孙永河2, 徐少华1,2, 梁锋3, 刘露2, 李爽1,2   

  1. 1. 重庆科技大学 石油与天然气工程学院, 重庆 401331;
    2. 复杂油气田勘探开发重庆市重点实验室, 重庆 401331;
    3. 中国石油西南油气田分公司 川中油气矿, 四川 遂宁 629000
  • 收稿日期:2023-05-10 修回日期:2023-05-23 出版日期:2024-07-01 发布日期:2024-07-04
  • 第一作者:卢科良(1998—),男,重庆科技大学在读硕士研究生,研究方向为油气地质。地址:(401331)重庆市沙坪坝区大学城东路20号重庆科技大学。Email:lkl511623@163.com。
  • 通信作者: 吴康军(1983—),男,博士,讲师,主要从事油气地质、非常规油气勘探方面的教学和研究工作。Email:wukangjun520@163.com。
  • 基金资助:
    重庆市自然科学基金创新发展联合基金(重点项目)“复式断陷盆地断裂分段生长机制及对油气成藏与开发的控制作用研究”(编号:CSTB2022NSCQ-LZX0020)、重庆市教委科学技术研究项目“川中古隆起北斜坡龙王庙组沥青成因及其油气勘探意义”(编号:KJQN202201549)与重庆科技大学研究生科技创新训练计划项目“川中古隆起北斜坡龙王庙组断裂演化及其控藏机理”(编号:YKJCX2220104)联合资助。

Characteristics and evolution model of hydrocarbon accumulation of Cambrian Longwangmiao Formation in the north slope of central Sichuan paleo-uplift

LU Keliang1,2, WU Kangjun1,2, LI Zhijun1,2, SUN Yonghe2, XU Shaohua1,2, LIANG Feng3, LIU Lu2, LI Shuang1,2   

  1. 1. School of Petroleum Engineering, Chongqing University of Science and Technology, Chongqing 401331, China;
    2. Chongqing Key Laboratory of Complex Oil & Gas Field Exploration and Development, Chongqing 401331, China;
    3. Central Sichuan Oil and Gas District, PetroChina Southwest Oil & Gas Field Company, Suining 629000, Sichuan, China
  • Received:2023-05-10 Revised:2023-05-23 Online:2024-07-01 Published:2024-07-04

摘要: 利用测井、录井、岩心分析化验等资料,对川中古隆起北斜坡下寒武统龙王庙组油气成藏条件、油气充注特征及成藏演化模式展开了深入研究。研究结果表明:①川中古隆起北斜坡下寒武统龙王庙组天然气具备良好的成藏条件,下伏筇竹寺组烃源岩在北斜坡腹部及西侧裂陷槽存在 2 个生烃中心,其TOC 平均值分别为 1.90% 和 3.46%,有机质以Ⅰ型干酪根为主,可提供充足且优质的烃源;龙王庙组内部发育的颗粒滩体岩溶储层与上覆高台组厚层致密泥质云岩,构成了优势储-盖组合;区内广泛发育的油源断裂可作为纵向优势运移通道高效输导油气。②研究区龙王庙组具 3 期成藏特征:晚三叠世末期(约 214~206 Ma)发生第 1 期充注,大量成熟油聚集形成古油藏;早侏罗世末期(约 193~186 Ma)发生第 2 期充注,表现为“多油少气”混合充注;中侏罗世末期(约 170~164 Ma)发生第 3 期充注,大量油裂解气充注储层并聚集形成现今气藏。③研究区龙王庙组油气成藏演化可划分为 4 个阶段:加里东早期—二叠纪前少量低熟油充注阶段、二叠纪—三叠纪大量成熟油充注形成古油藏阶段、中侏罗世—白垩纪古油藏被破坏形成裂解气藏阶段以及晚白垩世至今气藏调整阶段。

关键词: 颗粒滩体岩溶储层, 泥质云岩盖层, 储-盖组合, 油源断裂, 古油藏, 混合充注, 裂解气, 龙王庙组, 寒武系, 北斜坡, 川中古隆起

Abstract: Based on logging,well log,core analysis and laboratory data,a study was conducted on the hydro‐carbon accumulation conditions,hydrocarbon filling characteristics,and accumulation evolution model of Lower Cambrian Longwangmiao Formation in the north slope of central Sichuan paleo-uplift. The results show that:(1)The natural gas of Lower Cambrian Longwangmiao Formation in the north slope of central Sichuan paleo-uplift has good hydrocarbon accumulation conditions. The source rocks of underlying Qiongzhusi Formation have two hydrocarbon generation centers in the central and western rift troughs of the north slope,with an average TOC of 1.90% and 3.46%,respectively. The organic matter is mainly type Ⅰ kerogen,which can provide sufficient and high-quality hydrocarbon sources. The grain-shoal karst reservoirs developed within Longwangmiao Formation and the dense argillaceous dolomites of the overlying the Gaotai Formation form a dominant reservoir-cap assemblage. The widely developed oil-source faults in the study area can serve as vertically dominant migration channels for efficient hydrocarbon migration.(2)The Longwangmiao Formation in the study area has three stages of hydrocarbon accumulation characteristics:The first stage of filling occurred at the end of Late Triassic(approximately 214-206 Ma),with a large amount of mature oil accumulating to form paleo-oil reservoirs. In the late Early Jurassic(approximately 193-186 Ma),the second stage of filling occurred,characterized by a mixed filling of more oil and less gas. At the end of the Middle Jurassic(approximately 170-164 Ma),the third stage of filling occurred,with a large amount of oil cracked gases filling the reservoir and accumulating to form the current gas reservoir.(3)The hydrocarbon accumulation evolution of Longwangmiao Formation in the study area can be divided into four stages:the early Caledonian to pre Permian stage with a small amount of low mature oil filling,the Permian to Triassic stage with a large amount of mature oil filling to form ancient oil reservoirs,the Middle Jurassic to Cretaceous stage with the destruction of paleo-oil reservoirs to form cracked gas reservoirs,and the Late Cretaceous to present stage with gas reservoir adjustment.

Key words: grain-shoal karst reservoir, argillaceous dolomite cap rock, reservoir-cap assemblage, oil-source fault, paleo-oil reservoirs, mixed filling, cracked gas, Longwangmiao Formation, Cambrian, north slope, central Sichuan paleo‐uplift

中图分类号: 

  • TE122.1
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