地质勘探

川中地区侏罗系大安寨段沉积相及有利岩石组合分析

  • 黄董 ,
  • 曾德铭 ,
  • 王兴志 ,
  • 谢圣阳 ,
  • 张芮 ,
  • 张少敏 ,
  • 郭奕浩
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  • 1.西南石油大学,四川 成都 610500;
    2.中国石油西南油气田分公司,四川 成都 610041
黄董(1997—),男,2020年毕业于西南石油大学资源勘查专业,现为该校地质学专业在读硕士研究生,研究方向为沉积学与储层地质学。

收稿日期: 2022-01-29

  修回日期: 2022-09-02

  网络出版日期: 2023-03-24

基金资助

中国石油-西南石油大学创新联合体项目“四川盆地侏罗系湖相页岩油地质理论技术研究与有利区评价”(2020CX050000)

Sedimentary Facies and Favorable Rock Assemblages of Jurassic Da′anzhai Member, Central Sichuan

  • Huang Dong ,
  • Zeng Deming ,
  • Wang Xingzhi ,
  • Xie Shengyang ,
  • Zhang Rui ,
  • Zhang Shaomin ,
  • Guo Yihao
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  • 1. Southwest Petroleum University, Chengdu, Sichuan 610500, China;
    2. PetroChina Southwest Oil & Gasfield Company, Chengdu, Sichuan 610041, China

Received date: 2022-01-29

  Revised date: 2022-09-02

  Online published: 2023-03-24

摘要

针对川中地区侏罗系大安寨段沉积相划分不精细,有利岩石组合及有利勘探区不明确的问题,利用3口全取心井的岩心描述和6条野外剖面观察结果,结合薄片鉴定、测井解释及有机地球化学分析方法,对研究区岩石类型、沉积相类型、沉积相分布及沉积模式、岩石组合及有利勘探区进行研究。研究结果表明:岩石类型划分为10种;沉积相划分为滨湖、浅湖、半深湖3个亚相,以及半深湖泥、生物滩、重力流等10种微相;公山庙—莲池—营山一线为沉积中心,为半深湖环境,识别出C、D、E共3种岩石组合类型;南充—渠县—仪陇一线为呈环状发育的浅湖环境,识别出A、B、F共3种岩石组合类型。研究成果可由常规致密油拓展至页岩油勘探领域,通过TOC、孔隙度、渗透率、压裂效果等评价指标,认为A型岩石组合在断裂和裂缝匹配下,是致密油碳酸盐岩的有利勘探组合,F型为最有利页岩油勘探组合,主要分布于浅湖相大一亚段—大二a亚段。研究成果对页岩油下一步勘探有重要指示意义。

本文引用格式

黄董 , 曾德铭 , 王兴志 , 谢圣阳 , 张芮 , 张少敏 , 郭奕浩 . 川中地区侏罗系大安寨段沉积相及有利岩石组合分析[J]. 特种油气藏, 2023 , 30(1) : 65 -73 . DOI: 10.3969/j.issn.1006-6535.2023.01.009

Abstract

In view of the imprecise sedimentary facies division, unclear favorable rock assemblage and undefined favorable exploration area of Jurassic Da′anzhai Member in Central Sichuan, a study was conducted on the rock type, sedimentary facies type, sedimentary facies distribution, sedimentary model, rock assemblage and favorable exploration area in the study area by the core description of three fully cored wells and the observation results of six field profiles in combination with thin slice identification, logging interpretation and organic geochemical analysis methods. The study results show that Rock was divided into 10 types. The sedimentary facies was divided into 3 subfacies (shore lake, shallow lake and fairly deep lake) and 10 microfacies (including fairly deep lake mud, organic bank and gravity flow). Gongshanmio-Lianchi-Yingshan line is the sedimentary center developed in a fairly deep lake environment, and three rock assemblage types (C, D and E) were identified. Nanchong-Quxian-Yilong line was circularly developed in a shallow lake environment, and three rock assemblage types (A, B and F) were identified. The study results were applied from conventional tight oil to shale oil exploration. According to the TOC, porosity, permeability, fracturing effect and other evaluation indicators, it was considered that Type A rock assemblage was a favorable combination for tight oil carbonate rock exploration under the matching of fractures and cracks, and Type F was the most favorable combination for shale oil exploration, which was mainly distributed in the shallow lake facies at Sub-member 1 to Sub-member 2a of Da′anzhai Member. The study results are of great significance for shale oil exploration in the future.

参考文献

[1] 卢炳雄,郑荣才,梁西文,等.四川盆地东部地区大安寨段页岩气(油)储层特征[J].中国地质,2014,41(4):1387-1398.
LU Bingxiong,ZHENG Rongcai,LIANG Xiwen,et al.Characteristics analysis of Da′anzhai shale gas(oil)reservoirs in eastern Sichuan Basin[J].Geology in China,2014,41(4):1387-1398.
[2] 卢炳雄,郑荣才,梁西文,等.川东地区侏罗系自流井组大安寨段页岩气(油)储层评价[J].石油与天然气地质,2015,36(3):488-496.
LU Bingxiong,ZHENG Rongcai,LIANG Xiwen,et al.Evaluation of reservoirs in the Da′anzhai Member of the Jurassic Ziliujing Formation in eastern Sichuan Basin[J].Oil & Gas Geology,2015,36(3):488-496.
[3] 陈超,杨雪飞,王兴志,等.湖相碳酸盐岩沉积相分析:以四川盆地东北部下侏罗统自流井组大安寨段为例[J].地质论评,2019,65(增刊1):117-119.
CHEN Chao,YANG Xuefei,WANG Xingzhi,et al.Analysis of lacustrine of carbonate rocks sedimentary facies:a case study of the Da′anzhai Member of the Jurassic Ziliujing Formation in eastern Sichuan Basin[J].Geological Review,2019,65(S1):117-119.
[4] 刘达望,张文济,任康绪,等.川东地区大安寨段岩石类型及其组合特征的勘探意义[J].科学技术与工程,2018,18(6):73-80.
LIU Dawang,ZHANG Wenji,REN Kangxu,et al.Rock types and their association characteristics and significance for exploration in the Da′anzhai[J].Science Technology and Engineering,2018,18(6):73-80.
[5] 雷文智,陈冬霞,张芮,等.川中地区下侏罗统自流井组大二亚段陆相页岩层系岩性组合类型及其特征[J].地球科学,2021,46(10):3657-3672.
LEI Wenzhi,CHEN Dongxia,ZHANG Rui,et al.Lithological combination types and characteristics of continental shale strata in the second sub-member of Da′anzhai in central Sichuan[J].Journal of Earth Science,2021,46(10):3657-3672.
[6] 杨跃明,黄东,杨光,等.四川盆地侏罗系湖相页岩油气地质特征及勘探开发新认识[J].天然气工业,2019,39(6):22-33.
YANG Yueming,HUANG Dong,YANG Guang,et al.Geological characteristics and new understandings of exploration and development of Jurassic lacustrine shale oil and gas in the Sichuan Basin[J].Natural Gas Industry,2019,39(6):22-33.
[7] 厚刚福,宋兵,倪超,等.致密油源储配置特征及油气勘探意义——以四川盆地川中地区侏罗系大安寨段为例[J].沉积学报,2021,39(5):1078-1085.
HOU Gangfu,SONG Bing,NI Chao,et al.Tight oil source-reservoir matching characteristics and its significance for oil and gas exploration:a case study of the Jurassic Da′anzhai Member in the central Sichuan Basin[J].Acta Sedimentologica Sinica,2021,39(5):1078-1085.
[8] 张宇,杜垚,刘耘,等.四川盆地侏罗系大安寨段湖相页岩油气基本特征及勘探方向[J].中国地质,2022,49(1):51-65.
ZHANG Yu,DU Yao,LIU Yun,et al.Basic characteristics and exploration direction of lacustrine shale oil and gas in Da′anzhai Member of Jurassic in Sichuan Basin[J].Geology in China,2022,49(1):51-65.
[9] 冯增昭.沉积相的一些术语定义的评论[J].古地理学报,2020,22(2):207-220.
FENG Zengzhao.A review on the definitions of terms of sedimentary facies[J].Journal of Palaeogeography,2020,22(2):207-220.
[10] 施开兰,陈芳文,段卓,等.重庆北碚和平水库剖面下侏罗统大安寨段湖相碳酸盐岩岩石类型及沉积环境[J].古地理学报,2015,17(2):198-212.
SHI Kailan,CHEN Fangwen,DUAN Zhuo,et al.Lacustrine carbonate rock types and sedimentary environments of the Lower Jurassic Da′anzhai Member of Heping Reservoir section in Beibei Area,Chongqing[J].Journal of Palaeogeography,2015,17(2):198-212.
[11] 郑荣才,郭春利,梁西文,等.四川盆地大安寨段非常规储层的储集空间类型与评价[J].岩性油气藏,2016,28(1):16-29.
ZHENG Rongcai,GUO Chunli,LIANG Xiwen,et al.Characteristics and evaluation of reservoir spaces of shale gas(oil)in Da′anzhai member of Ziliujing Formation in Sichuan Basin[J].Lithologic Reservoirs,2016,28(1):16-29.
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