贵州习水骑龙村奥陶系五峰组—志留系龙马溪组剖面  

Outcrop of Ordovician Wufeng Formation-Silurian Longmaxi Formation in Qilong Village,Xishui,Guizhou

作　　者：刘树根[1,2] 冉波 叶玥豪[1] 王世玉[3] 杨迪 罗超[4] 韩雨樾[1] 宋金民 张旋[4] LIU Shugen;RAN Bo;YE Yuehao;WANG Shiyu;YANG Di;LUO Chao;HAN Yuyue;SONG Jinmin;ZHANG Xuan(State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu,Sichuan 610059,China;Xihua University,Chengdu,Sichuan 610039,China;Research Institute of Yanchang Petroleum(Group)Co.,Ltd.,Xi'an,Shaanxi 710075,China;PetroChina Southwest Oil&Gasfield Company,Chengdu,Sichuan 610041,China)

机构地区：[1]油气藏地质及开发工程国家重点实验室(成都理工大学),四川成都610059 [2]西华大学,四川成都610039 [3]陕西延长石油(集团)有限责任公司研究院,陕西西安710075 [4]中国石油西南油气田分公司,四川成都610041

出　　处：《油气藏评价与开发》2022年第1期10-28,共19页Petroleum Reservoir Evaluation and Development

基　　金：国家自然科学基金企业联合基金02课题“海相深层碳酸盐岩层系油气成藏机理与开发方法”——“四川盆地震旦系—寒武系油气成藏过程与机理”(P19038);国家自然科学基金面上项目“川西地区深层雷口坡组微生物岩及其储层形成机理研究”(41872150)。

摘　　要：对贵州习水骑龙村奥陶系五峰组—志留系龙马溪组剖面实测,通过古生物对比、薄片鉴定、扫描电镜和氮气吸附等方法对五峰组—龙马溪组开展了系统性的研究,其主要认识有:①骑龙村五峰组—龙马溪组剖面出露完整,与上覆志留系石牛栏组和下伏奥陶系涧草沟组均为整合接触,发育12个笔石带,无地层缺失;②骑龙村五峰组—龙马溪组剖面黑色页岩主要发育6种页岩岩相;③骑龙村五峰组—龙马溪组剖面页岩中的石英含量从底到顶逐渐减少,而黏土矿物却逐渐增加,因此脆性矿物的含量从底到顶逐渐减少,页岩易压裂性降低;④骑龙村剖面五峰组—龙马溪组有机质类型主要为Ⅰ型和Ⅱ1型,高总有机碳含量(TOC)优质页岩主要分布在五峰组和龙马溪组下段;⑤骑龙村剖面五峰组—龙马溪组古生产力相对较低,优质黑色页岩沉积环境为缺氧—贫氧条件,其有机质含量高得益于高有机质埋藏效率;⑥骑龙村剖面五峰组—龙马溪组有机质孔主要分布在龙马溪组下段和五峰组,龙马溪组上段与观音桥段有机质孔不发育,纵向上表现为小孔径孔隙占比随地层向上递减,大孔径孔隙占比随地层向上递增;⑦骑龙村剖面五峰组—龙马溪组天然气吸附量最小为1.62 m^(3)/t,最大为2.8 m^(3)/t,平均值为2.13 m^(3)/t,表现为TOC值越大,相应的吸附能力也越强,反映出有机质含量对富有机质页岩的含气能力起决定性的作用。As a systematic study of the Wufeng-Longmaxi Formation was carried out by paleontological comparison,thin section identification,scanning electron microscopy and Nitrogen Adsorption Method in Qilong Village outcrop,Xishui,Guizhou Province,the following main insights are obtained:(1)The Wufeng-Longmaxi Formation in Qilong Village outcrop is complete,and is conformable with overlying Silurian Shiniulan Formation and the underlying Ordovician Jiancaogou Formation,with 12 graptolite biozones developed and without unconformity;(2)Based on a variety of sedimentary fabric features,six major shale lithofacies in the Wufeng-Longmaxi Formation are determined;(3)The quartz content of the Wufeng Longmaxi Formation decreases,while clay minerals increase gradually from the bottom to the top in Qilong Village outcrop,which shows the content of brittle minerals decreases,and a decrease of fracability of the shale from the bottom to the top;(4)The organic matter types of Wufeng-Longmaxi Formation in Qilong Village outcrop are mainly of typeⅠand typeⅡ1,and the high TOC shale is mainly distributed in the Wufeng and lower Longmaxi Formation;(5)There is relatively low paleoproductivity of the Wufeng-Longmaxi Formation in Qilong Village outcrop.The high quality black shale was deposited in anoxic-dysoxic conditions,and high content of organic matter benefits from the high burial efficiency of organic matter;(6)The organic pores of the Wufeng-Longmaxi Formation in Qilong Village outcrop are mainly distributed in Wufeng and lower Longmaxi Formation,while organic pores were not developed in the upper member of Longmaxi Formation or Guanyinqiao member.The abundance of the small pores vertically decreases with stratigraphy upwards and The abundance of the large pore increases with stratigraphy upwards;(7)The natural gas adsorption capacity of the WufengLongmaxi Formation in Qilong Village outcrop is a minimum of 1.62 m^(3)/t,a maximum of 2.8 m^(3)/t,and an average value of 2.13 m^(3)/t.This shows that the larger the TOC value is,the st

关 键 词：有机质丰度 孔隙结构 含气量 五峰组—龙马溪组 骑龙村 

分 类 号：TE122[石油与天然气工程—油气勘探]