天然气地球科学

• 天然气地质学 • 上一篇    下一篇

川中地区雷口坡组风化壳岩溶作用研究

宋文燕,刘利清,甘学启,秦启荣,苏培东,范存辉   

  1. 1.重庆一三六地质队,重庆 渝北 401147; 2.中国石化西北油田分公司塔河采油三厂,新疆 轮台 841000; 3.斯伦贝谢中国公司,四川 成都 610041; 4.西南石油大学科技园,四川 成都 610500; 5.西南石油大学资源与环境学院,四川 成都 610500
  • 收稿日期:2012-02-03 修回日期:2012-06-15 出版日期:2012-12-10 发布日期:2012-12-10
  • 通讯作者: 宋文燕song_wenyan@126.com. E-mail:song_wenyan@126.com.
  • 作者简介:宋文燕(1985-),女,四川遂宁人,助理工程师,硕士,主要从事岩溶、构造、矿产资源方面的研究.E-mail:song_wenyan@126.com.
  • 基金资助:

    四川省重点学科建设项目“矿产普查与勘探”(编号:SZD0414)资助.

Weathering Crust Karstification in Leikoupo Formation in Central Sichuan Area

SONG Wen-yan,LIU Li-qing,GAN Xue-qi,QIN Qi-rong,SU Pei-dong,FAN Cun-hui   

  1. 1.Chongqing Yisanliu Geoteam,Chonqing 401147,China;2.The 3rd Oil Production Company in Tahe Oil Field, SINOPIC, Luntai 841000,China;3.Schlumberger in China, Chengdu 610041,China; 4.Science and Technology Park of Southwest Petroleum University,Chengdu 610500,China; 5.Resources and Environment Institute of Southwest Petroleum University, Chengdu 610050,China
  • Received:2012-02-03 Revised:2012-06-15 Online:2012-12-10 Published:2012-12-10

摘要:

通过考察川中地区8条优选的野外地质剖面,搞清雷口坡组顶面岩性特征、溶蚀孔缝发育情况、风化壳发育层位及发育厚度等。地层分析表明:川中雷口坡组地面露头岩性包括白云岩、溶塌角砾岩以及石灰岩;溶蚀孔洞发育,以半充填或未充填为主;在65m左右的岩溶作用深度范围内,岩溶作用改善了地层的岩性、孔隙空间、储渗性能,可形成良好的古风化壳储层。该认识对研究深埋于地下的雷口坡组顶部风化壳储层具有重要的借鉴意义,可为川中地区雷口坡组风化壳储层进一步的勘探开发提供地质依据。

关键词: 风化壳, 岩溶作用, 储层, 雷口坡组, 川中地区

Abstract:

Through the investigation of 8 preferred geological sections, the lithology, corrosion holes and fractures growth conditions, growth layer and thickness of the weathering crust in the top of Leikoup Formation have been determined.The stratum analysis suggests that the lithology of the Leikoupo outcrop are mainly dolomite, dissolution collapse breccia and limestone.The corrosion holes are developed, and dominated by half-filling or no filling.In the range of the karstification depth, about 65m, karstification improved lithology, pore space, storage and permeability.It forms a good reservoir of ancient weathering crust.The research provides an important reference for the study of deep underground weathering crust reservoir and can provide a basis for the geological exploration and development of Sichuan Leikoupo weathering crust reservoir.

Key words: Weathering crust, Karstification, Reservoir, Leikoupo Formation, Central Sichuan area

中图分类号: 

  • TE122.2

[1]Rahardjo H,Aung K K,Leong E C,et al.Characteristics of residual soils in singapore as formed by weathering[J].Engineering Geology,2004,73(1/2):157-169.



[2]Zhao Yonggang.Study on Palaeo-Rock-Solution of Carbonate Rock of Ordovician and Its Reservoir[D].Chengdu:Southwest Petroleum University,2006.[赵永刚.奥陶系碳酸盐岩古岩溶及其储层研究[D].成都:西南石油大学,2006.]



[3]Duan Jie.Research for the Lower Palaeozoic Carbonatite Reservoir Characteristics in the South of Ordos Basin[D].Chengdu:Chengdu University of  Technology,2009.[段杰.鄂尔多斯盆地南缘下古生界碳酸盐岩储层特征研究[D].成都:成都理工大学,2009.]



[4]Wang Hua,Liu Shugen,Wang Guizhi,et al.Palaeokarst reservoir research of the middle Triassic Leikoupo in the south area of central Sichuan basin[J].Computing Techniques for Geophysical and Geochemical Exploration,2009,31(3):264-270.[汪华,刘树根,王国芝,等.川中南部地区中三叠统雷口坡组顶部古岩溶储层研究[J].物探化探计算技术,2009,31(3):264-270.]



[5]Liu Shanhua.The Research on Ordovician Sedimentology and Reservoir Property of Leshan-Longnvsi Paleo-uplift in Centre Sichuan Area[D].Chengdu:Southwest Petroleum University,2006.[刘善华.川中地区乐山—龙女寺古隆起奥陶系沉积、储层特征研究[D].成都:西南石油大学,2006.]



[6]Wu Yong,Tan Jianxiong,Yu Jing.Ancient karst development characteristics of L11 reservoir of Moxi gas field in central Sichuan[J].Natural Gas Geoscience,1996,7(2):15-21.[吴勇,覃建雄,于静.川中磨溪气田雷一1储层古岩溶发育特征[J].天然气地球科学,1996,7(2):15-21.]



[7]Sun Chonghao,Yu Hongfeng,Wang Huaisheng,et al.Vugular formation of carbonates in Ordovician Yingshan reservoir in Tazhong northern slope of Tarim basin[J].Natural Gas Geoscience,2012,23(2):230-236.[孙崇浩,于红枫,王怀盛,等.塔里木盆地塔中地区奥陶系鹰山组碳酸盐岩孔洞发育规律研究[J].天然气地球科学,2012,23(2):230-236.]



[8]Jia Zhenyuan,Cai Zhongxian.Carbonate paleo-weathered crust reservoirs(body)[J].Geological Science and Technology Information,2004,23(4):94-104.[贾振远,蔡忠贤.碳酸盐岩古风化壳储集层(体)研究[J].地质科技情报,2004,23(4):94-104.]



[9]Chen Xueshi.The paleokarst reservoirs of oil/gas fields in China[J].Acta Sedimentologica Sinica,2004,22(2):244-254.[陈学时.中国油气田古岩溶与油气储层[J].沉积学报,2004,22(2):244-254.]



[10]Su Jing,Zhang Yongchang,Yang Haijun,et al.Control of fault system to formation of effective carbonate reservoir and the rules of petroleum accumulation[J].Acta Petrolei Sinica,2010,31(2):196-202.[苏劲,张永昌,杨海军,等.断裂系统对碳酸盐岩有效储层的控制及其成藏规律[J].石油学报,2010,31(2):196-202.]



[11]Pang Yanjun,Dai Zongyang,Liu Shanhua,et al.The geological condition analysis of Ordovician paleo-kastification of Leshan-Longnvsi paleohigh in central Sichuan[J].Journal of Chongqing University of Science and Technology:Natural Sciences Edition,2007,9(3):1-4.[庞艳君,代宗仰,刘善华,等.川中乐山—龙女寺古隆起奥陶系古岩溶发育地质因素分析[J].重庆科技学院学报:自然科学版,2007,9(3):1-4.]



[12]Wang Huanhuan,Zhu Guangyou,Xue Haitao,et al.Formation and controlling factors of effective weathered crust carbonate reservoirs:Taking the Yingmaili-Yaha area of Tarim basin as an example[J].Natural Gas Geoscience,2009,20(2):182-190.[王欢欢,朱光有,薛海涛,等.碳酸盐岩风化壳型有效储层的形成与控制因素研究——以塔里木盆地英买力牙哈地区为例[J].天然气地球科学,2009,20(2):182-190.]



[13]Xia Riyuan,Tang Jiansheng,Guan Bizhu,et al.Paleokarst landforms and law of natural gas accumulation in Ordovician of Ordos basin[J].Oil and Gas Geology,1999,20(2):133-136.[夏日元,唐建生,关壁珠,等.鄂尔多斯盆地奥陶系古岩溶地貌及天然气富集规律[J].石油与天然气地质,1999,20(2):133-136.]



[14]Liu Jinhua.Study on the Formation,Distribution and Effectiveness of Reservoir Fractures with Oil and Gas[D].Beijing:China University of Petroleum,2009.[刘金华.油气储层裂缝形成、分布及有效性研究[D].北京:中国石油大学,2009.]

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