天然气地球科学

• 天然气地质学 • 上一篇    下一篇

四川盆地高石梯构造灯影组四段溶蚀孔洞型储层类型及组合模式

张林1,万玉金1,杨洪志2,苏云河1,张满郎1   

  1. 1.中国石油勘探开发研究院,河北 廊坊 065007;
    2.中国石油西南油气田分公司勘探开发研究院,四川 成都 610000
  • 收稿日期:2016-06-07 修回日期:2016-09-10 出版日期:2017-08-10 发布日期:2017-08-10
  • 作者简介:张林(1969-),男,重庆忠县人,高级工程师,博士,主要从事天然气勘探和开发地质研究. E-mail:ZL69@petrochina.com.cn.
  • 基金资助:

    中国石油股份公司深层油气重大专项“深层油气藏开发关键技术”(编号:2014E-3203)资助.

The type and combination pattern of karst vuggy reservoir in the fourth member of the Dengying Formation of Gaoshiti structure in Sichuan Basin

Zhang Lin1,Wan Yu-jin1,Yang Hong-zhi2,Su Yun-he1,Zhang Man-lang1   

  1. 1.PetroChina Research Institute of Petroleum Exploration and Development,Langfang 065007,China;
    2.Research Institute of Petroleum Exploration and Development,PetroChina SouthwestOil & Gasfield Company,Chengdu 610000,China
  • Received:2016-06-07 Revised:2016-09-10 Online:2017-08-10 Published:2017-08-10

摘要:

震旦纪高石梯构造位于四川盆地绵竹—长宁克拉通内裂陷东侧的台地边缘带,发育藻灰泥丘、砂屑滩及云坪,同时受震旦纪末期桐湾Ⅱ幕构造运动的抬升暴露剥蚀并形成岩溶风化壳。灯四段为溶蚀孔洞型白云岩储层,主要储集空间有溶洞、溶孔及晶间孔。在岩心,成像测井和常规测井对溶蚀孔洞型储层的定量判识基础上,划分洞穴型、孔洞型、孔隙型、裂缝—孔洞型、裂缝—孔隙型和裂缝型6类储集空间。在纵向上,根据储集空间类型及其组合特征提出洞穴—孔洞型、裂缝—孔洞型、孔洞型、裂缝—孔隙型、裂缝型5类储层组合模式。其中洞穴—孔洞型、裂缝—孔洞型为高产长期稳产型,是最好的储层组合类型;孔洞型为中产长期稳产型;裂缝—孔隙型和裂缝型则为高产短期稳产型。

关键词: 岩溶储层, 组合模式, 灯影组四段, 高石梯, 四川盆地

Abstract:

In the Sinian Dengsi period,the Gaoshiti-Moxi structure located in east side of Mianzhu-Changning intracratonic rift.There is a platform edge with microfacies of algal plaster mound,psammitic beach and dolomitic flat.With the exposure and erosion of Tongwan Ⅱ episode of tectonic uplift in the Late Sinian,it became Karst weathering crust formation.The Dengsi member was corrosion vuggy dolomite reservoir with main reservoir space of vug,pore and fracture.On the basis of the quantitative analysis with core description,imaging-log and conventional log,the reservoir space can be divided into six types,such as cavernous,vuggy,pore,fracture-vuggy,fracture-pore,and fracture.In the vertical,according to the type of reservoir space and its combination characteristics,there are five combination patterns,such as cave-vuggy,fracture-vuggy,vuggy,fracture-pore and fracture.The cave-vuggy type and fracture-vuggy type are the best reservoir combination pattern which has long-term high production and steady produce of gas. The vuggy type is long-term middle production and steady produce of gas,while fracture-pore type and fracture type are high gas production and short stable period.

Key words: Vuggy reservoir, Combination pattern, The fourth member of the Dengying Formation, Gaoshiti, Sichuan Basin

中图分类号: 

  • TE122.1

[1]Song Wenhai.Some new knowledge of Caledonian paleo-uplift in Sichuan Basin[J].Natural Gas Industry,1987,7(3):6-11.[宋文海.对四川盆地加里东期古隆起的新认识[J].天然气工业,1987,7(3):6-11.]
[2]Luo Bing,Luo Wenjun,Wang Wenzhi,et al.Formation mechanism of the Sinian natural gas reservoir in the Leshan-Longnvsi Paleo-Uplift,Sichuan Basin[J].Natural Gas Geoscience,2015,26(3):444-455.[罗冰,罗文军,王文之,等.四川盆地乐山—龙女寺古隆起震旦系气藏形成机制[J].天然气地球科学,2015,26(3):444-455.]
[3]Li Xiao qing,Wang Zecheng,Zhang Xingwei,et al.Characteristics of paleo-uplifts in Sichuan Basin and their control action on natural gases[J].Oil & Gas Geology,2001,22(4):347-350.[李晓清,汪泽成,张兴为,等.四川盆地古隆起特征及对天然气的控制作用[J].石油与天然气地质,2001,22(4):347-350.]
[4]Liu Shun,Luo Zhili,Xiong Rongguo,et al.On formation mechanism of Caledonian Paleo-Uplift in Sichuan Basin from experimental rocks deformational process[J].Journal of Chengdu University of Technology,2000,27(4):343-347.[刘顺,罗志立,熊荣国,等.从实验岩石变形过程探讨四川盆地加里东古隆起的形成机制[J].成都理工学院学报,2000,27(4):343-347.]
[5]Luo Zhili,Liu Shun,Xu Shiqi,et al.Selection of favorable area of exploration in Sinian  bearing gas formation of Sichuan Basin[J].Acta Petrolei Sinica,1998,19(4):1-7.[罗志立,刘顺,徐世琦,等.四川盆地震旦系含气层中有利勘探区块的选择[J].石油学报,1998,19(4):1-7.]
[6]Wei Guoqi,Shen Ping,Yang Wei,et al.Formation conditions and exploration prospects of Sinian large gasfields,Sichuan Basin[J].Petroleum Exploration and Development,2013,40(2):129-138.[魏国齐,沈平,杨威,等.四川盆地震旦系大气田形成条件与勘探远景区[J].石油勘探与开发,2013,40(2):129-138.]
[7]Song Wenhai.Research on reservoir-formed condition of large-medium gas fields of Leshan-Longnvsi palaeohigh[J].Natural Gas Industry,1996,16(supplement1):13-26.[宋文海.乐山—龙女寺古隆起大中型气田成藏条件研究[J].天然气工业,1996,16(增刊):13-26.]
[8]Zhang Jianyong,Luo Wenjun,Zhou Jingao,et al.Main origins of high quality reservoir of Lower Cambrian Longwangmiao Formation in the giant Anyue Gasfield,Sichuan Basin,SW China[J].Natural Gas Geoscience,2015,26(11):2063-2074.[张建勇,罗文军,周进高,等.四川盆地安岳特大型气田下寒武统龙王庙组优质储层形成的主控因素[J].天然气地球科学,2015,26(11):2063-2074.]
[9]Zou Caineng,Du Jinhu,Xu Chunchun,et al.Formation,distribution,resource potential and discovery of the Sinian-Cambrian giant gasfield,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):278-293.[邹才能,杜金虎,徐春春,等.四川盆地震旦系—寒武系特大型气田形成分布、资源潜力及勘探发现[J].石油勘探与开发,2014,41(3):278-293.]
[10]Wei Guoqi,Yank Wei,Du Jinhu,et al.Geological characteristics of the Sinian-Early Cambrian intracratonic rift Sichuan Basin[J].Natural Gas Industry,2015,35(1):24-35.[魏国齐,杨威,杜金虎等.四川盆地震旦纪—早寒武世克拉通内裂陷地质特征[J].天然气工业,2015,35(1):24-35.]
[11]Luo Bing,Yang  Yueming,Luo Wenjun,et al.Controlling factors and distribution of reservoir development in Dengying Formation of palco-uplift in central Sichuan Basin[J].Acta Petrolei Sinica,2015,36(4):416-426.[罗冰,杨跃明,罗文军等.川中古隆起灯影组储层发育控制因素及展布[J].石油学报,2015,36(4):416-426.]
[12]Zhou Zheng,Wang Xingzhi,Xie Lin,et al.Reservoir features and physical influences of the Sinian Dengying Lormation(Sinian) in central Sichuan,China[J].Natural Gas Geoscience,2014,25(5):701-709.[周正,王兴志,谢林,等.川中地区震旦系灯影组储层特征及物性影响因素[J].天然气地球科学,2014,25(5):701- 709.]
[13]Wei Guoqi,Yang Wei,Du Jinhu,et al.Tectonic features of Gaoshiti-Moxi Paleo-Uplift and its controls on the formation of a giant gasfield,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2015,42(3):257-265.[魏国齐,杨威,杜金虎,等.四川盆地高石梯—磨溪古隆起构造特征及对特大型气田形成的控制作用[J].石油勘探与开发,2015,42(3):257-265.]

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[1] 张延敏, . 1996~1999年世界天然气产量[J]. 天然气地球科学, 2000, 11(3): 44 -45 .
[2] 付广;付晓飞;薛永超;杨勉;. 引起油气藏破坏与再分配的地质因素分析[J]. 天然气地球科学, 2000, 11(6): 1 -6 .
[3] 安菊华;陈振岩;常津焕;宋玉军;. 大民屯凹陷泥丘形成机制及其与油气的关系[J]. 天然气地球科学, 2000, 11(6): 20 -28 .
[4] 王连进;叶加仁;. 残余盆地特征及研究方法[J]. 天然气地球科学, 2000, 11(3): 8 -12 .
[5] 张树林;. 莺琼盆地岩石弹性物性规律之研究[J]. 天然气地球科学, 2000, 11(3): 35 -43 .
[6] 金奎励;李荣西;. 烃源岩组分组合规律及其意义[J]. 天然气地球科学, 1998, 9(1): 23 -29 .
[7] P.R.Miles;刘文汇;. 欧洲大陆边缘甲烷水合物的远景分布[J]. 天然气地球科学, 1998, 9(3-4): 57 -60 .
[8] M.P.Koopmans;C.Schaeffer-Reiss;J.W.de Leeuw(荷兰)等;郑军卫(译). 热成熟早期阶段未熟干酪根n-C37和n-C38不饱和酮的S、O键合及其碳骨架的释放[J]. 天然气地球科学, 1999, 10(1-2): 76 -81 .
[9] 妥进才, 王先彬, 周世新, 陈晓东, . 深层油气勘探现状与研究进展[J]. 天然气地球科学, 1999, 10(6): 1 -8 .
[10] 何承恩, 李树枝. 星疤研究与冲击构造油气藏[J]. 天然气地球科学, 1990, 1(1): 9 -13 .