黔南碳酸盐岩地区断层周缘构造变形及封闭性

doi:10.7623/syxb201005013

石油学报 ›› 2010, Vol. 31 ›› Issue (5): 781-786.DOI: 10.7623/syxb201005013

黔南碳酸盐岩地区断层周缘构造变形及封闭性

崔敏 1,2 汤良杰 1

1中国石油大学油气资源与探测国家重点实验室北京 102249； 2中海油研究总院北京 100027

收稿日期:2010-01-03 修回日期:2010-03-29 出版日期:2010-09-25 发布日期:2010-11-30
通讯作者: 崔敏
作者简介:崔敏，男，1981年4月生，2007年获吉林大学构造地质学硕士学位，现为中国石油大学（北京）构造地质学在读博士研究生，主要从事石油构造和油气保存方面的研究。
基金资助:
国家自然科学基金项目（No.40972090和No.40672143）、国家重点基础研究发展规划（973）项目(2005CB422107)、国家科技重大专项（2008ZX05005）和高等学校博士学科点专项科研基金项目(200804250001)联合资助。

Structural deformation and sealing ability around fault in carbonate rock area of South Guizhou

CUI Min 1,2 TANG Liangjie 1

Received:2010-01-03 Revised:2010-03-29 Online:2010-09-25 Published:2010-11-30

摘要/Abstract

摘要：

构造变形和油气保存是碳酸盐岩层系油气勘探的主要制约因素和研究内容。通过野外露头、薄片观察、地震剖面的解释以及实验数据的分析，对黔南地区的逆冲断层及其周缘的构造变形和断层封闭性进行了研究。碳酸盐岩地区逆冲背景下，断层周缘的构造变形具有明显的分带性(破碎带和断层核)。在泥质含量较少的块状白云岩地层中，主要以高角度逆冲断层突破和节理密集发育为特征；泥页岩和泥质含量较高的泥灰岩地层中，以低角度断层突破和断层传播褶皱变形为主。灰岩和白云岩具有相似的抗压强度可能是伸展背景下碳酸盐岩变形对岩性不敏感的原因。碎裂作用和压溶作用促使围岩中泥质成分和氧化物在主断层面富集，阻碍流体运移。

关键词: 黔南地区, 构造变形, 冲断层分带, 碳酸盐岩, 泥质含量, 断层封闭性

Abstract:

The structural deformation and preservation conditions are the main controlling factors for hydrocarbon exploration in carbonate rocks. The structural elements from photomicrograph, outcrop, seismic cross-section and laboratory data including mechanical properties and petrophysical properties were analyzed. The characteristics of deformation and fault sealing ability around the Changming thrust zone in South Guizhou were discussed. The evidence and characteristics of zonation were found around the thrust zones including fault core and damage zone. The relatively high-angle breakthrough faults and high-density joints were well developed in the massive and clay-poor dolomites. The faults in the high-content clay mudstone and marlites tended to breakup on low-angle and formed the fault-propagation fold. There is only a little difference in the tensile strength between the limestone and dolostones, which results in the similar deformation in the extensional environment. Under the action of cataclasis and pressure dissolution, the argillaceous content and oxidation are rich on the main fault surface where the fluid is impeded and which is good for fault sealing.

Key words: South Guizhou, structural deformation, thrust zonation, carbonate rock, clay content, fault sealing ability

崔敏汤良杰. 黔南碳酸盐岩地区断层周缘构造变形及封闭性[J]. 石油学报, 2010, 31(5): 781-786.

CUI Min TANG Liangjie. Structural deformation and sealing ability around fault in carbonate rock area of South Guizhou[J]. Editorial office of ACTA PETROLEI SINICA, 2010, 31(5): 781-786.

参考文献

[1]陈洪德,倪新锋,刘文均,等.中国南方盆地覆盖类型及油气成藏[J].石油学报,2008,29(3):317-323.

Chen Hongde,Ni Xinfeng,Liu Wenjun,et al.Overlay relationship of basins and hydrocarbon accumulation in South China

[J].Acta Petrolei Sinica,2008,29(3):317-323.

[2]Rawling G C,Goodwin L B,Wilson J L.Internal architecture,permeability structure,and hydrologic significance of contrasting fault-zone types[J].Geology,2001,29(1):43-46.

[3]Flodin E,Gerdes M,Aydin A,et al.Petrophysical properties of cataclastic fault rock in sandstone[G]//Sorkhabi R,Tsuji Y.Faults,fluid flow,and petroleum traps.Canada:AAPG Memoir 85，2005：197-217.

[4]Agosta F,Aydin A.Architecture and deformation mechanism of a basin-bounding normal fault in Mesozoic platform carbonates,central Italy[J].Journal of Structural Geology,2006,28(8):1445-1467.

[5]Tondi E,Antonellini M,Aydin A,et al.The role of deformation bands,stylolites and sheared stylolites in fault development in carbonate grainstones of Majella Mountain,Italy[J].Journal of Structural Geology,2006,28(3):376-391.

[6]刘运黎,沈忠民,丁道桂,等.江南—雪峰山推覆体前缘沥青古油藏及油源对比[J].成都理工大学学报：自然科学版，2008,35(1):34-40.

Liu Yunli,Shen Zhongmin,Ding Daogui,et al.The characters of the old asphalt-oil pool in the Jiangnan-Xuefeng thrust nappe front and the correlation of oil sources[J].Journal of Chengdu University of Technology：Science & Technology Edition,2008,35(1):34-40.

[7]贵州省地质矿产局.贵州省区域地质志[M].北京:地质出版社,1987:608-616.

Guizhou Bureau of Geology and Mineral Resources.Regional geology of Sichuan Province[M].Beijing:Geological Publishing House,1987:608-616.

[8]崔敏,汤良杰,郭彤楼,等.黔南地区古生代正断层对构造特征的制约[J].现代地质,2009,23(3)：409-413.

Cui Min,Tang Liangjie,Guo Tonglou,et al.Constraints of Paleozoic normal faults on structural characteristics in South Guizhou

[J].Geoscience,2009,23(3):409-413.

[9]Billi A,Salvini F,Storti F.The damage zone-fault core transition in carbonate rocks:Implications for fault growth,structure and permeability[J].Journal of Structural Geology,2003,25(11):1779-1794.

[10]崔敏,汤良杰，郭彤楼,等.黔东南地区褶皱构造样式及其断层突破模式[J].地球科学——中国地质大学学报,2009,34(6):907-913.

Cui Min,Tang Liangjie,Guo Tonglou,et al.Structural style and thrust breakthrough model of fold in Southeast Guizhou

[J].Earth Science:Journal of China University of Geosciences,2009,34(6):907-913.

[11]Mollema P N,Antonellini M.Development of strike-slip faults in the dolomites of the Sella Group,Northern Italy[J].Journal of Structural Geology,1999,21(3):273-292.

[12]Graham B,Antonellini M,Aydin A.Formation and growth of normal faults in carbonates within a compressive environment

[J].Geology,2003,31(1):11-14.

[13]Ferrill D A,Morris A P.Fault zone deformation controlled by carbonate mechanical stratigraphy,Balcones fault system,Texas

[J].AAPG Bulletin,2008,92(3):359-380.

[14]Davatzes N C,Aydin A,Eichhubl P.Overprinting faulting mechanisms during the development of multiple fault sets in sand stone,Chimney Rock fault array,Utah,USA[J].Tectonophysics,2003,363(1/2): 1-18.

[15]Agosta F,Prasad M,Aydin A.Physical properties of carbonate fault rocks,Fucino basin(Central Italy):Implications for fault seal in platform carbonates[J].Geofluids,2007,7(14):19-32.

[16]付晓飞,潘国强,贺向阳,等.大庆长垣南部黑帝庙浅层生物气的断层侧向封闭性[J].石油学报,2009,30(5):678-684.

Fu Xiaofei,Pan Guoqiang,He Xiangyang,et al.Lateral sealing of faults for shallow biogas in Heidimiao Formation of the southern Daqing placanticline[J].Acta Petrolei Sinica,2009,30(5):678-684.

[17]吕延防,沙子萱,付晓飞,等.断层垂向封闭性定量评价方法及其应用[J].石油学报,2007,28(5):34-38.

Lü Yanfang,Sha Zixuan,Fu Xiaofei,et al.Quantitative evaluation method for fault vertical sealing ability and its application

[J].Acta Petrolei Sinica,2007,28(5):34-38.

[18]李振生,刘德良,刘波,等.断裂性能差异的力学和化学因素分析[J].天然气地球科学,2005,16(4):485-491.

Li Zhensheng,Liu Deliang,Liu Bo,et al.The analysis of mechanical and chemical factors making the difference of fault’s action

[J].Natural Gas Geoscience,2005,16(4):485-491.

黔南碳酸盐岩地区断层周缘构造变形及封闭性

Structural deformation and sealing ability around fault in carbonate rock area of South Guizhou

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	刘鹏, 王永诗, 宋明水, 刘雅利, 王敏, 张顺, 王彤达. 碳酸盐岩断裂带断层岩特征及演化——以渤海湾盆地济阳坳陷车镇凹陷下古生界为例[J]. 石油学报, 2021, 42(5): 588-597.
[2]	张友, 李强, 郑兴平, 厉玉乐, 沈安江, 朱茂, 熊冉, 朱可丹, 王显东, 齐井顺, 张君龙, 邵冠铭, 佘敏, 宋叙, 孙海航. 塔里木盆地东部古城—肖塘地区寒武纪—奥陶纪台地类型、演化过程及有利储集相带[J]. 石油学报, 2021, 42(4): 447-465.
[3]	张世铭, 王建功, 张永庶, 张小军, 张婷静, 崔俊. 柴达木盆地西部地区下干柴沟组湖相白云岩晶间孔型储层物性下限的确定[J]. 石油学报, 2021, 42(1): 45-55,118.
[4]	吴小奇, 陈迎宾, 翟常博, 王彦青, 曾华盛, 刘文汇, 杨俊, 倪春华, 周凌方, 宋晓波. 川西坳陷中三叠统雷口坡组天然气气源对比[J]. 石油学报, 2020, 41(8): 918-927,1018.
[5]	王建功, 张永庶, 李翔, 徐丽, 石亚军, 黄叶秋, 王玉林, 管斌, 张世铭, 高妍芳. 柴达木盆地西部渐新统纹理石沉积特征与原位成藏[J]. 石油学报, 2020, 41(8): 940-959.
[6]	刘宝增, 漆立新, 李宗杰, 刘军, 黄超, 杨林, 马灵伟, 龚伟. 顺北地区超深层断溶体储层空间雕刻及量化描述技术[J]. 石油学报, 2020, 41(4): 412-420.
[7]	程洪, 汪彦, 鲁新便. 塔河地区深层碳酸盐岩断溶体圈闭类型及特征[J]. 石油学报, 2020, 41(3): 301-309.
[8]	齐宁, 陈国彬, 李振亮, 梁冲, 何龙. 基于分步算法的裂缝性碳酸盐岩油藏大尺度酸化数值模拟[J]. 石油学报, 2020, 41(3): 348-362,371.
[9]	王宜林, 宋新民, 王贵海, 汪华, 李兆明, 张红, 聂臻. 中东地区油气合作区快速规模上产关键技术与实践[J]. 石油学报, 2020, 41(12): 1633-1642.
[10]	郭建春, 任冀川, 王世彬, 苟波, 赵俊生, 伍林. 裂缝性致密碳酸盐岩储层酸压多场耦合数值模拟与应用[J]. 石油学报, 2020, 41(10): 1219-1228.
[11]	康琳, 吕丁友, 尚锁贵, 高京华, 张江涛. 辽东湾坳陷新生代构造变形特征及营潍断裂带的表现[J]. 石油学报, 2019, 40(S2): 79-90.
[12]	刘航宇, 田中元, 刘波, 郭睿, 石开波, 叶玉峰. 中东地区巨厚强非均质碳酸盐岩储层分类与预测——以伊拉克W油田中白垩统Mishrif组为例[J]. 石油学报, 2019, 40(6): 677-691.
[13]	郭荣涛, 马达德, 张永庶, 刘波, 陈晓冬, 崔俊, 王鹏, 张庆辉, 姜营海, 李亚锋. 柴达木盆地英西地区下干柴沟组上段超压孔缝型储层特征及形成机理[J]. 石油学报, 2019, 40(4): 411-422.
[14]	马永生, 何治亮, 赵培荣, 朱宏权, 韩俊, 尤东华, 张军涛. 深层—超深层碳酸盐岩储层形成机理新进展[J]. 石油学报, 2019, 40(12): 1415-1425.
[15]	韩剑发, 苏洲, 陈利新, 郭东升, 张银涛, 吉云刚, 张慧芳, 袁敬一. 塔里木盆地台盆区走滑断裂控储控藏作用及勘探潜力[J]. 石油学报, 2019, 40(11): 1296-1310.