塔中低凸起的构造属性和解释方法

doi:10.11743/ogg20110517

石油与天然气地质 ›› 2011, Vol. 32 ›› Issue (5): 777-786.doi: 10.11743/ogg20110517

塔中低凸起的构造属性和解释方法

管树巍¹, 杨海军², 韩剑发², 李本亮¹, 罗春树²

1. 中国石油勘探开发研究院盆地构造与油气成藏重点实验室,北京 100083;
2. 中国石油塔里木油田分公司勘探开发研究院,新疆库尔勒 841000

收稿日期:2010-09-25 修回日期:2011-09-01 出版日期:2011-10-28 发布日期:2011-12-16
第一作者简介:管树巍(1970-),男,高级工程师,盆地构造和勘探方法研究。
基金项目:
国家科技重大专项(2008ZX05003-001);国家重点基础研究发展计划("973"计划)项目(2006CB202301)。

Structural properties and interpretation methods of the Tazhong Low Salient

Guan Shuwei¹, Yang Haijun², Han Jianfa², Li Benliang¹, Luo Chunshu²

1. Key Laboratory of Basin Structure and Petroleum Accumulation,PetroChina Research Institute of Petroleum Exploration and Development,Beijing 100083,China;
2. Research Institute of Petroleum Exploration and Development, PetroChina Tarim Oilfield Company,Korla,Xinjiang 841000,China

Received:2010-09-25 Revised:2011-09-01 Online:2011-10-28 Published:2011-12-16

摘要/Abstract

摘要：

塔中低凸起是中奥陶世-晚泥盆世早期塔东南前陆冲断体系的一部分。这个时期塔中地区的断裂以北倾反冲为主,并可能与深部由南向北逆冲的主控断裂交汇,形成向北扩展的楔形构造前锋。塔中低凸起历经多期断裂作用,在不同地层单元内部形成了特有的构造形态,如震旦系-奥陶系构造层内主要发育北西向的挤压断层相关褶皱,志留系-泥盆系构造层内主要发育北东向的负花状构造和拉分地堑,石炭系-二叠系构造层内主要发育由岩浆刺穿或底辟形成的正花状构造和垮塌构造。多期断裂作用也造成了早期构造通常被晚期构造切割与破坏而在地震资料上难以识别的问题,构造解释工作应尽量在纵横比例相等的地震剖面上进行,以直观显示并准确识别这些构造层内部的变形形态,并从资料可信度高的位置入手,由已知到未知,逐步获得资料不好地区的断裂解释方案。

关键词: 构造属性, 前缘隆起, 构造层, 断裂解释, 塔中低凸起

Abstract:

Tazhong low salient is part of the foreland thrusting system in the southeastern Tarim Basin from Middle Ordovician to early Late Devonian.During this geologic period,the faults in Tazhong area were dominated by north-dipping and thrusts,and might intersected the deep north-thrusting major fault,forming a north-propagating wedge structure front.The low salient in Tazhong area experienced multistage tectonic movements,resulting in different structural geometries in different stratigraphic units.For example,NW-trending compressional fault-related folds dominate the Sinian-Ordovician structural layer;NE-trending negative flow structures and pull-apart grabens are predominant in the Silurian-Devonian structural layer;while positive flow structures and collapse structures resulted from magma invasion or diaper are prevalent in the Carboniferous-Permian structural layer.The early structures are commonly destroyed by the later structures duo to multistage faulting,making it difficult to identifying them on seismic section.Therefore,structure interpretation should be based on the seismic profiles with approximate the same vertical and horizontal scales,so as to correctly define the deformation features in these structural layers and extrapolate into areas where seismic data quality is low.

Key words: structural property, forebulge, structural layer, fault interpretation, Tazhong Low Salient area

中图分类号:

TE121.2

管树巍,杨海军,韩剑发,等. 塔中低凸起的构造属性和解释方法[J]. 石油与天然气地质, 2011, 32(5): 777-786. doi: 10.11743/ogg20110517 Guan Shuwei,Yang Haijun,Han Jianfa,et al. Structural properties and interpretation methods of the Tazhong Low Salient[J]. Oil & Gas Geology, 2011, 32(5): 777-786. doi: 10.11743/ogg20110517

参考文献

[1] 何登发, 周新源, 张朝军, 等. 塔里木地区奥陶纪原型盆地类型及其演化[J]. 科学通报, 2007, 52(增刊1): 126-135. He Dengfa, Zhou Xinyuan, Zhang Chaojun, et al. Type and evolution of Ordovician original basin in Tarim area[J]. Chinese Science Bulletin, 2007, 52(S1): 126-135. [2] 何登发, 周新源, 杨海军, 等. 塔里木盆地克拉通内古隆起的成因机制与构造类型[J]. 地学前缘, 2008, 15(2): 207-221. He Dengfa, Zhou Xinyuan, Yang Haijun, et al. Formation mechanism and tectonic types of intracratonic paleo-uplifts in the Tarim basin[J]. Earth Science Frontiers, 2008, 15(2): 207-221. [3] 何登发, 李德生. 塔里木盆地构造演化与油气聚集[M]. 北京: 地质出版社, 1996: 1-171. He Dengfa, Li Desheng. Structural evolution and hydrocarbon accumulation of Tarim Basin[M]. Beijing: Geological Publishing House, 1996: 1-171. [4] 李明杰, 郑孟林, 冯朝荣, 等. 塔中低凸起的结构特征及其演化[J]. 西安石油大学学报(自然科学版), 2004, 19(4): 43-46. Li Mingjie, Zheng Menglin, Feng Chaorong, et al. Structural characteristics and evolution of Tazhong low uplift[J]. Journal of Xi'an Shiyou University(Natural Science Edition), 2004, 19(4): 43-46. [5] 张振生, 李明杰, 刘社平. 塔中低凸起的形成和演化[J]. 石油勘探与开发, 2002,29(1): 28-31. Zhang Zhensheng, Li Mingjie, Liu Sheping. Generation and evolution of Tazhong low uplift[J]. Petroleum Exploration and Development, 2002,29(1): 28-31. [6] 贾承造,魏国齐, 姚慧君, 等. 中国塔里木盆地构造特征与油气[M] . 北京: 石油工业出版社, 1997: 1-438. Jia Chengzao, Wei Guoqi, Yao Huijun, et al. Structural feature and hydrocarbon potential in Tarim Basin, China[M]. Beijing: Petroleum Industry Press, 1997: 1-438. [7] 贾承造, 魏国齐. 塔里木盆地构造特征与含油气性[J] . 科学通报, 2002, 47 (增刊1): 1-8. Jia Chengzao, Wei Guoqi. Structural feature and hydrocarbon potential in Tarim Basin[J]. Chinese Science Bulletin, 2002, 47(S1): 1-8. [8] 邬光辉, 李启明, 肖中尧, 等. 塔里木盆地古隆起演化特征及油气勘探[J]. 大地构造与成矿学, 2009, 33(1): 124-130. Wu Guanghui, Li Qiming, Xiao Zhongyao, et al. The evolution characteristics of paleo-uplifts in Tarim Basin and its exploration directions for oil and gas[J]. Geotectonica Et Metallogenia, 2009, 33(1): 124-130. [9] 吕修祥, 胡轩. 塔里木盆地塔中低凸起油气聚集与分布[J]. 石油与天然气地质, 1997, 18(4): 288-294. Lv Xiuxiang, Hu Xuan. Hydrocarbon accumulation and distribution in Tazhong low uplift of Tarim Basin[J]. Oil & Gas Geology,1997, 18(4): 288-294. [10] 张小兵, 赵锡奎. 塔里木盆地塔中构造演化与志留系油气关系[J]. 天然气勘探与开发, 2004, 6(2): 11-15. Zhang Xiaobing, Zhao Xikui. Relationship between Tazhong tectonic evolution and Silurian hydrocarbon distribution in Tarim Basin[J]. Natural Gas Exploration & Development, 2004, 27(2): 11-15. [11] 李曰俊, 吴根耀, 孟庆龙, 等. 塔里木盆地中央地区的断裂系统: 几何学、运动学和动力学背景[J]. 地质科学, 2008, 43(1): 82-118. Li Yuejun, Wu Genyao, Meng Qinglong, et al. Fault systems in central area of the Tarim Basin: geometry, kinematics and dynamic settings[J]. Scientia Geologica Sinica, 2008, 43(1): 82-118. [12] 张仲培,王毅,云金表,等. 塔中地区断裂不同演化阶段对油气聚集的控制[J]. 石油与天然气地质,2009,30(3):316-323. Zhang Zhongpei, Wang Yi, Yun Jinbiao, et al. Control of faults at different evolution stages on hydrocarbon accumulation in Tazhong area, the Tarim Basin[J]. Oil & Gas Geology,2009,30(3):316-323. [13] 宁飞,汤良杰,张钰,等. 塔中隆起早古生代反转构造及其石油地质意义[J]. 石油与天然气地质,2010,31(1):57-62. Ning Fei,Tang Liangjie,Zhang Yu,et al. Eopaleozoic inversion structures in the Tazhong Uplift and their significance to petroleum geology[J]. Oil & Gas Geology,2010,31(1):57-62. [14] 邬光辉,汪海,陈志勇,等. 塔里木盆地奥陶系碳酸盐岩复杂油气藏的特性[J]. 石油与天然气地质,2010,31(6):763-769. Wu Guanghui,Wang Hai,Chen Zhiyong, et al. Characteristics of the complex Ordovician carbonate reservoirs in the Tarim Basin[J]. Oil & Gas Geology,2010,31(6):763-769. [15] 肖朝晖,王招明,姜仁旗, 等. 塔里木盆地寒武系碳酸盐岩层序地层特征[J]. 石油与天然气地质,2011,32(1):1-10. Xiao Zhaohui,Wang Zhaoming,Jiang Renqi,et al. Sequence stratigraphic features of the Cambrian carbonate rocks in the Tarim Basin[J]. Oil & Gas Geology,2011,32(1):1-10. [16] 王祥,张敏,刘玉华. 塔里木盆地塔中地区天然气成因及其差异[J]. 石油与天然气地质,2010,31(3):335-342. Wang Xiang,Zhang Min, Liu Yuhua. Origins of natural gas in Tazhong area, the Tarim Basin and their differences[J]. Oil & Gas Geology,2010,31(3):335-342. [17] 丁道桂, 汤良杰. 塔里木盆地形成与演化[M]. 南京: 河海大学出版社, 1996: 182-253. Ding Daogui, Tang Liangjie. Formation and evolution of Tarim Basin[M]. Nanjing: Hehai University Press, 1996: 182-253. [18] 康南昌. 阿尔金断裂系与塔中构造带的形成与演化[J]. 石油地球物理勘探, 2002, 37(1): 48-52. Kang Nanchang. Altun fault system and formation and evolution of Tazhong structural belt[J]. Oil Geophysical Prospecting, 2002, 37(1): 48-52. [19] Suppe J. Geometry and kinematics of fault-bend folding[J]. American Journal of Science, 1983, 283(7): 684-721. [20] Suppe J, Medwedeff D. Geometry and kinematics of fault-pro-pagation folding[J]. Eclogae Geologicae Helvetiae, 1990, 83(3): 409-454. [21] Shaw J H, Hook S C, Suppe J. Structural trend analysis by axial surface mapping[J]. American Association of Petroleum Geologists Bulletin, 1994, 78(5): 700-721. [22] Shaw J H, Suppe J. Earthquake hazards of active blind-thrust faults under the central Los Angeles basin, California[J]. Journal of Geophysical Research, 1996, 101(B4): 8623-8642. [23] Shaw J H, Bilotte F, Brennan P A. Patterns of imbricate thrusting[J]. Geological Society of America Bulletin, 1999, 111(7): 1140-1154. [24] Shaw J H, Connors C, Suppe J. Seismic interpretation of contractional fault-related folds: an AAPG seismic atlas[M]//American Association of Petroleum Geologists Special Publication, 2004: 1-270. [25] Medwedeff D A, Suppe J. Multibend fault-bend folding[J]. Journal of Structural Geology, 1997, 19(3-4): 279-292.

塔中低凸起的构造属性和解释方法

Structural properties and interpretation methods of the Tazhong Low Salient

PDF (PC)

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 10

编辑推荐

Metrics

[1]	单帅强, 张煜颖, 张锐锋. 渤海湾盆地徐水凹陷地质结构与构造演化[J]. 石油与天然气地质, 2018, 39(5): 1037-1047.
[2]	刘长磊, 张艺琼, 张永, 孙方源, 陈槚俊, 何登发. 塔北-塔中区域构造地质大剖面解析及古隆起成因新解[J]. 石油与天然气地质, 2018, 39(5): 1001-1010.
[3]	易泽军, 何登发. 准噶尔盆地东部构造地层层序及盆地演化[J]. 石油与天然气地质, 2018, 39(5): 932-942.
[4]	陈石, 郭召杰, 漆家福, 邢向荣. 准噶尔盆地西北缘三期走滑构造及其油气意义[J]. 石油与天然气地质, 2016, 37(3): 322-331.
[5]	漆家福, 陈书平, 杨桥, 于福生. 准噶尔-北天山盆山过渡带构造基本特征[J]. 石油与天然气地质, 2008, 29(2): 252-260,282.
[6]	张臣, 郑多明, 李江海. 柯坪断隆古生代的构造属性及其演化特征[J]. 石油与天然气地质, 2001, 22(4): 314-318.
[7]	董月霞, 周海民, 夏文臣. 南堡凹陷火山活动与裂陷旋回[J]. 石油与天然气地质, 2000, 21(4): 304-307.
[8]	夏文臣, 张宁, 袁晓萍, 孟科, 张兵山, 彭晓群. 柴达木侏罗系的构造层序及前陆盆地演化[J]. 石油与天然气地质, 1998, 19(3): 173-180,195.
[9]	陈全茂, 张光亚, 梁晓东, 陈昭年, 周绍强, 王占忠. 张强凹陷及邻区火山岩特征与构造属性[J]. 石油与天然气地质, 1997, 18(4): 309-313.
[10]	吕修祥, 胡轩. 塔里木盆地塔中低凸起油气聚集与分布[J]. 石油与天然气地质, 1997, 18(4): 288-293,308.