Structural characteristics and physical modeling of Fusha-Keliyang segment of the western Kunlun thrust belt in southwestern Tarim Basin

doi:10.7623/syxb201206004

Editorial office of ACTA PETROLEI SINICA ›› 2012, Vol. 33 ›› Issue (6): 941-948.DOI: 10.7623/syxb201206004

• Petroleum Exploration • Previous Articles Next Articles

Structural characteristics and physical modeling of Fusha-Keliyang segment of the western Kunlun thrust belt in southwestern Tarim Basin

TIAN Jiqiang 1,2 　JIA Chengzao 3 　DUAN Shufu 1 　CHEN Zhuxin 1　XIAO Ancheng 4　 GAO Li 1 　CHEN Zhiyong 1 　WANG Chenglin 1

Received:2012-04-05 Revised:2012-07-31 Online:2012-11-25 Published:2012-12-07

塔西南昆仑山前冲断带甫沙-克里阳段构造特征与物理模拟

田继强 1,2　贾承造 3　段书府 1 　陈竹新 1　肖安成 4　高　力 1　陈志勇 1 　王成林 1

1. 中国石油勘探开发研究院北京 100083; 2. 中石油煤层气有限责任公司北京 100028; 3. 中国石油天然气集团公司北京 100724; 4. 浙江大学浙江杭州 310058

通讯作者: 田继强
作者简介:田继强，男，1981年8月生，2011年获中国石油勘探开发研究院矿产普查与勘探专业工学博士学位，现为中石油煤层气有限责任公司工程师，主要从事煤层气勘探开发研究工作。
基金资助:
国家重大科技专项（2011ZX05003-002）及全国油气资源战略选区调查与评价国家专项（2009GYXQ02-01）资助。

Abstract

Abstract:

The establishment of seismic structural models has been great difficulty in the petroleum exploration of southwestern Tarim Basin due to complicated surface conditions. The fine structural interpretation and growth formation analysis of 2D seismic sections in Fusha-Keliyang segment were performed based on outcrop survey, 2D seismic data and drilling materials. The result shows that structural types of the western Kunlun foreland thrust belt mainly include thick-skinned structure, Alberta-style triangle zone, passive-roof double-thrust structure and fault-bend fold. Furthermore, three rows of anticlinal structure belts in the piedmont zone of the western Kunlun mountain developed from south to north in Early Pliocene, Middle-Late Pliocene and Early-Middle Pleistocene, respectively. On the basis of the foregoing result, a double-decollement plus unidirectional compressing pattern was put forward with respect to the formation of the western Kunlun thrust belt in the southwestern Tarim Basin. A sandbox physical modeling experiment was accordingly designed and carried out. The experimental result indicates that the double-decollement plus unidirectional compressing pattern can be able to better simulate the deformation process and typical structure style of Fusha-Keliyang segment in the western Kunlun thrust belt and the physical simulation fundamentally coincides well with seismic structural interpretation. In addition, both the intensive northward compression created by the lift of the western Kunlun orogenic zone and the double-decollement stratigraphic framework are the two important factors for the formation of Fusha-Keliyang structural segment in the western Kunlun thrust belt.

Key words: southwestern Tarim Basin, piedmont, thrust belt, Fusha-Keliyang segment, structural characteristics, physical modeling

摘要：

受复杂地表条件影响，地震构造建模一直是塔西南昆仑山前冲断带油气勘探中的难点。基于野外地质调查、二维地震、钻井等资料，通过对二维地震剖面进行精细构造解释和生长地层分析，表明塔西南昆仑山前冲断带甫沙-克里阳段主要发育基底卷入式构造、阿尔伯特型构造三角带、被动顶板双重逆冲构造和断层转折褶皱等构造样式，塔西南昆仑山前3排背斜构造带自南向北依次发育于上新世早期、上新世中晚期和更新世早中期。在此基础上，提出了“双滑脱层-单向挤压”冲断构造发育模式，设计并开展了相应的砂箱物理模拟实验。实验结果表明，该模型能够较好地模拟塔西南昆仑山前冲断带甫沙-克里阳段的“前展式”构造变形过程和典型构造样式，物理模拟实验结果与地震构造解释模型吻合，西昆仑造山带隆升产生的强烈向北挤压力和双滑脱层地层结构是塔西南昆仑山前冲断带甫沙-克里阳段构造形成的2个关键因素。

关键词: 塔西南, 山前带, 冲断带, 甫沙-克里阳段, 构造特征, 物理模拟

TIAN Jiqiang JIA Chengzao DUAN Shufu CHEN Zhuxin XIAO Ancheng GAO Li. Structural characteristics and physical modeling of Fusha-Keliyang segment of the western Kunlun thrust belt in southwestern Tarim Basin[J]. Editorial office of ACTA PETROLEI SINICA, 2012, 33(6): 941-948.

田继强贾承造段书府陈竹新肖安成高　力. 塔西南昆仑山前冲断带甫沙-克里阳段构造特征与物理模拟[J]. 石油学报, 2012, 33(6): 941-948.

References

[1] 张玮，漆家福，雷刚林，等.塔西南拗陷甫沙构造带结构模型及形成机制[J].西南石油大学学报：自然科学版，2011,33(1):42-48.

Zhang Wei,Qi Jiafu,Lei Ganglin,et al.Analysis of structure model and formation mechanism of Fusha structure zone in southwestern depression of Tarim Basin[J].Journal of Southwest Petroleum University:Science & Technology Edition,2011，33(1):42-48.

[2] 贾承造，魏国齐，李本亮，等.中国中西部两期前陆盆地的形成及其控气作用[J].石油学报，2003,24(2):13-17.

Jia Chengzao,Wei Guoqi,Li Benliang,et al.Tectonic evolution of two-epoch foreland basins and its control for natural gas accumulation in China’s mid-western areas[J].Acta Petrolei Sinica,2003,24(2):13-17.

[3] 王平在，何登发，雷振宇，等.中国中西部前陆冲断带构造特征[J].石油学报，2002,23(3):11-17.

Wang Pingzai,He Dengfa,Lei Zhenyu,et al.Tectonic features of foreland thrust belts in central and western China[J].Acta Petrolei Sinica,2002,23(3):11-17.

[4] 贾承造，宋岩，魏国齐，等.中国中西部前陆盆地的地质特征及油气聚集[J].地学前缘，2005,12(3):3-13.

Jia Chengzao,Song Yan,Wei Guoqi,et a1.Geological features and petroleum accumulation in the foreland basins in central and western China[J].Earth Science Frontiers,2005,12(3):3-13.

[5] 丁道桂，王道轩，刘伟新，等.西昆仑造山带与盆地[M].北京：地质出版社，1996.

Ding Daogui,Wang Daoxuan,Liu Weixin,et al.The western Kunlun orogenic belt and basin[M].Beijing:Geological Publishing House,1996.

[6] 牟中海，唐勇，崔炳富，等.塔西南地区地层剥蚀厚度恢复研究[J].石油学报，2002,23(1):40-44.

Mu Zhonghai,Tang Yong,Cui Bingfu,et al.Erosion thickness restoration in southwest Tarim Basin[J].Acta Petrolei Sinica,2002,23(1):40-44.

[7] 胡建中，谭应佳，张平，等.塔里木盆地西南缘山前带逆冲推覆构造特征[J].地学前缘，2008,15(2)：222-231.

Hu Jianzhong，Tan Yingjia，Zhang Ping，et a1.Structural features of Cenozoic thrust-fault belts in the piedmont of southwestern Tarim Basin[J].Earth Science Frontiers,2008,15(2):222-231.

[8] 程晓敢，雷刚林，陈汉林，等.西昆仑山前甫沙-克里阳地区新生代变形特征及油气控制作用[J].石油学报，2011,32(1):83-89.

Cheng Xiaogan,Lei Ganglin,Chen Hanlin,et al.Cenozoic structural deformation of the Fusha-Keliyang area in the piedmont of the western Kunlun mountains and its control on hydrocarbon accumulation[J].Acta Petrolei Sinica,2011,32(1):83-89.

[9] 刘胜，汪新，伍秀芳，等.塔西南山前晚新生代构造生长地层与变形时代[J].石油学报，2004,25(5):24-28.

Liu Sheng,Wang Xin,Wu Xiufang,et al.Growth strata and the deformation time of the late Cenozoic along front belts of Pamir-western Kunlun-southwestern Tianshan in China[J].Acta Petrolei Sinica,2004,25(5):24-28.

[10] 伍秀芳，刘胜，汪新，等.帕米尔-西昆仑北麓新生代前陆褶皱冲断带构造剖面分析[J].地质科学，2004,39(2):260-271.

Wu Xiufang,Liu Sheng,Wang Xin,et al.Analysis on structural sections in the Cenozoic Pamir-western Kunlun foreland fold-and-thrust belt[J].Chinese Journal of Geology,2004,39(2):260-271.

[11] 曲国胜，李亦纲，李岩峰，等.塔里木盆地西南前陆构造分段及其成因[J].中国科学D辑：地球科学，2005,35(3):193-202.

Qu Guosheng,Li Yigang,Li Yanfeng,et al.Segmentations of foreland belts and their tectonic mechanism in the southwest Tarim Basin[J].Science in China Ser.D:Earth Sciences,2005,35(3):193-202.

[12] 向奎.塔里木盆地西南边缘压扭构造体系及其石油地质意义[J].古地理学报，2006,8(2):233-240.

Xiang Kui.Transpressional structural systems and their petroleum geological significance in southwestern margin of Tarim Basin[J].Journal of Palaeogeography,2006,8(2):233-240.

[13] 胡望水，陈毓遂，肖安成，等.塔西南坳陷主要断裂带构造特征及其控油作用[J].新疆石油地质，1997,18(3):201-207.

Hu Wangshui,Chen Yusui,Xiao Ancheng,et al.Structural features of major fault zones in the southwest depression in Tarim Basin and their control on oil accumulation[J].Xinjiang Petroleum Geology,1997,18(3):201-207.

[14] 张玮，漆家福，李勇.塔里木盆地西南缘构造样式及其主导因素[J].地质科学，2011,46(3):723-732.

Zhang Wei,Qi Jiafu,Li Yong.Structural styles in south-western margin of Tarim Basin and their dominate factors[J].Chinese Journal of Geology,2011,46(3):723-732.

[15] 杨海军，王步清，杨芝林，等.塔里木盆地西南坳陷柯东构造建模与油气勘探[J].地质科学，2011,46(2):456-465.

Yang Haijun，Wang Buqing,Yang Zhilin，et al.Structure modeling and hydrocarbon exploration of Kedong structural belt in southwestern Tarim Basin[J].Chinese Journal of Geology,2011,46(2):456-465.

[16] 梁向豪，罗仁泽，周翼，等.巨厚黄土覆盖区表层地震信号衰减测量[J].天然气技术，2010,4(5):1-3.

Liang Xianghao,Luo Renze,Zhou Yi,et al.Measurement of seismic signal attenuation for surface in very-thick-loess-covering area[J].Natural Gas Technolgy,2010,4(5):1-3.

[17] 贾承造,张师本，吴绍祖，等.塔里木盆地及周边地层（上、下册）[M].北京：科学出版社，2004.

Jia Chengzao，Zhang Shiben,Wu Shaozu,et al.Statigraphy of the Tarim Basin and adjacent areas(volume I,II)[M].Beijing:Science Press,2004.

[18] 张师本，黄智斌，朱怀诚,等.塔里木盆地覆盖区显生宙地层[M].北京：石油工业出版社，2004.

Zhang Shiben,Huang Zhibin,Zhu Huaicheng，et al.Phanerozoic strata in the overlay area of Tarim Basin[M].Beijing:Petroleum Industry Press,2004.

[19] 陈杰，尹金辉，曲国胜，等.塔里木盆地西缘西域组的底界、时代、成因与变形过程的初步研究[J]．地震地质，2000,22(增刊)：104-116.

Chen Jie,Yin Jinghui,Qu Guosheng,et al．Timing，lower boundary，genesis，and deformation of Xiyu Formation around the western margins of Tarim Basin[J]．Seismology and Geology，2000,22 (supplement):104-116.

[20] 宋岩，方世虎，赵孟军，等.前陆盆地冲断带构造分段特征及其对油气成藏的控制作用[J].地学前缘，2005,12(3)：31-38.

Song Yan,Fang Shihu,Zhao Mengjun,et a1.The structural segmentation of foreland thrust belts and its implications for hydrocarbon accumulation in foreland basins in central and western China[J].Earth Science Frontiers，2005,12(3)：31-38.

[21] 肖安成.塔里木盆地西南缘西昆仑前陆逆冲-褶皱带主滑脱面深度[J].江汉石油学院学报,1996,18(1):19-23.

Xiao Ancheng.Depth of detachment surface in foreland thrust-fold belt of western Kunlun mountain in southwestern Tarim Basin[J].Journal of Jianghan Petroleum Institute,1996,18(1):19-23.

[22] 肖安成.塔里木盆地西南缘的构造特征与油气聚集规律[J].江汉石油学院学报，1997,19(2):1-6.

Xiao Ancheng.Structural characteristics and petroleum accumulation of thrust belt in southwestern margin of Tarim Basin[J].Journal of Jianghan Petroleum Institute,1997,19(2):1-6.

[23] 王步清，谢会文，陈汉林，等.塔里木盆地西南坳陷周缘的滑脱构造[J].地质科学，2011,46(3):733-742.

Wang Buqing,Xie Huiwen,Chen Hanlin,et al.Decollement structure of southwest Tarim depression and its periphery[J].Chinese Journal of Geology,2011,46(3)：733-742.

[24] Couzens-Schultz B A,Vendeville B C,Wiltschko D V.Duplex style and triangle zone formation:insights from physical modeling[J].Journal of Structural Geology,2003,25(10):1623-1644.

[25] 王瑞瑞，张岳桥，董树文，等.构造三角带的概念及其油气勘探意义[J].地质通报,2010,29(2/3)：317-329.

Wang Ruirui,Zhang Yueqiao,Dong Shuwen,et al．The definition of triangle zone and its petroleum prospecting significance[J]．Geological Bulletin of China,2010,29(2/3):317-329.

[26] Zheng Hongbo,Powell C M,An Zhisheng,et al.Pliocene uplift of the northern Tibetan plateau[J].Geology,2000,28(8):715-718.

[27] 单家增.构造模拟实验在石油地质学中的应用[M].北京：石油工业出版社，1996.

Shan Jiazeng.Application of structural simulation experiment in petroleum geology[M].Beijing:Petroleum Industry Press,1996.

[28] McClay K R.Extensional fault systems in sedimentary basins:a review of analogue model studies[J].Marine and Petroleum Geology,1990,7(3):206-233.

[29] Pichot T,Nalpas T.Influence of synkinematic sedimentation in a thrust system with two decollement levels;analogue modeling[J].Tectonophysics,2009,473 (3/4):466-475.

[30] McClay K,Bonora M.Analog models of restraining stopovers in strike-slip fault systems[J].AAPG Bulletin,2001,85(2):233-260.

[31] 时秀朋，李理，龚道好，等.构造物理模拟实验方法的发展与应用[J].地球物理学进展，2007,22(6):1728-1735.

Shi Xiupeng,Li Li,Gong Daohao,et al.The development and application of structure physical modeling[J].Progress in Geophysics,2007,22(6):1728-1735.

[32] 吴兴宁，周建勋.渤海湾盆地构造成因观点剖析[J].地球物理学进展,2000,15(1):98-107.

Wu Xingning,Zhou Jianxun.The anatomy about the tectonic cause of fomation of Bohaiwan Basin[J].Progress in Geophysics,2000,15 (1):98-107.

[33] 张玉兰，王伟峰，马宗晋.准噶尔盆地南缘构造物理模拟实验[J].石油大学学报：自然科学版，2003,27(3):1-5.

Zhang Yulan,Wang Weifeng,Ma Zhongjin.Physical simulation experiment on geological structures in the south of Juggar Basin[J].Journal of the University of Petroleum:Science & Technology Edition,2003,27(3):1-5.

[34] 陈书平，汤良杰，贾承造，等.秋里塔格构造带盐构造形成的传力方式的构造物理模拟[J].西安石油大学学报：自然科学版，2004,19(1):6-10.

Chen Shuping,Tang Liangjie,Jia Chengzao,et al.Tectonophysical modeling of two kinds of stress transmission forms for forming the salt structure in Qiulitake structural zone[J].Journal of Xi’an Shiyou University:Natural Science Edition,2004,19(1):6-10.

[35] Lohrmann J,Kukowski N,Adam J,et al.The impact of analogue material properties on the geometry,kinematics,and dynamics of convergent sand wedges[J].Journal of Structural Geology,2003,25(10):1691-1711.

[36] Panien M,Schreurs G,Pfiffner A.Mechanical behavior of granular materials used in analogue modeling:insights form grain characterization,ring-shear tests and analogue experiments[J].Journal of Structural Geology,2006,28(9):1710-1724.

[37] Byerlee J D.Friction of rocks[J].Pure and Applied Geophysics,1978,116(4/5):615-626.

Structural characteristics and physical modeling of Fusha-Keliyang segment of the western Kunlun thrust belt in southwestern Tarim Basin

塔西南昆仑山前冲断带甫沙-克里阳段构造特征与物理模拟

PDF

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 15

Recommended Articles

Metrics

Comments

[1]	Gao Guohui, Cao Jian, Luo Bing, Xiao Di, Zhang Ya, Chen Cong. Evidence of the Middle Permian marine mixed type source rocks in the northwestern Sichuan Basin and its contribution to large gas reservoirs in Shuangyushi area [J]. Acta Petrolei Sinica, 2020, 41(4): 433-445.
[2]	Guo Zhaojie, Zhao Haonan, Zhang Yuanyuan. Lateral foreland belt—a new type of foreland belt:a case study of Longmenshan [J]. Acta Petrolei Sinica, 2020, 41(12): 1477-1489.
[3]	Cao Zhenglin, Sun Xiujian, Wu Wujun, Tian Guangrong, Zhang Shiming, Li Haibin, Sun Zhiming, Xu Li, Wang Ruiju. Formation and evolution of thrusted paleo-uplift at the margin of Qaidam Basin and its influences on hydrocarbon accumulation [J]. Acta Petrolei Sinica, 2018, 39(9): 980-989.
[4]	Liu Chun, Zhang Ronghu, Zhang Huiliang, Huang Wei, Mo Tao, Zhou Lu. Genetic types and geological significance of micro pores in tight sandstone reservoirs: a case study of the ultra-deep reservoir in the Kuqa foreland thrust belt, NW China [J]. Acta Petrolei Sinica, 2017, 38(2): 150-159.
[5]	Hu Jian, Wang Tieguan, Chen Jianping, Cui Jingwei, Zhang Bin, Shi Shengbao, Wang Xiaomei. Geochemical characteristics and origin patterns of oils in periphery of southwestern Tarim Basin [J]. Acta Petrolei Sinica, 2015, 36(10): 1221-1233.
[6]	Zhuo Qingong, Zhao Mengjun, Li Yong, Wang Yuan. Dynamic sealing evolution and hydrocarbon accumulation of evaporite cap rocks：an example from Kuqa foreland basin thrust belt [J]. ACTA PETROLEI SINICA, 2014, 35(5): 847-856.
[7]	Wu Zhenyun, Yin Hongwei, Wang Xin, Zheng Junzhang, Wang Xingyuan. Simulation of salt structure formation and evaluation of its geological significance to oil-gas accumulation：a case study of the Sudanese Red Sea rift basin [J]. ACTA PETROLEI SINICA, 2014, 35(5): 879-889.
[8]	DU Zhili　LIANG Han　SHI Jun　CHEN Cai　WANG Yu . Cenozoic structural deformation and hydrocarbon exploration of Kedong structure in the piedmont of western Kunlun mountain [J]. Editorial office of ACTA PETROLEI SINICA, 2013, 34(1): 22-29.
[9]	CHENG Xiaogan LEI Ganglin CHEN Hanlin DU Zhili LIAO Lin LUO Juncheng. Cenozoic structural deformation of the Fusha-Keliyang area in the piedmont of the western Kunlun Mountains and its control on hydrocarbon accumulation [J]. Editorial office of ACTA PETROLEI SINICA, 2011, 32(1): 83-89.
[10]	CHEN Wei HAO Jinjin ZHANG Jian XIAO Lixin XIAN Di LI Zhigang CHEN Lihua . Geometrical kinematics of the Tuositai Anticline in the southern margin of the Junggar Basin [J]. Editorial office of ACTA PETROLEI SINICA, 2011, 32(1): 90-94.
[11]	MA Yongsheng CAI Xunyu ZHAO Peirong LUO Yi ZHANG Xuefeng. Distribution and further exploration of the large-medium sized gas fields in Sichuan Basin [J]. Editorial office of ACTA PETROLEI SINICA, 2010, 31(3): 347-354.
[12]	NING Fei TANG Liangjie ZHANG Yu WANG Penghao ZHU Chuanling. Structural characteristics and exploration prospect of No.Ⅱ fault zone in Tazhong area [J]. Editorial office of ACTA PETROLEI SINICA, 2010, 31(3): 368-372.
[13]	MA Yongsheng CAI Xunyu ZHAO Peirong LUO Yi ZHANG Xuefeng. Distribution and further exploration of the large-medium sized gas fields in Sichuan Basin [J]. Editorial office of ACTA PETROLEI SINICA, 2010, 31(3): 347-520.
[14]	GUAN Wenlong MA Desheng LIANG Jinzhong LI Chuntao XI Changfeng ZHANG Xialin. Experimental research on thermodynamic characteristics of in-situ combustion zones in heavy oil reservoir [J]. Editorial office of ACTA PETROLEI SINICA, 2010, 31(1): 100-104.
[15]	LI Qi, CHANG Du, XU Yingzhuo, TANG Jiping, LIANG Hongjun. Drilling risk management system based on knowledge integration [J]. Editorial office of ACTA PETROLEI SINICA, 2009, 30(5): 755-759.