塔里木盆地含盐褶皱冲断带变形特征与变形机制
|
摘要
塔里木盆地发育大量含盐褶皱冲断构造,采用对比研究的方法,通过分析塔里木盆地库车坳陷、塘古坳陷和西南坳陷不同滑脱层组合形成的含盐褶皱冲断带规模和构造样式,讨论含盐褶皱冲断带的演化特征和形成机制。对比结果表明,区域滑脱层的深度、厚度和流动性对褶皱冲断带规模及变形样式具有重要的影响。褶皱冲断带的规模和滑脱层强弱成反比,与上覆地层的厚度成反比;在具有强流动性的厚层膏盐层影响下,膏盐层上下地层发生明显解耦变形,上下地层变形呈现明显的不一致性;受流动性较弱的薄层膏盐层影响,膏盐层上下地层可以呈现一定的分层变形特征,但上下层构造变形仍具有较明显的相关性;基于含盐构造变形特征与变形机制分析,认为西南坳陷玛扎塔格构造带的主控因素不是中寒武统膏盐层,而是中寒武统之下的先存构造。
There are a large number of salt-related fold thrust structures in Tarim basin. Using a comparative analysis method, the paper analyzes the scales and structural styles of the salt-related fold thrust belts of various detachment layer combinations in Kuqa depression,Tanggu depression and Southwest depression, and discusses the evolution characteristics and forming mechanism of the salt-related fold thrust belts. The comparison result shows that the depth, thickness and fluidity of the regional detachment layer have significant influences on the scale and deformation style of the fold thrust belt. The scale of the fold thrust belt is inversely proportional to the intensity of the detachment layer and to the thickness of overlying stratum. Influenced by the thick gypsum layer with strong fluidity, the overlying and underlying strata of the gypsum layer show obvious decoupling deformation, and their deformations are different. Influenced by the thin gypsum layer with weak fluidity, the overlying and underlying strata of the gypsum layer have a certain degree of deformation, but there is an obvious correlation between the deformations of the overlying and underlying strata. The analyses on the deformation characteristics and mechanism of the salt-related structure show that the Mazhatage structural belt in the Southwest depression is controlled by the pre-existing structure under the Middle Cambrian strata, rather than controlled by the Middle Cambrian gypsum layer.
There are a large number of salt-related fold thrust structures in Tarim basin. Using a comparative analysis method, the paper analyzes the scales and structural styles of the salt-related fold thrust belts of various detachment layer combinations in Kuqa depression,Tanggu depression and Southwest depression, and discusses the evolution characteristics and forming mechanism of the salt-related fold thrust belts. The comparison result shows that the depth, thickness and fluidity of the regional detachment layer have significant influences on the scale and deformation style of the fold thrust belt. The scale of the fold thrust belt is inversely proportional to the intensity of the detachment layer and to the thickness of overlying stratum. Influenced by the thick gypsum layer with strong fluidity, the overlying and underlying strata of the gypsum layer show obvious decoupling deformation, and their deformations are different. Influenced by the thin gypsum layer with weak fluidity, the overlying and underlying strata of the gypsum layer have a certain degree of deformation, but there is an obvious correlation between the deformations of the overlying and underlying strata. The analyses on the deformation characteristics and mechanism of the salt-related structure show that the Mazhatage structural belt in the Southwest depression is controlled by the pre-existing structure under the Middle Cambrian strata, rather than controlled by the Middle Cambrian gypsum layer.
引文
[1]汤良杰,金之钧,贾承造,等.库车前陆褶皱-冲断带前缘大型盐推覆构造[J].地质学报,2004,78(1):17-25.TANG Liangjie,JIN Zhijun,JIA Chengzao,et al. A large-scale saltnappe complex in the leading edge of the Kuqa foreland fold-thrustbelt,Tarim basin,northwest China[J]. Acta Geologica Sinica,2004,78(1):17-25.
[2]汤良杰,李京昌,余一欣,等.库车前陆褶皱-冲断带盐构造差异变形和分段性特征探讨[J].地质学报,2006,80(3):313-320.TANG Liangjie,LI Jingchang,YU Yixin,et al. Differential salt tec-tonic deformation and segmentation of the Kuqa foreland fold-thrustbelt,Tarim basin,northwest China[J]. Acta Geologica Sinica,2006,80(3):313-320.
[3]能源,漆家福,谢会文,等.塔里木盆地库车坳陷北部边缘构造特征[J].地质通报,2012,31(9):1 510-1 519.NENG Yuan,QI Jiafu,XIE Huiwen,et al. Structural characteristicsof northern margin of Kuqa depression,Tarim basin[J]. GeologcalBulletin of China,2012,31(9):1 510-1 519.
[4]汪新,王招明,谢会文,等.塔里木库车坳陷新生代盐构造解析及其变形模拟[J].中国科学:地球科学,2010,40(12):1 655-1 668.WANG Xin,WANG Zhaoming,XIE Huiwen,et al. Cenozoic salt tec-tonics and physical models in the Kuqa depression of Tarim basin,China[J]. Science China:Earth Sciences,2010,40(12):1 655-1 668.
[5]范小根,程晓敢,陈汉林,等.塔西南新生代前陆盆地东段盆山结构与冲断带变形特征[J].大地构造与成矿学,2015,39(2):241-249.FAN Xiaogen,CHENG Xiaogan,CHEN Hanlin,et al. Basin-rangecoupling structure and deformation features of the eastern Cenozoicforeland basin in SW Tarim[J]. Geotectonica et Metallogenia,2015,39(2):241-249.
[6]田继强,贾承造,段书府,等.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.TIAN Jiqiang,JIA Chengzao,DUAN Shufu,et al. Structural charac-teristics and physical modeling of Fusha-Keliyang segment of thewestern Kunlun thrust belt in southwestern Tarim basin[J]. ActaPetrolei Sinica,2012,33(6):941-948.
[7]谢会文,王春阳,王智斌,等.基底滑脱层分布对褶皱冲断带变形影响的物理模拟研究:以塔西南西昆仑山前褶皱冲断带为例[J].高校地质学报,2012,18(4):701-710.XlE Huiwen,WANG Chunyang,WANG Zhibin,et al. The effect ofspatial distribution of basement detachment on deformation in a foldand thrust belt:an analogue modeling approach an example of westKunlun fold-and-thrust belt[J]. Geological Journal of China Univer-sities,2012,18(4):701-710.
[8]龚艳萍,尹宏伟,汪新,等.西昆仑山前柯东构造带变形特征、机制及物理模拟[J].石油实验地质,2014,36(3):299-303.GONG Yanping,YIN Hongwei,WANG Xin,et al. Structural defor-mation characteristics,mechanics and physical modeling of Kedong structure in piedmont of western Kunlun mountain[J]. PetroleumGeology&Experiment,2014,36(3):299-303.
[9]徐振平,谢会文,李勇,等.库车坳陷克拉苏构造带盐下差异构造变形特征及控制因素[J].天然气地球科学,2012,23(6):1 034-1 038.XU Zhenping,XIE Huiwen,LI Yong,et al. Characteristics and con-trolling factors of the subsalt differential structure in the Kelasustructural belt,Kuqa depression[J]. Natural Gas Geoscience,2012,23(6):1 034-1 038.
[10]张玮,漆家福,雷刚林,等.塔西南坳陷西昆仑山前冲断带的收缩构造变形模式[J].新疆石油地质,2010,31(6):567-571.ZHANG Wei,QI Jiafu,LEI Ganglin,et al. Deformation model ofcontraction structure of west Kunlun piedmont thrust belt in south-western depression of Tarim basin[J]. Xinjiang Petroleum Geolo-gy,2010,31(6):567-571.
[11]汪新,贾承造,杨树锋,等.南天山库车冲断褶皱带构造变形时间——以库车河地区为例[J].地质学报,2002,76(1):55-63.WANG Xin,JIA Chengzao,YANG Shufeng,et al. The time of de-formation on the Kuqa fold-and-thrust belt in the southern Tian-shan-based on the Kuqa river area[J]. Acta Geologica Sinica,2002,76(1):55-63.
[12]汪新,贾承造,杨树锋.南天山库车褶皱冲断带构造几何学和运动学[J].地质科学,2002,37(3):372-384.WANG Xin,JIA Chengzao,YANG Shufeng. Geometry and kine-matics of the Kuqa fold-and-thrust belt in the southern Tianshan[J]. Chinese Journal of Geology,2002,37(3):372-384.
[13]刘玉萍,尹宏伟,张洁,等.褶皱—冲断体系双层滑脱构造变形物理模拟实验[J].石油实验地质,2008,30(4):424-428.LIU Yuping,YIN Hongwei,ZHANG Jie,et al. Physical modelingon double decollements structure in fold-and-thrust belt[J]. Petro-leum Geology&Experiment,2008,30(4):424-428.
[14]何登发,李德生,何金有,等.塔里木盆地库车坳陷和西南坳陷油气地质特征类比及勘探启示[J].石油学报,2013,34(2):201-218.HE Dengfa,LI Desheng,HE Jinyou,et al. Comparison in petro-leum geology between Kuqa depression and southwest depressionin Tarim basin and its exploration significance[J]. Acta Petrolei Si-nica,2013,34(2):201-218.
[15]杨海军,李曰俊,李勇,等.塔里木盆地南部玛东早古生代褶皱-冲断带[J].岩石学报,2016,32(3):815-824.YANG Haijun,LI Yuejun,LI Yong,et al. Madong Early Paleozoicfold-thrust belt in the southern Tarim basin[J]. Acta Petrologica Si-nica,2016,32(3):815-824.
[16]谢会文,尹宏伟,唐雁刚,等.基于面积深度法对克拉苏构造带中部盐下构造的研究[J].大地构造与成矿学,2015,39(6):1 033-1 040.XIE Huiwen,YIN Hongwei,TANG Yangang,et al. Research onsubsalt structure in the central Kelasu structure belt based on thearea-depth technique[J]. Geotectonica et Metallogenia,2015,39(6):1 033-1 040.
[17] WANG Wei,YIN Hongwei,JIA Dong,et al. A sub-salt structuralmodel of the Kelasu structure in the Kuqa foreland basin,north-west China[J]. Marine and Petroleum Geology,2017,88:115-126.
[18]何娟,王毅,刘士林,等.塔里木盆地西南坳陷东部构造特征及对油气成藏的控制[J].石油实验地质,2016,38(3):326-332.HE Juan,WANG Yi,LIU Shilin,et al. Characteristics of faultstructure and its control on hydrocarbon accumulation in the east-ern part of southwestern Tarim basin[J]. Petroleum Geology&Experiment,2016,38(3):326-332.
[19]卢华复,贾承造,贾东,等.库车再生前陆盆地冲断构造楔特征[J].高校地质学报,2001,7(3):257-271.LU Huafu,JIA Chengzhao,JIA Dong,et al. Features of the thrustwedge of deformation belt in Kuqa rejuvenation foreland basin[J].Geological Journal of China Universities,2001,7(3):257-271.
[20]文磊,杨海军,李曰俊,等.天山南麓库车晚新生代褶皱-冲断带[J].岩石学报,2016,32(3):847-855.WEN Lei,YANG Haijun,LI Yuejun,et al. Kuqa Late Cenozoic fold-thrust belt in the southern flank of Tianshan mountains[J]. ActaPetrologica Sinica,2016,32(3):847-855.
[21]郭颖,汤良杰,余腾孝,等.塔里木盆地塘古巴斯坳陷玛东构造带断裂特征及成因探讨[J].大地构造与成矿学,2016,40(4):643-653.GUO Ying,TANG Liangjie,YU Tengxiao,et al. Fault features andformation mechanism of Madong structural belt in Tanggubasi de-pression,Tarim basin[J]. Geotectonica et Metallogenia,2016,40(4):643-653.
[22]李浩武,王建君,邬光辉,等.塔里木盆地塘古孜巴斯坳陷西部中加里东期断裂特征及形成机制[J].中南大学学报(自然科学版),2014,45(12):4 331-4 341.LI Haowu,WANG Jianjun,WU Guanghui,et al. Features and for-mation mechanism of middle Caledonian faults in west of Tangguzi-basi depression,Tarim basin[J]. Journal of Central South Universi-ty(Science and Technology),2014,45(12):4 331-4 341.
[23]李浩武,邬光辉,史玲玲,等.塔里木盆地西部玛东冲断带构造特征与形成演化[J].新疆地质,2013,31(3):180-185.LI Haowu,WU Guanghui,SHI Lingling,et al. The structural fea-tures and evolution series of Madong thrust belt,west of Tarim ba-sin[J]. Xinjiang Geology,2013,31(3):180-185.
[24] YIN A,NIE S,CRAIG P,et al. Late Cenozoic tectonic evolution ofthe southern Chinese Tian Shan[J]. Tectonics,1998,17(1):1-27.
[25] SUN Jimin,LIU Tungsheng. The age of the Taklimaken desert[J].Science,2006,312(5 780):1 621.
[26]周路,张欣吉,钟克修,等.四川盆地东部五百梯地区构造变形特征[J].新疆石油地质,2018,39(3):251-256.ZHOU Lu,ZHANG Xinji,ZHONG Kexiu,et al. Structure deforma-tion characteristics of Wubaiti area in the eastern Sichuan basin[J]. Xinjiang Petroleum Geology,2018,39(3):251-256.
[27] WU Zhenyun,YIN Hongwei,WANG Xin,et al. Characteristics anddeformation mechanism of salt-related structures in the westernKuqa depression,Tarim basin:insights from scaled sandbox model-ing[J]. Tectonophysics,2014,612-613:81-96.
[28] SUN Chuang,JIA Dong,YIN Hongwei,et al. Sandbox modeling ofevolving thrust wedges with different preexisting topographic relief:implications for the Longmen Shan thrust belt,eastern Tibet[J]. Jour-nal of Geophysical Research-Solid Earth,2016,121:4 591-4 614.
[29]王步青,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. Decollementstructure of southwest Tarim depression and its periphery[J]. Chi-nese Journal of Geology,2011,46(3):733-742.
[30]解国爱,贾东,张庆龙,等.川东侏罗山式褶皱构造带的物理模拟研究[J].地质学报,2013,87(6):773-788.XIE Guoai,JIA Dong,ZHANG Qinglong,et al. Physical modelingof the Jura-type folds in eastern Sichuan[J]. Acta Geologica Sini-ca,2013,87(6):773-778.
[2]汤良杰,李京昌,余一欣,等.库车前陆褶皱-冲断带盐构造差异变形和分段性特征探讨[J].地质学报,2006,80(3):313-320.TANG Liangjie,LI Jingchang,YU Yixin,et al. Differential salt tec-tonic deformation and segmentation of the Kuqa foreland fold-thrustbelt,Tarim basin,northwest China[J]. Acta Geologica Sinica,2006,80(3):313-320.
[3]能源,漆家福,谢会文,等.塔里木盆地库车坳陷北部边缘构造特征[J].地质通报,2012,31(9):1 510-1 519.NENG Yuan,QI Jiafu,XIE Huiwen,et al. Structural characteristicsof northern margin of Kuqa depression,Tarim basin[J]. GeologcalBulletin of China,2012,31(9):1 510-1 519.
[4]汪新,王招明,谢会文,等.塔里木库车坳陷新生代盐构造解析及其变形模拟[J].中国科学:地球科学,2010,40(12):1 655-1 668.WANG Xin,WANG Zhaoming,XIE Huiwen,et al. Cenozoic salt tec-tonics and physical models in the Kuqa depression of Tarim basin,China[J]. Science China:Earth Sciences,2010,40(12):1 655-1 668.
[5]范小根,程晓敢,陈汉林,等.塔西南新生代前陆盆地东段盆山结构与冲断带变形特征[J].大地构造与成矿学,2015,39(2):241-249.FAN Xiaogen,CHENG Xiaogan,CHEN Hanlin,et al. Basin-rangecoupling structure and deformation features of the eastern Cenozoicforeland basin in SW Tarim[J]. Geotectonica et Metallogenia,2015,39(2):241-249.
[6]田继强,贾承造,段书府,等.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.TIAN Jiqiang,JIA Chengzao,DUAN Shufu,et al. Structural charac-teristics and physical modeling of Fusha-Keliyang segment of thewestern Kunlun thrust belt in southwestern Tarim basin[J]. ActaPetrolei Sinica,2012,33(6):941-948.
[7]谢会文,王春阳,王智斌,等.基底滑脱层分布对褶皱冲断带变形影响的物理模拟研究:以塔西南西昆仑山前褶皱冲断带为例[J].高校地质学报,2012,18(4):701-710.XlE Huiwen,WANG Chunyang,WANG Zhibin,et al. The effect ofspatial distribution of basement detachment on deformation in a foldand thrust belt:an analogue modeling approach an example of westKunlun fold-and-thrust belt[J]. Geological Journal of China Univer-sities,2012,18(4):701-710.
[8]龚艳萍,尹宏伟,汪新,等.西昆仑山前柯东构造带变形特征、机制及物理模拟[J].石油实验地质,2014,36(3):299-303.GONG Yanping,YIN Hongwei,WANG Xin,et al. Structural defor-mation characteristics,mechanics and physical modeling of Kedong structure in piedmont of western Kunlun mountain[J]. PetroleumGeology&Experiment,2014,36(3):299-303.
[9]徐振平,谢会文,李勇,等.库车坳陷克拉苏构造带盐下差异构造变形特征及控制因素[J].天然气地球科学,2012,23(6):1 034-1 038.XU Zhenping,XIE Huiwen,LI Yong,et al. Characteristics and con-trolling factors of the subsalt differential structure in the Kelasustructural belt,Kuqa depression[J]. Natural Gas Geoscience,2012,23(6):1 034-1 038.
[10]张玮,漆家福,雷刚林,等.塔西南坳陷西昆仑山前冲断带的收缩构造变形模式[J].新疆石油地质,2010,31(6):567-571.ZHANG Wei,QI Jiafu,LEI Ganglin,et al. Deformation model ofcontraction structure of west Kunlun piedmont thrust belt in south-western depression of Tarim basin[J]. Xinjiang Petroleum Geolo-gy,2010,31(6):567-571.
[11]汪新,贾承造,杨树锋,等.南天山库车冲断褶皱带构造变形时间——以库车河地区为例[J].地质学报,2002,76(1):55-63.WANG Xin,JIA Chengzao,YANG Shufeng,et al. The time of de-formation on the Kuqa fold-and-thrust belt in the southern Tian-shan-based on the Kuqa river area[J]. Acta Geologica Sinica,2002,76(1):55-63.
[12]汪新,贾承造,杨树锋.南天山库车褶皱冲断带构造几何学和运动学[J].地质科学,2002,37(3):372-384.WANG Xin,JIA Chengzao,YANG Shufeng. Geometry and kine-matics of the Kuqa fold-and-thrust belt in the southern Tianshan[J]. Chinese Journal of Geology,2002,37(3):372-384.
[13]刘玉萍,尹宏伟,张洁,等.褶皱—冲断体系双层滑脱构造变形物理模拟实验[J].石油实验地质,2008,30(4):424-428.LIU Yuping,YIN Hongwei,ZHANG Jie,et al. Physical modelingon double decollements structure in fold-and-thrust belt[J]. Petro-leum Geology&Experiment,2008,30(4):424-428.
[14]何登发,李德生,何金有,等.塔里木盆地库车坳陷和西南坳陷油气地质特征类比及勘探启示[J].石油学报,2013,34(2):201-218.HE Dengfa,LI Desheng,HE Jinyou,et al. Comparison in petro-leum geology between Kuqa depression and southwest depressionin Tarim basin and its exploration significance[J]. Acta Petrolei Si-nica,2013,34(2):201-218.
[15]杨海军,李曰俊,李勇,等.塔里木盆地南部玛东早古生代褶皱-冲断带[J].岩石学报,2016,32(3):815-824.YANG Haijun,LI Yuejun,LI Yong,et al. Madong Early Paleozoicfold-thrust belt in the southern Tarim basin[J]. Acta Petrologica Si-nica,2016,32(3):815-824.
[16]谢会文,尹宏伟,唐雁刚,等.基于面积深度法对克拉苏构造带中部盐下构造的研究[J].大地构造与成矿学,2015,39(6):1 033-1 040.XIE Huiwen,YIN Hongwei,TANG Yangang,et al. Research onsubsalt structure in the central Kelasu structure belt based on thearea-depth technique[J]. Geotectonica et Metallogenia,2015,39(6):1 033-1 040.
[17] WANG Wei,YIN Hongwei,JIA Dong,et al. A sub-salt structuralmodel of the Kelasu structure in the Kuqa foreland basin,north-west China[J]. Marine and Petroleum Geology,2017,88:115-126.
[18]何娟,王毅,刘士林,等.塔里木盆地西南坳陷东部构造特征及对油气成藏的控制[J].石油实验地质,2016,38(3):326-332.HE Juan,WANG Yi,LIU Shilin,et al. Characteristics of faultstructure and its control on hydrocarbon accumulation in the east-ern part of southwestern Tarim basin[J]. Petroleum Geology&Experiment,2016,38(3):326-332.
[19]卢华复,贾承造,贾东,等.库车再生前陆盆地冲断构造楔特征[J].高校地质学报,2001,7(3):257-271.LU Huafu,JIA Chengzhao,JIA Dong,et al. Features of the thrustwedge of deformation belt in Kuqa rejuvenation foreland basin[J].Geological Journal of China Universities,2001,7(3):257-271.
[20]文磊,杨海军,李曰俊,等.天山南麓库车晚新生代褶皱-冲断带[J].岩石学报,2016,32(3):847-855.WEN Lei,YANG Haijun,LI Yuejun,et al. Kuqa Late Cenozoic fold-thrust belt in the southern flank of Tianshan mountains[J]. ActaPetrologica Sinica,2016,32(3):847-855.
[21]郭颖,汤良杰,余腾孝,等.塔里木盆地塘古巴斯坳陷玛东构造带断裂特征及成因探讨[J].大地构造与成矿学,2016,40(4):643-653.GUO Ying,TANG Liangjie,YU Tengxiao,et al. Fault features andformation mechanism of Madong structural belt in Tanggubasi de-pression,Tarim basin[J]. Geotectonica et Metallogenia,2016,40(4):643-653.
[22]李浩武,王建君,邬光辉,等.塔里木盆地塘古孜巴斯坳陷西部中加里东期断裂特征及形成机制[J].中南大学学报(自然科学版),2014,45(12):4 331-4 341.LI Haowu,WANG Jianjun,WU Guanghui,et al. Features and for-mation mechanism of middle Caledonian faults in west of Tangguzi-basi depression,Tarim basin[J]. Journal of Central South Universi-ty(Science and Technology),2014,45(12):4 331-4 341.
[23]李浩武,邬光辉,史玲玲,等.塔里木盆地西部玛东冲断带构造特征与形成演化[J].新疆地质,2013,31(3):180-185.LI Haowu,WU Guanghui,SHI Lingling,et al. The structural fea-tures and evolution series of Madong thrust belt,west of Tarim ba-sin[J]. Xinjiang Geology,2013,31(3):180-185.
[24] YIN A,NIE S,CRAIG P,et al. Late Cenozoic tectonic evolution ofthe southern Chinese Tian Shan[J]. Tectonics,1998,17(1):1-27.
[25] SUN Jimin,LIU Tungsheng. The age of the Taklimaken desert[J].Science,2006,312(5 780):1 621.
[26]周路,张欣吉,钟克修,等.四川盆地东部五百梯地区构造变形特征[J].新疆石油地质,2018,39(3):251-256.ZHOU Lu,ZHANG Xinji,ZHONG Kexiu,et al. Structure deforma-tion characteristics of Wubaiti area in the eastern Sichuan basin[J]. Xinjiang Petroleum Geology,2018,39(3):251-256.
[27] WU Zhenyun,YIN Hongwei,WANG Xin,et al. Characteristics anddeformation mechanism of salt-related structures in the westernKuqa depression,Tarim basin:insights from scaled sandbox model-ing[J]. Tectonophysics,2014,612-613:81-96.
[28] SUN Chuang,JIA Dong,YIN Hongwei,et al. Sandbox modeling ofevolving thrust wedges with different preexisting topographic relief:implications for the Longmen Shan thrust belt,eastern Tibet[J]. Jour-nal of Geophysical Research-Solid Earth,2016,121:4 591-4 614.
[29]王步青,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. Decollementstructure of southwest Tarim depression and its periphery[J]. Chi-nese Journal of Geology,2011,46(3):733-742.
[30]解国爱,贾东,张庆龙,等.川东侏罗山式褶皱构造带的物理模拟研究[J].地质学报,2013,87(6):773-788.XIE Guoai,JIA Dong,ZHANG Qinglong,et al. Physical modelingof the Jura-type folds in eastern Sichuan[J]. Acta Geologica Sini-ca,2013,87(6):773-778.