Structural deformation and origin of the arcuate fold-thrust belt in western Hubei Province
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摘要: 对川东—湘鄂西断褶带内鄂西地区的弧形构造,从构造剖面特征、叠加褶皱样式和断裂性质入手进行几何学和运动学分析。结果发现鄂西弧形构造具有多期变形特征:早期普遍为北东东向的直线型褶皱,随着弧形带扩展,在东、西两翼分别发育右行和左行的逆冲—走滑断裂,同时分别形成北北东向和北西西向的弧形褶皱。晚期弧形带中部发育北北东向构造并叠加改造了早期北东东和北西西向褶皱,同时在黄陵背斜以西还发育交切早期构造的北北西向仙女山右行走滑断裂。根据弧形带扩展的几何学—运动学分类原则,并结合前人的古地磁研究结果,推测鄂西弧形构造应属于构造弯曲形成的弯曲弧。区域滑脱层和黄陵隆起阻挡可能是控制弧形样式的主要原因。区域滑脱层控制了拆离滑脱褶皱的构造样式; 黄陵基底隆起的阻挡作用使弧形带东翼进一步弯曲变形,并导致了构造应力场方向发生改变,造成了晚期北北东向与早期北东东向构造的叠加。由此恢复的鄂西弧形构造变形过程对于揭示川东—湘鄂西断褶带构造演化具有重要的指示意义。Abstract: In northern Yangtze area,there are two Mesozoic arcuate fold-thrust belts,the southern Daba fold-thrust belt and the eastern Sichuan-Western Hubei fold-thrust belt.The origin of the southern Daba was due to the large arc-shape indentor(northern Daba divided by Chengkou-Fangxian thrust fault)and two basement uplift(Micangshan and Shennongjia),but the origin of the eastern Sichuan-Western Hubei fold-thrust belt was not well understood.Based on the cross sections and field mapping,this paper analyzed the geometry and kinematics of the folds and faults in western Hubei province.We found that the fold-thrust belt was characterized by multi-phase deformation.The early phase deformation was dominant by straight fold trending NEE.During the propagation of fold-thrust belt,the eastern and western limbs were developed with curved folds trending NNE and NWW,respectively.The strike-slip faults with opposite slip direction were also formed in the two limbs.The late phase deformation was concentrated in the central fold-thrust belt,characterized by NNE-trending fold and NNW-trending strike-slip fault.The NNE-trending folds superposed on the NEE-trending folds,while the NNW-trending fault cut across the NWW curved in the eastern limb.The two-phase deformation suggested the varied structural stress field controlled by different factors.We conclude that the arcuate fold-thrust belt is orocline with vertical-axis rotation in western Hubei Province.The early phase deformation was controlled by detachment horizons.The late phase deformation was controlled by Huangling basement uplift,which held the propagation of eastern limb of the fold-thrust belt and intensified the curved deformation.
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[1] 陈海泓,孙 枢,李继亮,王清晨,彭海波,徐树桐,许靖华.1993.雪峰山大地构造的基本特征初探.地质科学, 28 (3): 201-210.
[2] Chen Haihong, Sun Shu, Li Jiliang, Wang Qingchen, Peng Haibo, Xu Shutong and Hsü K J.1993.A preliminary study on tectonics of the Xuefeng Mountains,western Hunan.Chinese Journal of Geology(Scientia Geologica Sinica), 28 (3): 201-210.
[3] 董云鹏,查显峰,付明庆,张 茜,杨 钊,张 燕.2008.秦岭南缘大巴山褶皱-冲断推覆构造的特征.地质通报, 27 (9): 1493-1508.
[4] Dong Yunpeng,Zha Xianfeng,Fu Mingqing,Zhang Qian,Yang Zhao and Zhang Yan.2008.Characteristics of the Dabashan fold-thrust nappe structure at the southern margin of the Qinling,China.Geological Bulletin of China, 27 (9): 1493-1508.
[5] 郭正吾,邓康龄,韩永辉.1996.四川盆地形成与演化.北京:地质出版社.1-200.
[6] Guo Zhengwu,Deng Kangling and Han Yonghui.1996.The Formation and Development of Sichuan Basin.Beijing:Geological Publishing House.1-200.
[7] 韩玉林,许长海,周祖翼,谈晓冬.2009.扬子褶皱带侏罗纪砂岩古地磁及其褶皱带弧形弯曲的成因.地球物理学报, 52 (12): 3072-3082.
[8] Han Yulin,Xu Changhai,Zhou Zuyi and Tan Xiaodong.2009.Paleomagnetism of Jurassic sandstones from Yangtze fold belt and its implications for the fold belt curvature.Chinese Journal of Geophysics, 52 (12): 3072-3082.
[9] 胡召齐,朱 光,刘国生,张必龙.2009.川东"侏罗山式"褶皱带形成时代:不整合面的证据.地质论评, 55 (1): 32-42.
[10] Hu Shaoqi,Zhu Guang,Liu Guosheng and Zhang Bilong.2009.The folding time of the eastern Sichuan Jura-type fold belt:Evidence from unconformity.Geological Review, 55 (1): 32-42.
[11] 胡召齐,朱 光,张必龙,陈 印,魏 鑫,张 力.2010.上扬子北部褶皱带的构造应力场演化规律.地质科学, 45 (2): 361-379.
[12] Hu Zhaoqi,Zhu Guang,Zhang Bilong,Chen Yin,Wei Xin and Zhang Li.2010.Tectonic stress field evolution in fold belts in the northern upper Yangtze region.Chinese Journal of Geology, 45 (2): 361-379.
[13] 李岩峰,曲国胜,张 进.2007.弧形构造研究进展.地球科学进展, 22 (7): 708-715.
[14] Li Yanfeng,Qu Guosheng and Zhang Jin.2007.Developments in research of arcuate structure.Advances in Earth Science, 22 (7): 708-715.
[15] 李正祥,Mca Powell C,方大钧,楼 刚.1996.华南中生代以来弯山构造的发育和地块相对旋转--地质和古地磁证据.科学通报, 41 (5): 446-450.
[16] Li Zhengxiang,Mca Powell C,Fang Dajun and Lou Gang.1996.Since the Mesozoic tectonic development of mountain land and the relative rotation in southern China:Evidence of geological and paleomagnetic.Chinese Science Bulletin, 41 (5): 446-450.
[17] 刘少峰,王 平,胡明卿,郜瑭郡,王 凯.2010.中、上扬子北部盆-山系统演化与动力学机制.地学前缘, 17 (3): 14-26.
[18] Liu Shaofeng,Wang Ping,Hu Mingqing,Gao Tangjun and Wang Kai.2010.Evolution and geodynamic mechanism of basin-mountain systems in the northern margin of the middle-upper Yangtze.Earth Science Frontiers, 17 (3): 14-26.
[19] 刘海军,许长海,周祖翼,Donelick R A.2009.黄陵隆起形成(165-100 Ma)的碎屑岩磷灰石裂变径迹热年代学约束.自然科学进展, 19 (12):1326-1332.
[20] Liu Haijun,Xu Changhai,Zhou Zuyi and Donelick R A.2009.Thermochronology constraints of clastic apatite fission track of Huangling uplift.Progress in Natural Science, 19 (12):1326-1332.
[21] 梅廉夫,刘昭茜,汤济广,沈传波,凡元芳.2010.湘鄂西-川东中生代陆内递进扩展变形:来自裂变径迹和平衡剖面 的证据.地球科学, 35 (2): 161-174.
[22] Mei Lianfu,Liu Zhaoqian,Tang Jiguang,Shen Chuanbo and Fan Yuanfang.2010.Mesozoic intra-continental progressive deformation in western Hunan-Hubei-eastern Sichuan Provinces of China:Evidence from apatite fission track and balanced cross-section.Earth Science, 35 (2): 161-174.
[23] 曲国胜,Joseph Canerot,王宗起,赵 民.1996.造山带弧形构造--西昆仑-帕米尔弧及其预测.地质科学, 31 (4): 313-326.
[24] Qu Guosheng,Joseph Canerot,Wang Zongqi and Zhao Min.1996.Arc tectonics in orogenic belts.Chinese Journal of Geology(Scientia Geologica Sinica), 31 (4): 313-326.
[25] 孙 岩,刘德良,朱文斌,郭继春,李本亮,郭 建,王 锋,赵忠岩.2005.上扬子地壳区域性地层岩石物性力学参数与滑动层位关系研究.地质科学, 40 (4): 532-538.
[26] Sun Yan,Liu Deliang,Zhu Wenbin,Guo Jichun,Li Benliang,Guo Jian,Wang Feng and Zhao Zhongyan.2005.Study on relationship between rock physico-mechanic parameters and slipping layers of regional strata in the upper Yangtze crust.Chinese Journal of Geology, 40 (4): 532-538.
[27] 许长海,周祖翼,常 远,Guillot François.2010.大巴山弧形构造带形成与两侧隆起的关系:FT 和(U-Th)/He 低温热年代约束.中国科学(地球科学), 40 (12): 1684-1696.
[28] Xu Changhai,Zhou Zuyi,Chang Yuan and Guillot François.2010.Genesis of Daba arcuate structural belt related to adjacent base-ment upheavals:Constraints from fission-track and(U-Th)/He thermochronology.Science China(Earth Sciences), 53 (11): 1634-1646.
[29] 颜丹平,金哲龙,张维宸,刘少峰.2008.川渝湘鄂薄皮构造带多层拆离滑脱系的岩石力学性质及其对构造变形样式的控制.地质通报, 27 (10):1687-1697.
[30] Yan Danping, Jin Zhelong, Zhang Weichen and Liu Shaofeng. 2008. Rock mechanical characteristics of the multi-layer detachment fault system and their controls on the structural deformation style of the Sichuan-Chongqing-Human-Hubei thin-skinned belt, South China. Geological Bulletin of China, 27 (10):1687-1697.
[31] 杨振宇,Jean B.2000.四川盆地南缘早三叠世古地磁结果及其构造意义.地质科学, 35 (1): 77-82.
[32] Yang Zhenyu and Jean B.2000.Early Triassic paleomagnetic results from southern part of the Sichuan Basin and its tectonic implications.Chinese Journal of Geology(Scientia Geologica Sinica), 35 (1): 77-82.
[33] 张岳桥,施 炜,李建华,王瑞瑞,李海龙,董树文.2010.大巴山前陆弧形构造带形成机理分析.地质学报, 84 (9): 1300-1315.
[34] Zhang Yueqiao,Shi Wei,Li Jianhua,Wang Ruirui,Li Hailong and Dong Shuwen.2010.Formation mechanism of the Dabashan foreland arc-shaped structural belt.Acta Geologica Sinica, 84 (9): 1300-1315.
[35] 张 辉,谈晓冬,韩玉林.2007.白垩纪同褶皱重磁化组分揭示中扬子褶皱带构造旋转过程.科学通报, 52 (17): 2049-2056.
[36] Zhang Hui,Tan Xiaodong and Han Yulin.2007.Cretaceous synfolding remagnetization components revealing tectonic rotation of the middle Yangtze fold belt.Chinese Science Bulletin, 52 (20): 2837-2846.
[37] Carey S W.1955.The orocline concept in geotectonics,part Ⅰ.In:Papers and Proceedings of the Royal Society of Tasmania,v.89.255-288.
[38] Eldredge S,Bachtadse V and Van Der Voo R.1985.Paleomagnetism and the orocline hypothesis.Tectonophysics, 119 (1-4): 153-179.
[39] Ghosh S K,Mandal N,Khan D and Deb S K.1992.Modes of superposed buckling in single layers controlled by initial tightness of early folds.Journal of Structural Geology, 14 (4): 381-394.
[40] Hindle D and Burkhard M.1999.Strain,displacement and rotation associated with the formation of curvature in fold belts; the example of the Jura arc.Journal of Structural Geology, 21 (8-9): 1089-1101.
[41] Hu S B,Raza A,Min K,Kohn B P,Reiners P W,Ketcham R A,Wang J and Gleadow A J W.2006.Late Mesozoic and Cenozoic thermotectonic evolution along a transect from the North China Craton through the Qinling orogen into the Yangtze Craton,central China.Tectonics, 25 :C60096,doi:10.1029/2006TC001985.
[42] Huang K and Opdyke N D.1997.Middle Triassic paleomagnetic results from central Hubei Province,China and their tectonic implications.Geophysical Research Letters, 24 (13): 1571-1574.
[43] Liu S F,Steel R and Zhang G W.2005.Mesozoic sedimentary basin development and tectonic implication,northern Yangtze Block,eastern China:Record of continent-continent collision.Journal of Asian Earth Sciences, 25 (1): 9-27.
[44] Macedo J and Marshak S.1999.Controls on the geometry of fold-thrust belt salients.GSA Bulletin, 111 (12):1808-1822.
[45] Ramsay J G.1967.Folding and Fracturing of Rocks.New York:McGraw-Hill.1-568.
[46] Simón J L.2004.Superposed buckle folding in the eastern Iberian Chain,Spain.Journal of Structural Geology, 26 (8): 1447-1464.
[47] Sussman A J,Butler R F,Dinarès-Turell and Vergés J.2004.Vertical-axis rotation of a foreland fold and implications for orogenic curvature:An example from the southern Pyrenees,Spain.Earth and Planetary Science Letters, 218 (3-4): 435-449.
[48] Schwartz S Y and Van der Voo R.1984.Paleomagnetic study of thrust sheet rotation during foreland impingement in the Wyoming-Idaho overthrust belt.Journal of Geophysical Research, 89 (B12): 10077-10086.
[49] Tan X D,Kodama K P,Gilder S,Courtillot V and Cogne J P.2007.Palaeomagnetic evidence and tectonic origin of clockwise rotations in the Yangtze fold belt,South China Block.Geophysical Journal International, 168 (1): 48-58.
[50] Weil A B and Sussman A J.2004.Classifying curved orogens based on timing relationships between structural development and vertical-axis rotations.GSA Special Papers, 383 : 1-15.
[51] Yan D P,Zhou M F,Song H L,Wang X W and Malpas J.2003.Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze block(south China).Tectonophysics, 361 (3-4): 239-254.
[52] Yang Z Y and Besse J.2001.New mesozoic apparent polar wander path for south China:Tectonic consequences.Journal of Geophysical Research, 106 (B5): 8493-8520.
[53] Yonkee A and Weil A B.2010.Reconstructing the kinematic evolution of curved mountain belts:Internal strain patterns in the Wyoming salient,Sevier thrust belt,U.S.A.GSA Bulletin, 122 (1-2): 24-49.
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