川滇地块西部差异性旋转的构造意义:青藏高原东南缘白垩纪红层古地磁学新证据
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摘要
印度—欧亚板块碰撞以来青藏高原内部及其周缘地区经历了复杂的构造演化,复杂构造变形区的复合构造使得古地磁的数据解释究竟代表区域的构造旋转还是只能反映局部的构造变形一直是备受关注的问题.本文通过采集川滇地块西缘渔泡江断裂东侧三岔河地区白垩纪红层古地磁样品,揭示采样区差异性旋转并探讨川滇地块西部自中新世以来的构造演化规律.前人的地质调查表明川滇地块渔泡江断裂东侧上白垩统赵家店组地层发育倾伏褶皱.三岔河剖面以三岔河镇为界分为南北两段,三岔河南段剖面高温剩磁分量平均方向在倾斜校正后Ds=29.3°,Is=45.7°,ks=54.3,α95=6.6°,倾伏地层产状校正后Ds=30.6°,Is=46.6°,ks=69.3,α95=5.8°;而三岔河北侧剖面高温剩磁分量平均方向在倾斜校正后Ds=350.4°,Is=42.1°,ks=69.4,α95=9.2°,倾伏地层产状校正后Ds=347.4°,Is=41.9°,ks=96.6,α95=7.8°;两组高温剩磁分量均通过了褶皱检验,表明其获得于褶皱形成之前.相对于东亚稳定区80Ma古地磁极,三岔河南侧剖面发生了20.5°±4.8°的顺时针构造旋转量,与楚雄盆地核部之间不存在差异性旋转;但三岔河镇以北剖面却发生了22.7°±6.6°的逆时针旋转.综合分析川滇地块内部的古地磁数据表明自中新世以来川滇地块南部楚雄盆地经历了约20°的顺时针构造旋转,而三岔河镇北侧经历了约20°逆时针旋转.进一步分析表明三岔河北侧剖面相对于南侧剖面经历了约40°的逆时针旋转,可能由于研究区的滑脱构造导致岩石薄弱层拆离滑脱所引起.
The collision of India and Eurasia has produced significant crustal deformation in the Tibetan Plateau and its periphery.However its mechanism along faults in the southeastern margin of the plateau remains poorly understood.To address this issue,we carry out a palaeomagneticinvestigation of Cretaceous red beds in the Sanchahe area on the eastern Yupaojiang Fault in the western Sichuan-Yunnan Block in order to determine the range of rotation along the fault.The area is divided into two segments by Sanchahe town,and the bedding attitudes are defined by two plunging fold axes.The mean direction of the High Temperature Component(HTC)from the southern segment of the Sanchahe area is Ds=29.3°,Is=45.7°,ks= 54.3,α95=6.6°after tilt correction,and Ds=30.6°,Is=46.6°,κ=69.3,α95=5.8°after tilt correction using an inclined fold axis.The HTC direction for the northern segment is Ds=350.4°,Is=42.1°,κ=69.4,α95=9.2°after tilt correction,and Ds=347.4°,Is=41.9°,ks= 96.6,α95=7.8°after tilt correction using an inclined fold axis.The southern segment experienced 20.5°±4.8°of clockwise rotation,whereas the northern segment experienced 22.7°±6.6°of anticlockwise rotation with respect to East Asia.Compared with previous palaeomagnetic results in this area,our results suggest that the Sichuan-Yunnan Block experienced ～20°of clockwise rotation,and ～20°of anticlockwise rotation in the northern segment of the Sanchahe area relative to the South China Block.This indicates a ～40°range of anticlockwise rotation in the northern segment of the Sanchahe area relative to the southern segment of the Sanchahe area,and that intense local deformation occurred along the Yupaojiang Fault which induced the formation of detachments in the upper crust.
The collision of India and Eurasia has produced significant crustal deformation in the Tibetan Plateau and its periphery.However its mechanism along faults in the southeastern margin of the plateau remains poorly understood.To address this issue,we carry out a palaeomagneticinvestigation of Cretaceous red beds in the Sanchahe area on the eastern Yupaojiang Fault in the western Sichuan-Yunnan Block in order to determine the range of rotation along the fault.The area is divided into two segments by Sanchahe town,and the bedding attitudes are defined by two plunging fold axes.The mean direction of the High Temperature Component(HTC)from the southern segment of the Sanchahe area is Ds=29.3°,Is=45.7°,ks= 54.3,α95=6.6°after tilt correction,and Ds=30.6°,Is=46.6°,κ=69.3,α95=5.8°after tilt correction using an inclined fold axis.The HTC direction for the northern segment is Ds=350.4°,Is=42.1°,κ=69.4,α95=9.2°after tilt correction,and Ds=347.4°,Is=41.9°,ks= 96.6,α95=7.8°after tilt correction using an inclined fold axis.The southern segment experienced 20.5°±4.8°of clockwise rotation,whereas the northern segment experienced 22.7°±6.6°of anticlockwise rotation with respect to East Asia.Compared with previous palaeomagnetic results in this area,our results suggest that the Sichuan-Yunnan Block experienced ～20°of clockwise rotation,and ～20°of anticlockwise rotation in the northern segment of the Sanchahe area relative to the South China Block.This indicates a ～40°range of anticlockwise rotation in the northern segment of the Sanchahe area relative to the southern segment of the Sanchahe area,and that intense local deformation occurred along the Yupaojiang Fault which induced the formation of detachments in the upper crust.
引文
Akciz S,Burchfiel B C,Crowley J L,et al.2008.Geometry,kinematics,and regional significance of the Chong Shan shear zone,Eastern Himalayan Syntaxis,Yunnan,China.Geosphere,4(1):292-314.
Allen C R,Gillespie A R,Yuan H,et al.1984.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rates,and seismic hazard.Geological Society of America Bulletin,95(6):686-700.
Allen C R,Luo Z L,Qian H,et al.1991.Field study of a highly active fault zone:The Xianshuihe fault of southwestern China.Geological Society of America Bulletin,103(9):1178-1199.
Borradaile G J,Jackson M.2004.Anisotropy of magnetic susceptibility(AMS):magnetic petrofabrics of deformed rocks.Geological Society,London,Special Publications,238(1):299-360.
Bullard E,Everett J E,Smith A G.1965.The fit of the continents around the Atlantic.Philosophical Transactions of the Royal Society A:Mathematical,Physical&Engineering Sciences,258(1088):41-51.
Burchfiel B C,Wang E.2003.Northwest-trending,middle Cenozoic,left-lateral faults in southern Yunnan,China,and their tectonic significance.Journal of Structural Geology,25(5):781-792.
Burchfiel B C,Chen Z L.2013.Tectonics of the southeastern Tibetan Plateau and its adjacent foreland.Memoir of the Geological Society of America,210:1-164.
Cao S Y,Liu J L,Leiss B,et al.2012.Initiation of left-lateral deformation along the Ailao Shan-Red River shear zone:new microstructural,textural,and geochronological constraints from the Diancang Shan metamorphic massif,SW Yunnan,China.International Geology Review,54(3):348-367.
Chung S L,Lee T Y,Lo C H,et al.1997.Intraplate extension prior to continental extrusion along the Ailao Shan-Red River shear zone.Geology,25(4):311-314.
Chung S L,Searle M P,Yeh M W.2007.The age of the potassic alkaline igneous rocks along the Ailao Shan-Red River Shear Zone:Implications for the onset age of left-lateral shearing:Adiscussion.Journal of Geology,116(2):231-242.
CognéJ P.1987.TRM deviations in anisotropic assemblages of multidomain magnetite.Geophysical Journal International,91(3):1013-1023.
CognéJ P.2003.PaleoMac:A MacintoshTMapplication for treating paleomagnetic data and making plate reconstructions.Geochemistry,Geophysics,Geosystems,4(1):1007,doi:10.1029/2001GC000227.
CognéJ P.2013.Cenozoic Eurasia is not a single rigid plate:Paleomagnetic evidence.Comptes Rendus Geoscience,345(11-12):419-426.
CognéJ P,Besse J,Chen Y,et al.2013.A new Late Cretaceous to Present APWP for Asia and its implications for paleomagnetic shallow inclinations in Central Asia and Cenozoic Eurasian plate deformation.Geophysical Journal International,192(3):1000-1024.
Duan J Z,Tan X H.2000.The nature and feature of Cenozoic main strike-slip fault in the three-river area of west Yunnan.Yunnan Geology(in Chinese),19(1):8-23.
Duan J Z,Xue S R,Qian X G.2001.The Cenozoic geological tectonic framework and evolution in the three-river area of west Yunnan.Yunnan Geology(in Chinese),20(3):243-253.
Dubien J L,Warde W D.1979.A mathematical comparison of the members of an infinite family of agglomerative clustering algorithms.Canadian Journal of Statistics,7(1):29-38.
Evans M A,Lewchuk M T,Elmore R D.2003.Strain partitioning of deformation mechanisms in limestones:Examining the relationship of strain and anisotropy of magnetic susceptibility(AMS).Journal of Structural Geology,25(9):1525-1549.
Fan C,Wang G,Wang S F,et al.2006.Structural interpretation of extensional deformation along the Dali fault system,southeastern margin of the Tibetan Plateau.International Geology Review,48(4):287-310.
Finlay C C,Maus S,Beggan C D,et al.2010.International geomagnetic reference field:the eleventh generation.Geophysical Journal International,183(3):1216-1230.
Funahara S,Nishiwaki N,Miki M,et al.1992.Paleomagnetic study of Cretaceous rocks from the Yangtze block,central Yunnan,China:implications for the India-Asia collision.Earth&Planetary Science Letters,113(1-2):77-91.
Funahara S,Nishiwaki N,Murata F,et al.1993.Clockwise rotation of the Red River fault inferred from paleomagnetic study of Cretaceous rocks in the Shan-Thai-Malay block of Western Yunnan,China.Earth&Planetary Science Letters,117(1-2):29-42.
Geological Survey of Yunnan Province.1965.Regional geological survey report(Dayao)(in Chinese).
Geological Survey of Yunnan Province.1973.Regional geological survey report(Dali)(in Chinese).
Gilley L D,Harrison T M,Leloup P H,et al.2003.Direct dating of left-lateral deformation along the Red River shear zone,China and Vietnam.Journal of Geophysical Research:Solid Earth,108(B2):2127,doi:10.1029/2001JB001726.
Guillot S,Mahéo G,de Sigoyer J,et al.2008.Tethyan and Indian subduction viewed from the Himalayan high-to ultrahighpressure metamorphic rocks.Tectonophysics,451(1-4):225-241.
Harrison T M,Leloup P H,Ryerson F J,et al.1996.Diachronous initiation of transtension along the Ailao Shan-Red River shear zone,Yunnan and Vietnam.World&Regional Geology,1(8):208-226.
Hrouda F.2007.Magnetic susceptibility,anisotropy.∥Gubbins D,Herrero-Bervera E eds.Encyclopedia of Geomagnetism and Paleomagnetism.Netherlands:Springer.
Huang B C,Piper J D A,Peng S T,et al.2006.Magnetostratigraphic study of the Kuche Depression,Tarim Basin,and Cenozoic uplift of the Tian Shan Range,Western China.Earth&Planetary Science Letters,251(3-4):346-364.
Huang K N,Opdyke N D.1992.Paleomagnetism of Cretaceous to lower Tertiary rocks from southwestern Sichuan:a revisit.Earth&Planetary Science Letters,112(1-4):29-40.
Huang K N,Opdyke N D.1993.Paleomagnetic results from Cretaceous and Jurassic rocks of South and Southwest Yunnan:evidence for large clockwise rotations in the Indochina and ShanThai-Malay terranes.Earth&Planetary Science Letters,117(3-4):507-524.
Jelinek V.1981.Characterization of the magnetic fabric of rocks.Tectonophysics,79(3-4):T63-T67.
Jia D,Chen Z X,Luo L,et al.2007.Magnetic fabric and finite strain of fault-related folds:an example analysis of Minjiang thrust structure in western Sichuan province.Advances in Natural Science(in Chinese),17(2):188-195.
Johnson M R W.2002.Shortening budgets and the role of continental subduction during the India-Asia collision.EarthScience Reviews,59(1-4):101-123.
Kirschvink J L.1980.The least-squares line and plane and the analysis of palaeomagnetic data.Geophysical Journal International,62(3):699-718.
Leloup P H,Harrison T M,Ryerson F J,et al.1993.Structural,petrological and thermal evolution of a Tertiary ductile strikeslip shear zone,Diancang Shan,Yunnan.Journal of Geophysical Research:Solid Earth,98(B4):6715-6743.
Leloup P H,Lacassin R,Tapponnier P,et al.1995.The Ailao Shan-Red River shear zone(Yunnan,China),Tertiary transform boundary of Indochina.Tectonophysics,251(1-4):13-84.
Leloup P H,Arnaud N,Lacassin R,et al.2001.New constraints on the structure,thermochronology,and timing of the Ailao Shan-Red River shear zone,SE Asia.Journal of Geophysical Research:Solid Earth,106(B4):6683-6732.
Li G X.1994.A preliminary study of some thrust-nappe structures in Lanping basin.Yunnan Geology(in Chinese),13(2):203-215.
Li S H,Deng C L,Dong W,et al.2015.Magnetostratigraphy of the Xiaolongtan Formation bearing Lufengpithecus keiyuanensis in Yunnan,southwestern China:Constraint on the initiation time of the southern segment of the Xianshuihe-Xiaojiang fault.Tectonophysics,655:213-226.
Li S H,Huang B C,Zhu R X.2012.Paleomagnetic constraints on the tectonic rotation of the southeastern margin of the Tibetan Plateau.Chinese J.Geophys.(in Chinese),55(1):76-94,doi:10.6038/j.issn.0001-5733.2012.01.008.
Li Z Y,Huang B C,Zhang C X.2010.Characteristic of anisotropy of magnetic susceptibility(AMS)and its tectonic significance in typical Cretaceous section from Xixia basin,central China.Acta Petrologica Sinica(in Chinese),26(11):3418-3430.
Liu H F,Wang Z C,Xiong B X,et al.2000.Coupling analysis of Mesozoic-Cenozoic foreland basin and mountain system in central and western China.Earth Science Frontiers(in Chinese),7(3):55-72.
Liu J L,Tang Y,Tran M D,et al.2012.The nature of the Ailao Shan-Red River(ASRR)shear zone:Constraints from structural,microstructural and fabric analyses of metamorphic rocks from the Diancang Shan,Ailao Shan and Day Nui Con Voi massifs.Journal of Asian Earth Sciences,47:231-251.
Liu J L,Song Z J,Cao S Y,et al.2006.The dynamic setting and processes of tectonic and magmatic evolution of the oblique collision zone between Indian and Eurasian plates:Exemplified by the tectonic evolution of the Three River region,eastern Tibet.Acta Petrologica Sinica(in Chinese),22(4):775-786.
Lowrie W.1990.Identification of ferromagnetic minerals in a rock by coercivity and unblocking temperature properties.Geophysical Research Letters,17(2):159-162.
Luo L,Jia D,Li H B,et al.2009.Magnetic fabric investigation in the northwestern Sichuan Basin and its regional inference.Physics of the Earth&Planetary Interiors,173(1-2):103-114.
Lv C.2015.Study of tectonic evolution and oil and gas reservoir forming conditions of Chuxiong basin[Master′s thesis](in Chinese).Hubei Jingzhou:Yangtze University.
MacDonald W D.1978.Domains of tectonic rotation-paleomagnetic evidence from the western Caribbean.Washington,DC:American Geophysical Union.
MacDonald W D.1980.Net tectonic rotation,apparent tectonic rotation,and the structural tilt correction in paleomagnetic studies.Journal of Geophysical Research,85(B7):3659-3669.
McFadden P L.1990.A new fold test for palaeomagnetic studies.Geophysical Journal International,103(1):163-169.
Otofuji Y I,Liu Y Y,Yokoyam M,et al.1998.Tectonic deformation of the southwestern part of the Yangtze craton inferred from paleomagnetism.Earth&Planetary Science Letters,156(1-2):47-60.
Parés J M,van der Pluijm B Q,Dinarès-Turell J.1999.Evolution of magnetic fabrics during incipient deformation of mudrocks(Pyrenees,Northern Spain).Tectonophysics,307(1-2):1-14.
Parés J M,van der Pluijm B A.2002.Evaluating magnetic lineations(AMS)in deformed rocks.Tectonophysics,350(4):283-298.
Pearson K.1895.Contributions to the mathematical theory of evolution.III.Regression,heredity,and panmixia.Proceedings of the Royal Society of London,187(4):253-318.
Pueyo E L,Parés J M,Millán H,et al.2003.Conical folds and apparent rotations in paleomagnetism(a case study in the Southern Pyrenees).Tectonophysics,362(1-4):345-366.
Replumaz A,Lacassin R,Tapponnier P,et al.2001.Large river offsets and Plio-Quaternary dextral slip rate on the Red River fault(Yunnan,China).Journal of Geophysical Research:Solid Earth,106(B1):819-836.
Roger F,Calassou S,Lancelot J,et al.1995.Miocene emplacement and deformation of the Konga Shan granite(Xianshui He fault zone,west Sichuan,China):Geodynamic implications.Earth&Planetary Science Letters,130(1-4):201-216.
Sagnotti L.2011.Magnetic anisotropy.∥Gupta H K ed.Encyclopedia of Solid Earth Geophysics.Encyclopedia of Earth Sciences Series.Dordrecht:Springer,717-729.
Saint-Bezar B,Hebert R L,Aubourg C,et al.2002.Magnetic fabric and petrographic investigation of hematite-bearing sandstones within ramp-related folds:examples from the South Atlas Front(Morocco).Journal of Structural Geology,24(9):1507-1520.
Sch?rer U,Zhang L S,Tapponnier P.1994.Duration of strike-slip movements in large shear zones:The Red River belt,China.Earth&Planetary Science Letters,126(4):379-397.
Schoenbohm L M,Burchfiel B C,Chen L Z,et al.2006.Miocene to present activity along the Red River fault,China,in the context of continental extrusion,upper-crustal rotation,and lower-crustal flow.GSA Bulletin,118(5-6):672-688.
Shi P L,Yang T N,Liang M J,et al.2015.Temporal and spatial variation in the Cenozoic strain of the Sanjiang orogenic belt,SW China:A brief review and new observations.Acta Petrologica Sinica(in Chinese),31(11):3331-3352.
Stephenson A,Sadikun S,Potter D K.1986.A theoretical and experimental comparison of the anisotropies of magnetic susceptibility and remanence in rocks and minerals.Geophysical Journal International,84(1):185-200.
Stewart S A.1995.Palaeomagnetic analysis of plunging fold structures:Errors and a simple fold test.Earth&Planetary Science Letters,130(1-4):57-67.
Tamai M,Liu Y Y,Lu L Z,et al.2004.Palaeomagnetic evidence for southward displacement of the Chuan Dian fragment of the Yangtze Block.Geophysical Journal International,158(1):297-309.
Tan X H.1999.Characteristics and formation mechanism of Cenozoic structural basins in the Three River area of west Yunnan.Yunnan Geology(in Chinese),18(2):112-121.
Tapponnier P,Peltzer G,Le Dain A Y,et al.1982.Propagating extrusion tectonics in Asia:New insights from simple experiments with plasticine.Geology,10(12):611-616.
Tapponnier P,Peltzer G,Armijo R,1986.On the mechanics of the collision between India and Asia.Geological Society,London,Special Publications,19(1):113-157.
Tapponnier P,Lacassin R,Leloup P H,et al.1990.The Ailao Shan/Red River metamorphic belt:Tertiary left-lateral shear between Indochina and South China.Nature,343(6257):431-437.
Tapponnier P,Xu Z Q,Roger F,et al.2001.Oblique stepwise rise and growth of the Tibet plateau.Science,294(5547):1671-1677.
Tarling D,Hrouda F.1993.Magnetic Anisotropy of Rocks.Netherlands:Springer.
Tong Y B,Yang Z Y,Zheng L D,et al.2013.Internal crustal deformation in the northern part of Shan-Thai Block:New evidence from paleomagnetic results of Cretaceous and Paleogene redbeds.Tectonophysics,608:1138-1158.
Tong Y B,Yang Z Y,Wang H,et al.2015.The Cenozoic rotational extrusion of the Chuan Dian Fragment:New paleomagnetic results from Paleogene red-beds on the southeastern edge of the Tibetan Plateau.Tectonophysics,658:46-60.
Wang E,Burchfiel B C,Royden L H,et al.1998.Late Cenozoic Xianshuihe-Xiaojiang,Red River,and Dali fault systems of southwestern Sichuan and central Yunnan,China.Special Paper of the Geological Society of America,327:1-108.
Wang E,Meng K,Su Z,et al.2014.Block rotation:Tectonic response of the Sichuan basin to the southeastward growth of the Tibetan Plateau along the Xianshuihe-Xiaojiang fault.Tectonics,33(5):686-718.
Wang H,Yang Z Y,Tong Y B,et al.2016.Palaeomagnetic results from Palaeogene red beds of the Chuan-Dian Fragment,southeastern margin of the Tibetan Plateau:implications for the displacement on the Xianshuihe-Xiaojiang fault systems.International Geology Review,58(11):1363-1381.
Wang S F,Wang E,Fang X M,et al.2008a.Late Cenozoic systematic left-lateral stream deflections along the Ganzi-Yushu fault,Xianshuihe fault system,eastern Tibet.International Geology Review,50(7):624-635.
Wang S,Fan C,Wang G,et al.2008b.Late Cenozoic deformation along the northwestern continuation of the Xianshuihe fault system,Eastern Tibetan Plateau.Geological Society of America Bulletin,120(3-4):312-327.
Wang S F,Jiang G G,Xu T D,et al.2012.The Jinhe-Qinghe fault-an inactive branch of the Xianshuihe-Xiaojiang fault zone,Eastern Tibet.Tectonophysics,544-545:93-102.
Wu G Y.1994.Tertiary thrusting-nappe structures in northwest Yunnan,China.Geotectonica et Metallogenia(in Chinese),18(4):331-338.
Xu Y C,Tong Y B,Wang H,et al.2017.Paleomagnetic constrains on the reversed S-shaped structure deformation of the LanqingSimao Basin in the southeastern Xizang(Tibet)plateau.Geological Review(in Chinese),63(3):549-567.
Yan G L.1996.Application of Anisotropy of Susceptibility to Earth Science(in Chinese).Beijing:China University of Geosciences Press.
Yang T N,Liang M J,Fan J W,et al.2014.Paleogene sedimentation,volcanism,and deformation in eastern Tibet:evidence from structures,geochemistry,and zircon U-Pb dating in the Jianchuan Basin,SW China.Gondwana Research,26(2):521-535.
Yang Z Y,Besse J.1993.Paleomagnetic study of Permian and Mesozoic sedimentary rocks from Northern Thailand supports the extrusion model for Indochina.Earth&Planetary Science Letters,117(3-4):525-552.
Yang Z Y,Sun Z M,Ma X H,et al.2001.Palaeomagnetic study of the early Tertiary on both sides of the red river fault and its geological implications.Acta Geologica Sinica(in Chinese),75(1):35-44.
Yoshioka S Y,Liu Y Y,Sato K,et al.2003.Paleomagnetic evidence for post-Cretaceous internal deformation of the Chuan Dian Fragment in the Yangtze block:a consequence of indentation of India into Asia.Tectonophysics,376(1-2):61-74.
Yunnan Bureau of Geology and Mineral Resources.1990.Regional Geology of Yunnan Province(in Chinese).Beijing:Geological Publishing House.
Zhang B,Zhang J J,Zhong D L.2010.Structure,kinematics and ages of transpression during strain-partitioning in the Chongshan shear zone,western Yunnan,China.Journal of Structural Geology,32(4):445-463.
段建中,谭筱虹.2000.滇西三江地区新生代主要走滑断裂性质及特征.云南地质,19(1):8-23.
段建中,薛顺荣,钱祥贵.2001.滇西“三江”地区新生代地质构造格局及其演化.云南地质,20(3):243-253.
贾东,陈竹新,罗良等.2007.断层相关褶皱的磁组构与有限应变:川西岷江冲断构造的实例分析.自然科学进展,17(2):188-195.
李光勋.1994.兰坪盆地某些逆冲推覆构造研究.云南地质,13(2):203-215.
李仕虎,黄宝春,朱日祥.2012.青藏高原东南缘构造旋转的古地磁学证据.地球物理学报,55(1):76-94,doi:10.6038/j.issn.0001-5733.2012.01.008.
李震宇,黄宝春,张春霞.2010.河南西南部典型白垩纪剖面的岩石磁组构特征及其构造意义.岩石学报,26(11):3418-3430.
刘和甫,汪泽成,熊保贤等.2000.中国中西部中、新生代前陆盆地与挤压造山带耦合分析.地学前缘,7(3):55-72.
刘俊来,宋志杰,曹淑云等.2006.印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程——以藏东三江地区构造演化为例.岩石学报,22(4):775-786.
吕财.2015.楚雄盆地构造演化及油气成藏条件研究[硕士论文].湖北荆州:长江大学.
史鹏亮,杨天南,梁明娟等.2015.三江构造带新生代变形构造的时-空变化:研究综述及新数据.岩石学报,31(11):3331-3352.
谭筱虹.1999.滇西三江地区新生代构造盆地的特征及形成机制.云南地质,18(2):112-121.
吴根耀.1994.滇西北地区第三纪的逆冲-推覆构造.大地构造与成矿学,18(4):331-338.
徐颖超,仝亚博,王恒等.2017.青藏高原东南缘兰坪-思茅盆地反S型构造属性的古地磁约束.地质论评,63(3):549-567.
阎桂林.1996.岩石磁化率各向异性在地学中的应用.北京:中国地质大学出版社.
杨振宇,孙知明,马醒华等.2001.红河断裂两侧早第三纪古地磁研究及其地质意义.地质学报,75(1):35-44.
云南省地质局.1965.区域地质调查报告(大姚幅).
云南省地质局.1973.区域地质调查报告(大理幅).
云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社.
Allen C R,Gillespie A R,Yuan H,et al.1984.Red River and associated faults,Yunnan Province,China:Quaternary geology,slip rates,and seismic hazard.Geological Society of America Bulletin,95(6):686-700.
Allen C R,Luo Z L,Qian H,et al.1991.Field study of a highly active fault zone:The Xianshuihe fault of southwestern China.Geological Society of America Bulletin,103(9):1178-1199.
Borradaile G J,Jackson M.2004.Anisotropy of magnetic susceptibility(AMS):magnetic petrofabrics of deformed rocks.Geological Society,London,Special Publications,238(1):299-360.
Bullard E,Everett J E,Smith A G.1965.The fit of the continents around the Atlantic.Philosophical Transactions of the Royal Society A:Mathematical,Physical&Engineering Sciences,258(1088):41-51.
Burchfiel B C,Wang E.2003.Northwest-trending,middle Cenozoic,left-lateral faults in southern Yunnan,China,and their tectonic significance.Journal of Structural Geology,25(5):781-792.
Burchfiel B C,Chen Z L.2013.Tectonics of the southeastern Tibetan Plateau and its adjacent foreland.Memoir of the Geological Society of America,210:1-164.
Cao S Y,Liu J L,Leiss B,et al.2012.Initiation of left-lateral deformation along the Ailao Shan-Red River shear zone:new microstructural,textural,and geochronological constraints from the Diancang Shan metamorphic massif,SW Yunnan,China.International Geology Review,54(3):348-367.
Chung S L,Lee T Y,Lo C H,et al.1997.Intraplate extension prior to continental extrusion along the Ailao Shan-Red River shear zone.Geology,25(4):311-314.
Chung S L,Searle M P,Yeh M W.2007.The age of the potassic alkaline igneous rocks along the Ailao Shan-Red River Shear Zone:Implications for the onset age of left-lateral shearing:Adiscussion.Journal of Geology,116(2):231-242.
CognéJ P.1987.TRM deviations in anisotropic assemblages of multidomain magnetite.Geophysical Journal International,91(3):1013-1023.
CognéJ P.2003.PaleoMac:A MacintoshTMapplication for treating paleomagnetic data and making plate reconstructions.Geochemistry,Geophysics,Geosystems,4(1):1007,doi:10.1029/2001GC000227.
CognéJ P.2013.Cenozoic Eurasia is not a single rigid plate:Paleomagnetic evidence.Comptes Rendus Geoscience,345(11-12):419-426.
CognéJ P,Besse J,Chen Y,et al.2013.A new Late Cretaceous to Present APWP for Asia and its implications for paleomagnetic shallow inclinations in Central Asia and Cenozoic Eurasian plate deformation.Geophysical Journal International,192(3):1000-1024.
Duan J Z,Tan X H.2000.The nature and feature of Cenozoic main strike-slip fault in the three-river area of west Yunnan.Yunnan Geology(in Chinese),19(1):8-23.
Duan J Z,Xue S R,Qian X G.2001.The Cenozoic geological tectonic framework and evolution in the three-river area of west Yunnan.Yunnan Geology(in Chinese),20(3):243-253.
Dubien J L,Warde W D.1979.A mathematical comparison of the members of an infinite family of agglomerative clustering algorithms.Canadian Journal of Statistics,7(1):29-38.
Evans M A,Lewchuk M T,Elmore R D.2003.Strain partitioning of deformation mechanisms in limestones:Examining the relationship of strain and anisotropy of magnetic susceptibility(AMS).Journal of Structural Geology,25(9):1525-1549.
Fan C,Wang G,Wang S F,et al.2006.Structural interpretation of extensional deformation along the Dali fault system,southeastern margin of the Tibetan Plateau.International Geology Review,48(4):287-310.
Finlay C C,Maus S,Beggan C D,et al.2010.International geomagnetic reference field:the eleventh generation.Geophysical Journal International,183(3):1216-1230.
Funahara S,Nishiwaki N,Miki M,et al.1992.Paleomagnetic study of Cretaceous rocks from the Yangtze block,central Yunnan,China:implications for the India-Asia collision.Earth&Planetary Science Letters,113(1-2):77-91.
Funahara S,Nishiwaki N,Murata F,et al.1993.Clockwise rotation of the Red River fault inferred from paleomagnetic study of Cretaceous rocks in the Shan-Thai-Malay block of Western Yunnan,China.Earth&Planetary Science Letters,117(1-2):29-42.
Geological Survey of Yunnan Province.1965.Regional geological survey report(Dayao)(in Chinese).
Geological Survey of Yunnan Province.1973.Regional geological survey report(Dali)(in Chinese).
Gilley L D,Harrison T M,Leloup P H,et al.2003.Direct dating of left-lateral deformation along the Red River shear zone,China and Vietnam.Journal of Geophysical Research:Solid Earth,108(B2):2127,doi:10.1029/2001JB001726.
Guillot S,Mahéo G,de Sigoyer J,et al.2008.Tethyan and Indian subduction viewed from the Himalayan high-to ultrahighpressure metamorphic rocks.Tectonophysics,451(1-4):225-241.
Harrison T M,Leloup P H,Ryerson F J,et al.1996.Diachronous initiation of transtension along the Ailao Shan-Red River shear zone,Yunnan and Vietnam.World&Regional Geology,1(8):208-226.
Hrouda F.2007.Magnetic susceptibility,anisotropy.∥Gubbins D,Herrero-Bervera E eds.Encyclopedia of Geomagnetism and Paleomagnetism.Netherlands:Springer.
Huang B C,Piper J D A,Peng S T,et al.2006.Magnetostratigraphic study of the Kuche Depression,Tarim Basin,and Cenozoic uplift of the Tian Shan Range,Western China.Earth&Planetary Science Letters,251(3-4):346-364.
Huang K N,Opdyke N D.1992.Paleomagnetism of Cretaceous to lower Tertiary rocks from southwestern Sichuan:a revisit.Earth&Planetary Science Letters,112(1-4):29-40.
Huang K N,Opdyke N D.1993.Paleomagnetic results from Cretaceous and Jurassic rocks of South and Southwest Yunnan:evidence for large clockwise rotations in the Indochina and ShanThai-Malay terranes.Earth&Planetary Science Letters,117(3-4):507-524.
Jelinek V.1981.Characterization of the magnetic fabric of rocks.Tectonophysics,79(3-4):T63-T67.
Jia D,Chen Z X,Luo L,et al.2007.Magnetic fabric and finite strain of fault-related folds:an example analysis of Minjiang thrust structure in western Sichuan province.Advances in Natural Science(in Chinese),17(2):188-195.
Johnson M R W.2002.Shortening budgets and the role of continental subduction during the India-Asia collision.EarthScience Reviews,59(1-4):101-123.
Kirschvink J L.1980.The least-squares line and plane and the analysis of palaeomagnetic data.Geophysical Journal International,62(3):699-718.
Leloup P H,Harrison T M,Ryerson F J,et al.1993.Structural,petrological and thermal evolution of a Tertiary ductile strikeslip shear zone,Diancang Shan,Yunnan.Journal of Geophysical Research:Solid Earth,98(B4):6715-6743.
Leloup P H,Lacassin R,Tapponnier P,et al.1995.The Ailao Shan-Red River shear zone(Yunnan,China),Tertiary transform boundary of Indochina.Tectonophysics,251(1-4):13-84.
Leloup P H,Arnaud N,Lacassin R,et al.2001.New constraints on the structure,thermochronology,and timing of the Ailao Shan-Red River shear zone,SE Asia.Journal of Geophysical Research:Solid Earth,106(B4):6683-6732.
Li G X.1994.A preliminary study of some thrust-nappe structures in Lanping basin.Yunnan Geology(in Chinese),13(2):203-215.
Li S H,Deng C L,Dong W,et al.2015.Magnetostratigraphy of the Xiaolongtan Formation bearing Lufengpithecus keiyuanensis in Yunnan,southwestern China:Constraint on the initiation time of the southern segment of the Xianshuihe-Xiaojiang fault.Tectonophysics,655:213-226.
Li S H,Huang B C,Zhu R X.2012.Paleomagnetic constraints on the tectonic rotation of the southeastern margin of the Tibetan Plateau.Chinese J.Geophys.(in Chinese),55(1):76-94,doi:10.6038/j.issn.0001-5733.2012.01.008.
Li Z Y,Huang B C,Zhang C X.2010.Characteristic of anisotropy of magnetic susceptibility(AMS)and its tectonic significance in typical Cretaceous section from Xixia basin,central China.Acta Petrologica Sinica(in Chinese),26(11):3418-3430.
Liu H F,Wang Z C,Xiong B X,et al.2000.Coupling analysis of Mesozoic-Cenozoic foreland basin and mountain system in central and western China.Earth Science Frontiers(in Chinese),7(3):55-72.
Liu J L,Tang Y,Tran M D,et al.2012.The nature of the Ailao Shan-Red River(ASRR)shear zone:Constraints from structural,microstructural and fabric analyses of metamorphic rocks from the Diancang Shan,Ailao Shan and Day Nui Con Voi massifs.Journal of Asian Earth Sciences,47:231-251.
Liu J L,Song Z J,Cao S Y,et al.2006.The dynamic setting and processes of tectonic and magmatic evolution of the oblique collision zone between Indian and Eurasian plates:Exemplified by the tectonic evolution of the Three River region,eastern Tibet.Acta Petrologica Sinica(in Chinese),22(4):775-786.
Lowrie W.1990.Identification of ferromagnetic minerals in a rock by coercivity and unblocking temperature properties.Geophysical Research Letters,17(2):159-162.
Luo L,Jia D,Li H B,et al.2009.Magnetic fabric investigation in the northwestern Sichuan Basin and its regional inference.Physics of the Earth&Planetary Interiors,173(1-2):103-114.
Lv C.2015.Study of tectonic evolution and oil and gas reservoir forming conditions of Chuxiong basin[Master′s thesis](in Chinese).Hubei Jingzhou:Yangtze University.
MacDonald W D.1978.Domains of tectonic rotation-paleomagnetic evidence from the western Caribbean.Washington,DC:American Geophysical Union.
MacDonald W D.1980.Net tectonic rotation,apparent tectonic rotation,and the structural tilt correction in paleomagnetic studies.Journal of Geophysical Research,85(B7):3659-3669.
McFadden P L.1990.A new fold test for palaeomagnetic studies.Geophysical Journal International,103(1):163-169.
Otofuji Y I,Liu Y Y,Yokoyam M,et al.1998.Tectonic deformation of the southwestern part of the Yangtze craton inferred from paleomagnetism.Earth&Planetary Science Letters,156(1-2):47-60.
Parés J M,van der Pluijm B Q,Dinarès-Turell J.1999.Evolution of magnetic fabrics during incipient deformation of mudrocks(Pyrenees,Northern Spain).Tectonophysics,307(1-2):1-14.
Parés J M,van der Pluijm B A.2002.Evaluating magnetic lineations(AMS)in deformed rocks.Tectonophysics,350(4):283-298.
Pearson K.1895.Contributions to the mathematical theory of evolution.III.Regression,heredity,and panmixia.Proceedings of the Royal Society of London,187(4):253-318.
Pueyo E L,Parés J M,Millán H,et al.2003.Conical folds and apparent rotations in paleomagnetism(a case study in the Southern Pyrenees).Tectonophysics,362(1-4):345-366.
Replumaz A,Lacassin R,Tapponnier P,et al.2001.Large river offsets and Plio-Quaternary dextral slip rate on the Red River fault(Yunnan,China).Journal of Geophysical Research:Solid Earth,106(B1):819-836.
Roger F,Calassou S,Lancelot J,et al.1995.Miocene emplacement and deformation of the Konga Shan granite(Xianshui He fault zone,west Sichuan,China):Geodynamic implications.Earth&Planetary Science Letters,130(1-4):201-216.
Sagnotti L.2011.Magnetic anisotropy.∥Gupta H K ed.Encyclopedia of Solid Earth Geophysics.Encyclopedia of Earth Sciences Series.Dordrecht:Springer,717-729.
Saint-Bezar B,Hebert R L,Aubourg C,et al.2002.Magnetic fabric and petrographic investigation of hematite-bearing sandstones within ramp-related folds:examples from the South Atlas Front(Morocco).Journal of Structural Geology,24(9):1507-1520.
Sch?rer U,Zhang L S,Tapponnier P.1994.Duration of strike-slip movements in large shear zones:The Red River belt,China.Earth&Planetary Science Letters,126(4):379-397.
Schoenbohm L M,Burchfiel B C,Chen L Z,et al.2006.Miocene to present activity along the Red River fault,China,in the context of continental extrusion,upper-crustal rotation,and lower-crustal flow.GSA Bulletin,118(5-6):672-688.
Shi P L,Yang T N,Liang M J,et al.2015.Temporal and spatial variation in the Cenozoic strain of the Sanjiang orogenic belt,SW China:A brief review and new observations.Acta Petrologica Sinica(in Chinese),31(11):3331-3352.
Stephenson A,Sadikun S,Potter D K.1986.A theoretical and experimental comparison of the anisotropies of magnetic susceptibility and remanence in rocks and minerals.Geophysical Journal International,84(1):185-200.
Stewart S A.1995.Palaeomagnetic analysis of plunging fold structures:Errors and a simple fold test.Earth&Planetary Science Letters,130(1-4):57-67.
Tamai M,Liu Y Y,Lu L Z,et al.2004.Palaeomagnetic evidence for southward displacement of the Chuan Dian fragment of the Yangtze Block.Geophysical Journal International,158(1):297-309.
Tan X H.1999.Characteristics and formation mechanism of Cenozoic structural basins in the Three River area of west Yunnan.Yunnan Geology(in Chinese),18(2):112-121.
Tapponnier P,Peltzer G,Le Dain A Y,et al.1982.Propagating extrusion tectonics in Asia:New insights from simple experiments with plasticine.Geology,10(12):611-616.
Tapponnier P,Peltzer G,Armijo R,1986.On the mechanics of the collision between India and Asia.Geological Society,London,Special Publications,19(1):113-157.
Tapponnier P,Lacassin R,Leloup P H,et al.1990.The Ailao Shan/Red River metamorphic belt:Tertiary left-lateral shear between Indochina and South China.Nature,343(6257):431-437.
Tapponnier P,Xu Z Q,Roger F,et al.2001.Oblique stepwise rise and growth of the Tibet plateau.Science,294(5547):1671-1677.
Tarling D,Hrouda F.1993.Magnetic Anisotropy of Rocks.Netherlands:Springer.
Tong Y B,Yang Z Y,Zheng L D,et al.2013.Internal crustal deformation in the northern part of Shan-Thai Block:New evidence from paleomagnetic results of Cretaceous and Paleogene redbeds.Tectonophysics,608:1138-1158.
Tong Y B,Yang Z Y,Wang H,et al.2015.The Cenozoic rotational extrusion of the Chuan Dian Fragment:New paleomagnetic results from Paleogene red-beds on the southeastern edge of the Tibetan Plateau.Tectonophysics,658:46-60.
Wang E,Burchfiel B C,Royden L H,et al.1998.Late Cenozoic Xianshuihe-Xiaojiang,Red River,and Dali fault systems of southwestern Sichuan and central Yunnan,China.Special Paper of the Geological Society of America,327:1-108.
Wang E,Meng K,Su Z,et al.2014.Block rotation:Tectonic response of the Sichuan basin to the southeastward growth of the Tibetan Plateau along the Xianshuihe-Xiaojiang fault.Tectonics,33(5):686-718.
Wang H,Yang Z Y,Tong Y B,et al.2016.Palaeomagnetic results from Palaeogene red beds of the Chuan-Dian Fragment,southeastern margin of the Tibetan Plateau:implications for the displacement on the Xianshuihe-Xiaojiang fault systems.International Geology Review,58(11):1363-1381.
Wang S F,Wang E,Fang X M,et al.2008a.Late Cenozoic systematic left-lateral stream deflections along the Ganzi-Yushu fault,Xianshuihe fault system,eastern Tibet.International Geology Review,50(7):624-635.
Wang S,Fan C,Wang G,et al.2008b.Late Cenozoic deformation along the northwestern continuation of the Xianshuihe fault system,Eastern Tibetan Plateau.Geological Society of America Bulletin,120(3-4):312-327.
Wang S F,Jiang G G,Xu T D,et al.2012.The Jinhe-Qinghe fault-an inactive branch of the Xianshuihe-Xiaojiang fault zone,Eastern Tibet.Tectonophysics,544-545:93-102.
Wu G Y.1994.Tertiary thrusting-nappe structures in northwest Yunnan,China.Geotectonica et Metallogenia(in Chinese),18(4):331-338.
Xu Y C,Tong Y B,Wang H,et al.2017.Paleomagnetic constrains on the reversed S-shaped structure deformation of the LanqingSimao Basin in the southeastern Xizang(Tibet)plateau.Geological Review(in Chinese),63(3):549-567.
Yan G L.1996.Application of Anisotropy of Susceptibility to Earth Science(in Chinese).Beijing:China University of Geosciences Press.
Yang T N,Liang M J,Fan J W,et al.2014.Paleogene sedimentation,volcanism,and deformation in eastern Tibet:evidence from structures,geochemistry,and zircon U-Pb dating in the Jianchuan Basin,SW China.Gondwana Research,26(2):521-535.
Yang Z Y,Besse J.1993.Paleomagnetic study of Permian and Mesozoic sedimentary rocks from Northern Thailand supports the extrusion model for Indochina.Earth&Planetary Science Letters,117(3-4):525-552.
Yang Z Y,Sun Z M,Ma X H,et al.2001.Palaeomagnetic study of the early Tertiary on both sides of the red river fault and its geological implications.Acta Geologica Sinica(in Chinese),75(1):35-44.
Yoshioka S Y,Liu Y Y,Sato K,et al.2003.Paleomagnetic evidence for post-Cretaceous internal deformation of the Chuan Dian Fragment in the Yangtze block:a consequence of indentation of India into Asia.Tectonophysics,376(1-2):61-74.
Yunnan Bureau of Geology and Mineral Resources.1990.Regional Geology of Yunnan Province(in Chinese).Beijing:Geological Publishing House.
Zhang B,Zhang J J,Zhong D L.2010.Structure,kinematics and ages of transpression during strain-partitioning in the Chongshan shear zone,western Yunnan,China.Journal of Structural Geology,32(4):445-463.
段建中,谭筱虹.2000.滇西三江地区新生代主要走滑断裂性质及特征.云南地质,19(1):8-23.
段建中,薛顺荣,钱祥贵.2001.滇西“三江”地区新生代地质构造格局及其演化.云南地质,20(3):243-253.
贾东,陈竹新,罗良等.2007.断层相关褶皱的磁组构与有限应变:川西岷江冲断构造的实例分析.自然科学进展,17(2):188-195.
李光勋.1994.兰坪盆地某些逆冲推覆构造研究.云南地质,13(2):203-215.
李仕虎,黄宝春,朱日祥.2012.青藏高原东南缘构造旋转的古地磁学证据.地球物理学报,55(1):76-94,doi:10.6038/j.issn.0001-5733.2012.01.008.
李震宇,黄宝春,张春霞.2010.河南西南部典型白垩纪剖面的岩石磁组构特征及其构造意义.岩石学报,26(11):3418-3430.
刘和甫,汪泽成,熊保贤等.2000.中国中西部中、新生代前陆盆地与挤压造山带耦合分析.地学前缘,7(3):55-72.
刘俊来,宋志杰,曹淑云等.2006.印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程——以藏东三江地区构造演化为例.岩石学报,22(4):775-786.
吕财.2015.楚雄盆地构造演化及油气成藏条件研究[硕士论文].湖北荆州:长江大学.
史鹏亮,杨天南,梁明娟等.2015.三江构造带新生代变形构造的时-空变化:研究综述及新数据.岩石学报,31(11):3331-3352.
谭筱虹.1999.滇西三江地区新生代构造盆地的特征及形成机制.云南地质,18(2):112-121.
吴根耀.1994.滇西北地区第三纪的逆冲-推覆构造.大地构造与成矿学,18(4):331-338.
徐颖超,仝亚博,王恒等.2017.青藏高原东南缘兰坪-思茅盆地反S型构造属性的古地磁约束.地质论评,63(3):549-567.
阎桂林.1996.岩石磁化率各向异性在地学中的应用.北京:中国地质大学出版社.
杨振宇,孙知明,马醒华等.2001.红河断裂两侧早第三纪古地磁研究及其地质意义.地质学报,75(1):35-44.
云南省地质局.1965.区域地质调查报告(大姚幅).
云南省地质局.1973.区域地质调查报告(大理幅).
云南省地质矿产局.1990.云南省区域地质志.北京:地质出版社.