江南东段地区NE-SW向断裂带断层滑移矢量反演及其大地构造意义
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摘要
华南中-新生代构造演化受太平洋构造域和特提斯洋构造域的联合控制.以江南东段NE-SW向景德镇-歙县剪切带和球川-萧山断裂中发育的脆性断层为研究对象,利用野外交切关系和断层滑移矢量反演方法厘定了7期构造变形序列并反演了各期古构造应力场,讨论了断层活动的时代及其动力学.白垩纪至新生代研究区7期古构造应力场分别为:(1)早白垩世早期(136～125Ma)NW-SE向伸展;(2)早白垩世晚期(125～107Ma)N-S向挤压和E-W向伸展;(3)早白垩世末期至晚白垩世早期(105～86Ma)NW-SE向伸展;(4)白垩世中期(86～80Ma)NW-SE向挤压和NE-SW向伸展;(5)晚白垩世晚期至始新世末期(80～36Ma)N-S向伸展;(6)始新世末期至渐新世早期(36～30Ma)NE-SW向挤压和NW-SE向伸展;(7)渐新世早期至中新世中期(30～17Ma)NE-SW向伸展.结合区域地质研究表明,第1期至第4期古构造应力场与古太平洋构造域的板片后撤、俯冲以及微块体(菲律宾地块)间的碰撞作用有关;第5期伸展作用受控于新特提斯构造域俯冲板片后撤,而第6期和第7期古构造应力场主要与印-亚碰撞的远程效应有关.白垩纪至新生代,华南东部受伸展构造体制和走滑构造体制的交替控制.先存断裂的发育可能是导致华南晚中生代走滑构造体制的主要控制因素.
Mesozoic to Cenozoic tectonic evolution of the South China Block was dominated jointly by the Pacific tectonic domain and the Tethys tectonic domain.Brittle faulting of the NE-SW-striking Jingdezhen-Shexian shear zone and the QiuchuanXiaoshan fault was studied in the eastern Jiangnan area.Based on cross-cutting relations and inversion of fault-slip data,seven stages of structural deformation were identified and their paleostress fields were inverted.Their formation ages and geodynamics are also discussed.Cretaceous to Cenozoic paleostress fields that occurred in the eastern Jiangnan area are:(1)NW-SE extension during early stage of Early Cretaceous(136-125 Ma);(2)N-S compression and E-W extension during late stage of Early Cretaceous(125-107 Ma);(3)latest Early Cretaceous to early stage of Early Cretaceous(105-86 Ma)NW-SE extension;(4)middle Late Cretaceous(86-80 Ma)NW-SE compression and NE-SW extension;(5)N-S extension during late stage of Late Cretaceous to latest Eocene(80-36 Ma);(6)NE-SW compression and NW-SE extension during latest Eocene to early stage of Oligocene(36-30 Ma);(7)early stage of Oligocene to medium stage of Miocene(30-17 Ma)NE-SW extension.Combining these with regional geological evidences,the first to fourth paleostress fields were related to roll-back,subduction of the Pacific Plate and collision between micro-terrane(Philippine Sea plate)and the South China Block.The fifth paleostress field was attributed to the roll-back of Neo-Tethys oceanic plate whereas the sixth and seventh paleostress fields to the far-field effect of the India-Asia collision.Extensional regimes and strike-slip regimes alternately dominated Cretaceous to Cenozoic structural deformation in the South China Block.The predominated factor for the strike-slip regimes in the South China Block is re-existed faults occurred before Late Mesozoic.
Mesozoic to Cenozoic tectonic evolution of the South China Block was dominated jointly by the Pacific tectonic domain and the Tethys tectonic domain.Brittle faulting of the NE-SW-striking Jingdezhen-Shexian shear zone and the QiuchuanXiaoshan fault was studied in the eastern Jiangnan area.Based on cross-cutting relations and inversion of fault-slip data,seven stages of structural deformation were identified and their paleostress fields were inverted.Their formation ages and geodynamics are also discussed.Cretaceous to Cenozoic paleostress fields that occurred in the eastern Jiangnan area are:(1)NW-SE extension during early stage of Early Cretaceous(136-125 Ma);(2)N-S compression and E-W extension during late stage of Early Cretaceous(125-107 Ma);(3)latest Early Cretaceous to early stage of Early Cretaceous(105-86 Ma)NW-SE extension;(4)middle Late Cretaceous(86-80 Ma)NW-SE compression and NE-SW extension;(5)N-S extension during late stage of Late Cretaceous to latest Eocene(80-36 Ma);(6)NE-SW compression and NW-SE extension during latest Eocene to early stage of Oligocene(36-30 Ma);(7)early stage of Oligocene to medium stage of Miocene(30-17 Ma)NE-SW extension.Combining these with regional geological evidences,the first to fourth paleostress fields were related to roll-back,subduction of the Pacific Plate and collision between micro-terrane(Philippine Sea plate)and the South China Block.The fifth paleostress field was attributed to the roll-back of Neo-Tethys oceanic plate whereas the sixth and seventh paleostress fields to the far-field effect of the India-Asia collision.Extensional regimes and strike-slip regimes alternately dominated Cretaceous to Cenozoic structural deformation in the South China Block.The predominated factor for the strike-slip regimes in the South China Block is re-existed faults occurred before Late Mesozoic.
引文
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Hu,Q.H.,Yu,K.Z.,Liu,Y.S.,et al.,2017.The 131-134 Ma A-Type Granites from Northern Zhejiang Province,South China:Implications for Partial Melting of the Neoproterozoic Lower Crust.Lithos,294-295:39-52.https://doi.org/10.1016/j.lithos.2017.09.016
Huo,H.L.,Zhang,D.,Chen,Z.L.,et al.,2016.Deformation Characteristics and Geochronological Constraints of Mesozoic Nappe Structure in Jingdezhen Area,Northeastern Jiangxi.Journal of Geomechanics,24(1):9-24(in Chinese with English abstract).
Jiang,Y.H.,Zhao,P.,Zhou,Q.,et al.,2011.Petrogenesis and Tectonic Implications of Early Cretaceous S-and A-Type Granites in the Northwest of the Gan-Hang Rift,SE China.Lithos,121(1-4):55-73.
Li,J.,Dong,S.,Zhang,Y.,et al.,2016a.New Insights into Phanerozoic Tectonics of South China:Part 1.Polyphase Deformation in the Jiuling and Lianyunshan Domains of the Central Jiangnan Orogen.Journal of Geophysical Research(Solid Earth),121(4):3048-3080.https://doi.org/10.1002/2015jb012778
Li,Y.,Dong,S.W.,Zhang,Y.Q.,et al.,2016b.Episodic Mesozoic Constructional Events of Central South China:Constraints from Lines of Evidence of Superimposed Folds,Fault Kinematic Analysis,and Magma Geochronology.International Geology Review,58(9):1076-1107.https://doi.org/10.1080/00206814.2016.1146999
Li,J.H.,Ma,Z.L.,Zhang,Y.Q.,et al.,2014a.Tectonic Evolution of Cretaceous Extensional Basins in Zhejiang Province,Eastern South China:Structural and Geochronological Constraints.International Geology Review,56(13):1602-1629.https://doi.org/10.1080/00206814.2014.951978
Li,J.H.,Zhang,Y.Q.,Dong,S.W.,et al.,2014b.Cretaceous Tectonic Evolution of South China:A Preliminary Synthesis.Earth-Science Reviews,134:98-136.https://doi.org/10.1016/j.earscirev.2014.03.008
Li,J.H.,Zhang,Y.Q.,Dong,S.W.,et al.,2012.Late MesozoicEarly Cenozoic Deformation History of the Yuanma Basin,Central South China.Tectonophysics,570:163-183.https://doi.org/10.1016/j.tecto.2012.08.012
Li,J.H.,Zhang,Y.Q.,Dong,S.W.,et al.,2013a.The Hengshan Low-Angle Normal Fault Zone:Structural and Geochronological Constraints on the Late Mesozoic Crustal Extension in South China.Tectonophysics,606:97-115.https://doi.org/10.1016/j.tecto.2013.05.013
Li,Z.L.,Zhou,J.,Mao,J.R.,et al.,2013b.Zircon U-Pb Geochronology and Geochemistry of Two Episodes of Granitoids from the Northwestern Zhejiang Province,SE China:Implication for Magmatic Evolution and Tectonic Transition.Lithos,179:334-352.https://doi.org/10.1016/j.lithos.2013.07.014
Ma,Y.S.,Chen,H.D.,Wang,G.L.,2009.Sequence Stratigraphy and Paleogeography of South China.Science Press,Beijing,148(in Chinese).
Sato,H.,Kato,N.,Abe,S.,et al.,2015.Reactivation of an Old Plate Interface as a Strike-Slip Fault in a SlipPartitioned System:Median Tectonic Line,SW Japan.Tectonophysics,644:58-67.
Shu,L.S.,2012.An Analysis of Principal Features of Tectonic Evolution in South China Block.GeologicalBulletinofChina,31(7):1035-1053(in Chinese with English abstract).
Sun,W.D.,Ding,X.,Hu,Y.H.,et al.,2007.The Golden Transformation of the Cretaceous Plate Subduction in the West Pacific.Earth and Planetary Science Letters,262(3-4):533-542.
Sun,Y.,Ma,C.,Liu,B.,2017.Record of Late Yanshanian Mafic Magmatic Activity in the Middle-Lower Yangtze River Metallogenic Belt.Earth Science,42(6):891-908(in Chinese with English abstract).
Tan,Q.L.,Wang,Y.J.,Zhang,Y.Z.,et al.,2017.Taohong Diorite from Pingshui Region in Eastern Jiangnan Orogen:Evidence for Early Neoproterozoic Oceanic Crust Subduction.Earth Science,42(2):173-190(in Chinese with English abstract).
Tang,S.,Xu,X.B.,Yuan,Y.M.,2016.Geochemistry and Geochronology of the Volcanic Rocks from Tunxi Basin in Southern Anhui and Their Tectonic Significance.Acta Petrologica et Mineralogica,35(2):177-194(in Chinese with English abstract).
Wang,P.C.,Zhao,S.J.,Li,S.Z.,et al.,2015.The Styles and Dynamics of Thrust in the South of the Middle-Lower Yangtze River Area.Acta Petrologica Sinica,31(1):230-244(in Chinese with English abstract).
Wang,Y.J.,Fan,W.M.,Zhang,G.W.,et al.,2013a.Phanerozoic Tectonics of the South China Block:Key Observations and Controversies.Gondwana Research,23(4):1273-1305.https://doi.org/10.1016/j.gr.2012.02.019
Wang,Y.J.,Zhang,A.M.,Cawood,P.A.,et al.,2013b.Geochronological,Geochemical and Nd-Hf-Os Isotopic Fingerprinting of an Early Neoproterozoic Arc-Back-Arc System in South China and Its Accretionary Assembly along the Margin of Rodinia.Precambrian Research,231:343-371.https://doi.org/10.1016/j.precamres.2013.03.020
Wei,W.,Faure,M.,Chen,Y.,et al.,2015.Back-Thrusting Response of Continental Collision:Early Cretaceous NW-Directed Thrusting in the Changle-Nan’ao Belt(Southeast China).Journal of Asian Earth Sciences,100:98-114.https://doi.org/10.1016/j.jseaes.2015.01.005
Xiao,W.J.,He,H.Q.,2005.Early Mesozoic Thrust Tectonics of the Northwest Zhejiang Region(Southeast China).Geological Society of America Bulletin,117(7-8):945-961.
Xu,X.B.,Li,Y.,Tang,S.,et al.,2015.Neoproterozoic to Early Paleozoic Polyorogenic Deformation in the Southeastern Margin of the Yangtze Block:Constraints from Structural Analysis and 40 Ar/39 Ar Geochronology.Journal of Asian Earth Sciences,98:141-151.https://doi.org/10.1016/j.jseaes.2014.11.015
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