吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (4): 1005-1025.doi: 10.13278/j.cnki.jjuese.201604103
李三忠1,2,3, 李玺瑶1,2, 赵淑娟1,2, 杨朝1,2, 刘鑫1,2, 郭玲莉1,2, 王永明1,2, 郝义4, 张剑1,2, 胡梦颖1,2
Li Sanzhong1,2,3, Li Xiyao1,2, Zhao Shujuan1,2, Yang Zhao1,2, Liu Xin1,2, Guo Lingli1,2, Wang Yongming1,2, Hao Yi4, Zhang Jian1,2, Hu Mengying1,2
摘要：
华南早古生代加里东期变形、岩浆、沉积等特征表现为陆内造山带特征。通过对加里东期角度不整合分布、褶皱、断裂逆冲极性等特征的分析，发现大明山、大瑶山地区EW轴向的寒武系褶皱不对称性和角度不整合空间上向北的拓展变新规律，指示晚寒武世早奥陶世的由南向北推覆挤压可能是云开、滇桂北越地块依次向北推挤的结果；从全球背景看，可能和华南陆块南部一些地块与冈瓦纳大陆北缘依次碰撞接触导致的远程陆内效应有关。然而，湘赣边境、桂北元宝山及越城岭地区的早古生代NE向褶皱不对称性指示向西拓展，这可能是由于华夏地块与扬子地块在晚奥陶世早志留世沿郴州临武断裂陆内收缩挤压的结果，其全球背景可能和华南陆块顺时针旋转与冈瓦纳全面碰撞相关。总之，加里东期构造运动总体由南向北、由东向西渐新，变形强度由强到弱的特征，反映华南陆内碰撞造山事件的根本原因是其与冈瓦纳北缘碰撞的远程效应。450~420 Ma华南已经属于冈瓦纳北缘一部分。
中图分类号:
| [1] Li S Z, Zhao G C, Sun M, et al. Deformation History of the Paleoproterozoic Liaohe Assemblage in the Eastern Block of the North China Craton[J]. Journal of Asian Earth Sciences, 2005, 24(5): 659-674.[2] Wang X P, Peng P, Wang C, et al. Petrogenesis of the 2115 Ma Haicheng Mafic Sills From the Eastern North China Craton: Implications for an Intra-Continental Rifting[J]. Gondwana Research, 2016. in Press.[3] Hendrix M S, Dumitru T A, Graham S A. Late Oligocene-early Miocene Unroofing in the Chinese Tian Shan: An Early Effect of the India-Asia Collision[J]. Geology, 1994, 22(6): 487-90.[4] Cunningham W D. Lithospheric Controls on Late Cenozoic Construction of the Mongolian Altai[J]. Tectonics, 1998, 17(6): 891-902.[5] Li S Z, Guo L L, Xu L Q, et al. Coupling and Transition of Meso-Cenozoic Intracontinental Deformation Between the Taihang and Qinling Mountains[J]. Journal of Asian Earth Sciences, 2015, 114: 188-202.[6] Dong Y P, Yang Z, Liu X M, et al. Mesozoic Intracontinental Orogeny in the Qinling Mountains, Central China[J]. Gondwana Research, 2016, 30: 144-158.[7] 郝义, 李三忠, 金宠, 等. 湘赣桂地区加里东期构造变形特征及成因分析[J]. 大地构造与成矿学, 2010, 34(2): 166-180. Hao Yi, Li Sanzhong, Jin Chong, et al. Caledonian Structural Characteristics and Mechanism in Hunan-Jiangxi-Guangxi Provinces[J]. Geotectonicaet Metallogenia, 2010, 34(2): 166-180.[8] Wang Y J, Zhang F F, Fan W M, et al. Tectonic Setting of the South China Block in the Early Paleozoic: Resolving Intracontinental and Ocean Closure Models from Detrital Zircon U-Pb Geochronology[J]. Tectonics, 2010, 29(6): 1-70.[9] Charvet J, Shu L, Faure M, et al. Structural Development of the Lower Paleozoic Belt of South China: Genesis of an Intracontinental Orogen[J]. Journal of Asian Earth Sciences, 2010, 39(4): 309-330.[10] Song M J, Shu L S, Santosh M, et al. Late Early Paleozoic and Early Mesozoic Intracontinental Orogeny in the South China Craton: Geochronological and Geochemical Evidence[J]. Lithos, 2015, 232: 360-374.[11] Shu L S, Jahn B M, Charvet J, et al. Early Paleozoic Depositional Environment and Intraplate Tectono-Magmatism in the Cathaysia Block (South China): Evidence from Stratigraphic, Structural, Geochemical and Geochronological Investigation[J]. American Journal of Science, 2014, 314(1): 154-186.[12] Wang Y J, Fan W M, Sun M, et al. Geochronological, Geochemical and Geothermal Constraints on Petrogenesis of the Indosinian Peraluminous Granites in the South China Block: A Case Study in the Hunan Province[J]. Lithos, 2007, 96(3):475-502.[13] 舒良树, 周新民, 邓平, 等. 南岭构造带的基本地质特征[J]. 地质论评, 2012, 52(2): 251-265. Shu Liangshu, Zhou Xinmin, Deng Ping, et al. Principal Geological Features of Nanling Tectonic Belt South China[J]. Geological Review, 2012, 52(2): 251-265.[14] 张国伟, 郭安林, 王岳军, 等. 中国华南大陆构造与问题[J]. 中国科学: 地球科学, 2013, 43(10): 1553-1582. Zhang Guowei, Guo Anlin, Wang Yuejun, et al. Tectonics of South China Continent and Its Implications[J]. Science China: Earth Sciences, 2013, 43(10): 1553-1582.[15] Zhao G C. Jiangnan Orogen in South China: Developing from Divergent Double Subduction[J]. Gondwana Research, 2015, 27(3): 1173-1180.[16] Li X H, Su L, Chung S L, et al. Formation of the Jinchuan Ultramafic Intrusion and the World's Third Largest Ni-Cu Sulfide Deposit: Associated with the~825 Ma South China Mantle Plume?[J]. Geochemistry, Geophysics, Geosystems, 2005, 6(11): 1-16.[17] Li Z X, Bogdanova S V, Collins A S, et al. Assembly, Configuration, and Break-Up History of Rodinia: A Synthesis[J]. Precambrian Research, 2008, 160(1): 179-210.[18] Wang J, Li Z X. History of Neoproterozoic Rift Basins in South China: Implications for Rodinia Break-Up[J]. Precambrian Research, 2003, 122(1/2/3/4): 141-158.[19] Wang J, Mou C L. Neoproterozoic Rifting History of South China[J]. Gondwana Research, 2001, 4(4): 813-814.[20] 舒良树. 华南前泥盆纪构造演化: 从华夏地块到加里东期造山带[J]. 高校地质学报, 2006, 12(4): 418-431. Shu Liangshu. Predevonian Tectonic Evolution of South China: From Cathaysian Block to Caledonian Period Folded Orogenic Belt[J]. Geological Journal of China Universities, 2006, 12(4): 418-431.[21] Li Z X, Li X H. Formation of the 1 300 km Wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China: A Flat-Slab Subduction Model[J]. Geology, 2007, 35(2): 179-182.[22] 舒良树, 于津海, 贾东, 等. 华南东段早古生代造山带研究[J]. 地质通报, 2008, 27(10): 1581-1593. Shu Liangshu, Yu Jinhai, Jia Dong, et al. Early Paleozoic Orogenic Belt in the Eastern Segment of South China[J]. Geological Bulletin of China, 2008, 27(10):1581-1593.[23] 许靖华, 何起祥. 薄壳板块构造模式与冲撞型造山运动[J]. 中国科学:D辑, 1980, 10(11): 1081-1089. Xu Jinghua, He Qixiang. Model of Thin-Skinned Plate-Tectonics and Collision Orogeny[J]. Science China:Seris D, 1980,10 (11): 1081-1089.[24] 许靖华. 中国南方板块构造[J]. 广西地质, 1987(2): 1-9. Xu Jinghua. Plate Tectonics of Southern China[J]. Geology of Guangxi, 1987 (2): 1-9.[25] 刘宝珺, 许效松. 中国南方岩相古地理图集[M]. 北京:科学出版社, 1994: 10-11. Liu Baojun, Xu Xiaosong. Atlas of Lithofacies and Paleogeography of Southern China[M]. Beijing:Science Press, 1994: 10-11.[26] Wang H Z, Mo X X. An Outline of the Tectonic Evolution of China[J]. Episodes, 1995, 18(1/2): 6-16.[27] 蒲心纯, 周浩达, 王熙林, 等. 中国南方寒武纪岩相古地理与成矿作用[M]. 北京:地质出版社, 1993: 10-16. Pu Xinchun, Zhou Haoda, Wang Xilin, et al. Lithofacies Palaeogeography and Mineralization of the Cambrian in South China[M]. Beijing: Geological Publishing House, 1993: 10-16.[28] 殷鸿福, 吴顺宝, 杜远生, 等. 华南是特提斯多岛洋体系的一部分[J]. 地球科学, 1999, 24(1): 3-14. Yin Hongfu, Wu Shunbao, Du Yuansheng, et al. South China Defined as Part of Tethyan Archipelagle Ocean System[J]. Earth Science, 1999, 24(1): 3-14.[29] 尹福光, 许效松, 万方, 等. 华南地区加里东期前陆盆地演化过程中的沉积响应[J]. 地球学报, 2001, 22(5): 425-428. Yin Fuguang, Xu Xiaosong, Wan Fang, et al. The Sedimentary Response to the Evolutionary Process of Caledonian Foreland Basin System in South China[J]. Acta Geosicientia Sinica, 2001, 22(5): 425-428.[30] 万方, 尹福光, 许效松, 等. 华南加里东运动演化过程中烃源岩的成生[J]. 矿物岩石, 2003, 23(2): 82-86. Wan Fang, Yin Fuguang, Xu Xiaosong, et al. The Formation of Hydrocarbon Resources During the Evolution of China in Caledonian[J]. Journal of Mineralogy and Petrology, 2003, 23(2): 82-86.[31] 陈洪德, 侯明才, 许效松, 等. 加里东期华南的盆地演化与层序格架[J]. 成都理工大学学报(自然科学版), 2006, 33(1): 1-8. Chen Hongde, Hou Mingcai, Xu Xiaosong, et al. Tectonic Evolution and Sequence Stratigraphic Framework in South China During Caledonian[J]. Journal of Chengdu University of Technology(Science & Technology Edition), 2006, 33(1): 1-8.[32] Wang Y J, Wu C M, Zhang A M, et al. Kwangsian and Indosinian Reworking of the Eastern South China Block: Constraints on Zircon U-Pb Geochronology and Metamorphism of Amphibolites and Granulites[J]. Lithos, 2012, 150(5):227-242.[33] 郭福祥. 华南东部震旦志留纪大地构造属性[J]. 华南地质与矿产, 2000(1): 39-42. Guo Fuxiang. Sinian-Silurian Geotectonic Attribution of Southeast China[J]. Geology and Mineral Resources of South China, 2000(1): 39-42.[34] 杨森楠. 华南裂陷系的建造特征和构造演化[J]. 地球科学, 1989, 14(1): 29-36. Yang Sennan. The Formation Features and Tectonic Evolution of the South China Taphrogenic System[J]. Earth Science, 1989, 14(1): 29-36.[35] 刘宝珺, 许效松, 潘杏南, 等. 中国南方古大陆沉积地壳演化与成矿[M]. 北京:科学出版社, 1993: 9-124. Liu Baojun, Xu Xiaosong, Pan Xingnan, et al. Sedimentary Crustal Evolution and Metallization of South China Palaeocontinent[M]. Beijing: Science Press, 1993: 9-124.[36] 任纪舜. 论中国南部的大地构造[J]. 地质学报, 1990 (4): 275-288. Ren Jishun. On the Geotectonics of Southern China[J]. Acta Geological Sinica, 1990 (4): 275-288.[37] 戎嘉余, 陈旭. 华南晚奥陶世的动物群分异及生物相、岩相分布模式[J]. 古生物学报, 1987, 26(5): 507-535. Rong Jiayu, Chen Xu. Faunal Differentiation, Biofacies and Lithofacies Pattern of Late Ordovician(Ashgillian) in South China[J]. Acta Palaeontologica Sinica, 1987, 26(5): 507-535.[38] 陈旭, 戎嘉余, Rowley D B, 等. 对华南早古生代板溪洋的质疑[J]. 地质论评, 1995, 41(5): 389-400. Chen Xu, Rong Jiayu, Rowley D B, et al. Is the Early Paleozoic Banxi Ocean in South China Necessary?[J]. Geological Review, 1995, 41(5): 389-400.[39] 陈世悦, 张鹏飞, 杨怀宇. 湘西北江坪地区志留系风暴沉积特征及意义[J]. 古地理学报, 2009, 11(1): 51-57. Chen Shiyue, Zhang Pengfei, Yang Huaiyu. Silurian Storm Deposits in Jiangping Area, Northwestern Hunan Provice: Characteristic and Geological Significances[J]. Journal of Palaeogeography, 2009, 11(1): 51-57.[40] 张芳荣, 舒良树, 王德滋, 等. 华南东段加里东期花岗岩类形成构造背景探讨[J]. 地学前缘, 2009, 16(1): 248-260. Zhang Fangrong, Shu Liangshu, Wang Dezi, et al. Discussions on the Tectonic Setting of Caledonian Granitoids in the Eastern Segment of South China[J]. Earth Science Frontiers, 2009, 16(1): 248-260.[41] 陈旭, 张元动, 樊隽轩, 等. 广西运动的进程: 来自生物相和岩相带的证据[J]. 地球科学, 2012, 42(11): 1617-1626. Chen Xu, Zhang Yuandong, Fan Junxuan, et al. Onset of the Kwangsian Orogeny as Evidenced by Biofacies and Lithofacies[J]. Earth Sciences, 2012, 42(11): 1617-1626.[42] 王淼, 舒良树. 武夷山新元古代蛇绿混杂岩岩石地球化学特征[J]. 中国地质, 2007, 34(4): 572-583. Wang Miao, Shu Liangshu. Rock Geochemical Characteristics of the Neoproterozoic Wuyishan Ophiolite Mélange[J]. Geology in China, 2007, 34(4): 572-583.[43] Zheng Y F, Wu R X, Wu Y B, et al. Rift Melting of Juvenile Arc-Derived Crust: Geochemical Evidence from Neoproterozoic Volcanic and Granitic Rocks in the Jiangnan Orogen, South China[J]. Precambrian Research, 2008, 163(3): 351-383.[44] Li X H, Li Z X, Ge W, et al. Neoproterozoic Granitoids in South China: Crustal Melting Above a Mantle Plume at ca. 825 Ma?[J]. Precambrian Research, 2003, 122(1): 45-83.[45] 广西壮族自治区地质矿产局. 广西壮族自治区区域地质志[M]. 北京: 地质出版社, 1985: 656-657. Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonomous Region. Records of Regional Geology of Guangxi Zhuang Autonomous Region[M]. Beijing: Geological Publishing House, 1985: 656-657.[46] 杨树锋. 成对花岗岩带和板块构造[M]. 北京: 科学出版社, 1987: 1-98. Yang Shufeng. Granite Belt in Pairs and Plate Tectonics[M]. Beijing: Science Press, 1987: 1-98.[47] 丘元禧. 云开大山及其邻区构造演化[C]//云开大山及其邻区地质构造论文集. 北京: 地质出版社, 1993: 1-11. Qiu Yuanxi. The Tectonic Evolution of Yunkai Mountains and Its Adjacent Area[C]//Contribution on Geological Structure of Yunkai Mountains and Its Adjacent Area. Beijing: Geological Publishing House, 1993: 1-11.[48] 叶伯丹. 两广云开地区同位素地质年龄数据及其地质意义[J]. 广东地质, 1989, 4(3): 39-56. Ye Bodan. Isotopic Geochronological Data and Their Geological Significance in the Yunkai Area of Guangdong-Guangxi Provinces[J]. Guangdong Geology, 1989, 4(3): 39-56.[49] 劳秋元, 叶真华, 胡世玲, 等. 云开群硅质岩的40Ar/39Ar年龄及其地质意义[J]. 地球学报, 1997, 18(增刊): 98-101. Lao Qiuyuan, Ye Zhenhua, Hu Shiling, et al. The 40Ar/39Ar Age Data of Silicalite of Yunkai Group and Their Geological Significance[J]. Acta Geosicientia Sinica, 1997, 18(Sup.): 98-101.[50] 杨树锋, 陈汉林. 闽北早古生代岛弧火山岩的发现及其大地构造意义[J]. 地质科学, 1995, 30(2): 105-116. Yang Shufeng, Chen Hanlin. Discovery of Early Paleozoic Island-Arc Volcanic Rock in Northern Rate of Fujian Province and the Significance for Tectonic Study[J]. Science Geologica Sinica, 1995, 30(2): 105-116.[51] 舒良树, 卢华复, 贾东, 等. 华南武夷山早古生代构造事件的40Ar/39Ar同位素年龄研究[J]. 南京大学学报(自然科学), 1999, 35(6): 668-674. Shu Liangshu, Lu Huafu, Jia Dong, et al. Study of the 40Ar/39Ar Isotopic Age for the Early Paleozoic Tectonothermal Event in the Wuyishan Region, South China[J]. Journal of Nanjing University (Natural Sciences), 1999, 35(6): 668-674.[52] 朱清波, 黄文成, 孟庆秀, 等. 华夏地块加里东期构造事件: 两类花岗岩的锆石U-Pb 年代学和Lu-Hf 同位素制约[J]. 中国地质, 2015, 42(6): 1715-1739. Zhu Qingbo, Huang Wencheng, Meng Qingxiu, et al. Caledonian Tectonic Event of Cathaysia Block: Constraints on Zircon U-Pb Geochronology and Lu-Hf Isotope for Two Kinds of Granite[J]. Geology in China, 2015, 42(6): 1715-1739.[53] Chu Y, Lin W, Faure M, et al. Phanerozoic Tectonothermal Events of the Xuefengshan Belt, Central South China:Implications from U-Pb Age and Lu-Hf Determinations of Granites[J]. Lithos,2012,150:243-255.[54] Zhao K D, Jiang S Y, Sun T, et al. Zircon U-Pb Dating, Trace Element and Sr-Nd-Hf Isotope Geochemistry of Paleozoic Granites in the Miao'ershan-Yuechengling Batholith, South China: Implication for Petrogenesis and Tectonic-Magmatic Evolution[J]. Journal of Asian Earth Sciences,2013,16:1-20.[55] Zhang F F, Wang Y J, Zhang A M, et al. Geochronological and Geochemical Constraints on the Petrogenesis of Middle Paleozoic (Kwangsian) Massive Granites in the Eastern South China Block[J].Lithos,2012,150: 188-208.[56] Wang Y J, Zhang A M, Fan W M, et al. Kwangsian Crustal Anatexis Within the Eastern South China Block: Geochemical, Zircon U-Pb Geochronological and Hf Isotopic Fingerprints from the Gneissoid Granites of Wugong and Wuyi-Yunkai Domains[J]. Lithos, 2011, 127(1): 239-260.[57] Li Z X, Li X H, Wartho J A, et al. Magmatic and Metamorphic Events During the Early Paleozoic Wuyi-Yunkai Orogeny, Southeastern South China: New Age Constraints and Pressuretemperature Conditions[J]. Geological Society of America Bulletin,2010,122 (5/6):772-793.[58] Xu X B, Zhang Y Q, Shu L S, et al. La-ICP-MS U-Pb and 40Ar/39Ar Geochronology of the Sheared Metamorphic Rocks in the Wuyishan: Constraints on the Timing of Early Paleozoic and Early Mesozoic Tectono-Thermal Events in SE China[J]. Tectonophysics,2011,501:71-86.[59] 张爱梅, 王岳军, 范蔚茗, 等. 闽西南清流地区加里东期花岗岩锆石U-Pb 年代学及Hf 同位素组成研究[J]. 大地构造与成矿学, 2010, 34(3): 408-418. Zhang Aimei, Wang Yuejun, Fan Weiming, et al. LA-ICPMS Zircon U-Pb Geochronology and Hf Isotopic Compositions of Caledonian Granites from the Qingliu Area, Southwest Fujian[J].Geotectonica et Metallogenia, 2010, 34(3): 408-418.[60] 吴富江, 张芳荣. 华南板块北缘东段武功山加里东期花岗岩特征及成因探讨[J].中国地质,2003,3(2):166-172. Wu Fujiang, Zhang Fangrong. Features and Genesis of Caledonian Granites in the Wugongshan in the Eastern Segment of the Northern Margin of South China Plate[J]. Geology in China, 2003, 3(2):166-172.[61] 徐先兵, 张岳桥, 舒良树,等. 闽西南玮埔岩体和赣南菖蒲混合岩锆石La-ICPMS U-Pb 年代学: 对武夷山加里东运动时代的制约[J]. 地质论评, 2009,55(2):277-285. Xu Xianbing, Zhang Yueqiao, Shu Liangshu, et al. Zircon La-ICPMS U-Pb Dating of the Weipu Granitic Pluton in Southwest Fujian and the Changpu Migmatite in South Jiangxi: Constrains to the Timing of Caledonian Movement in Wuyi Mountains[J].Geological Review, 2009, 55(2): 277-285.[62] 黄标, 徐克勤, 孙志明, 等. 武夷山中段加里东早期交代改造型花岗岩类的特点及形成的碰撞造山环境[J]. 岩石学报, 1993, 9(3):388-400. Huang Biao, Xu Keqin, Sun Zhiming, et al. Features and Collosional Mountain Building Environment of Metasomatic Transformation Type Granitic Rocks in Middle Wuyi Mountains[J].Acta Peterologica Sinica, 1993, 9(3):388-400.[63] 陈正宏, 李寄嵎, 谢佩珊, 等. 利用EMP独居石定年法探讨浙闽武夷山地区变质基底岩石与花岗岩的年龄[J]. 高校地质学报,2008,14(1):1-15. Chen Zhenghong, Li Jiyu, Xie Peishan, et al. Approaching the Age Problem for Some Metamorphosed Precambrian Basement Rocks and Phanerozoic Granitic Bodies in the Wuyishan Area: The Application of EMP Monazite Age Dating[J]. Geological Journal of China Universities, 2008,14(1):1-15.[64] 王德滋, 周金城, 刘昌实, 等. 浙江桐庐自碎二长花岗斑岩的特征和成因[J]. 岩矿测试, 1982, 1(3): 15-25. Wang Dezi, Zhou Jincheng, Liu Changshi, et al. The Characteristics and the Origin of the Autoclastic Monzonitic Granite-Porphyry, Tonglu, Zhejiang[J]. Acta Petrologica Mineralogica et Analytica, 1982, 1(3): 15-25.[65] 莫柱孙. 南岭花岗岩地质学[M]. 北京:地质出版社, 1980: 1-50. Mo Zhusun. Granite Geology of Nanling[M]. Beijing:Geological Publishing House, 1980: 1-50.[66] 余开富, 王守德. 贵州南部的都匀运动及其古构造特征和石油地质意义[J]. 贵州地质, 1995, 12(3): 225-232. Yu Kaifu, Wang Shoude. Duyun Movement in South Guizhou Province and Its Paleostructure, and Their Significance in Petroleum Geology[J]. Guizhou Geology, 1995, 12(3): 225-232.[67] 卢华复. 赣南崇余山区前泥盆纪地层中角度不整合的发现及其意义[J]. 南京大学学报(地质学版) 1962 (1): 75-87. Lu Huafu. The Discovery of Angular Uncomformity in Predevonian Stratum in Chongyu Area, Southern Jiangxi and Its Significance[J]. Journal of Nanjing University(Geology), 1962 (1): 75-87.[68] Ting V K. The Orogenic Movements in China[J]. Bulletin of Geological Society of China, 1929, 8(2): 151-170.[69] 吴浩若. 重新解释广西运动[J]. 科学通报, 2000, 45(5): 555-558. Wu Haoruo. Reexplain the Guangxi Movement[J]. Chinese Science Bulletin, 2000, 45(5): 555-558.[70] Li S Z, Santosh M, Zhao G C, et al. Intracontinental Deformation in a Frontier of Super-Convergence: A Perspective on the Tectonic Milieu of the South China Block[J]. Journal of Asian Earth Sciences, 2012, 49: 313-329.[71] 刘博, 李三忠, 周永刚, 等. 桂北河池—宜州断裂带构造特征及其演化: 柳城段浅部到深部结构的启示[J]. 大地构造与成矿学, 2009, 33(4): 488-496. Liu Bo, Li Sanzhong, Zhou Yonggang, et al. Structural Features and Evolution of the Hechi-Yizhou Fault Zone, Northern Guangxi-Insights from Shallow to Deep Structures of Its Liucheng Segment[J]. Geotectonica et Metallogenia, 2009, 33(4): 488-496.[72] 汤世凯, 马筱, 杨坤光, 等. 黔东桂北加里东期两类构造变形特征与成因机制探讨[J]. 现代地质, 2014, 28(1): 109-118. Tang Shikai, Ma Xiao, Yang Kunguang, et al. Characteristics and Genesis of Two Types of Tectonic Deformation During Caledonian in Eastern Guizhou and Northern Guangxi[J]. Geoscience, 2014, 28(1): 109-118.[73] 邵建国, 彭少梅, 彭松柏. 云开地区前海西期构造演化的同位素年代学特征[J]. 广东地质, 1995, 10(2): 41-50. Shao Jianguo, Peng Shaomei, Peng Songbo. Isotopic Geochronology of Prevariscan Tectonic Evolution of Yunkai Area[J]. Guangdong Geology, 1995, 10(2): 41-50.[74] 彭少梅, 伍广宁. 云开地块的构造演化史及其动力学特征[J]. 广东地质, 1996, 11(2): 39-45. Peng Shaomei, Wu Guangning. Tectonic Evolutionary History and Dynamic Features of Yunkai Block[J]. Guangdong Geology, 1996, 11(2): 39-45.[75] 张国伟, 孟庆任, 于在平, 等. 秦岭造山带的造山过程及其动力学特征[J]. 中国科学, 1996, 26(3): 193-200. Zhang Guowei, Meng Qingren, Yu Zaiping, et al. Orogeny and Dynamic Characteristics of the Qinling Orogenic Belt[J]. Science in China, 1996, 26(3): 193-200.[76] 陈旭, 米切尔 C E. 塔康运动与广西运动的地层学证据[J]. 地层学杂志, 1996, 20(4): 305-324. Chen Xu, Mitchell C E. Stratigraphic Evidences on Taconican and Guangxi Orogeny[J]. Journal of Stratigraphy, 1996, 20(4): 305-324.[77] 白忠峰. 桂中坳陷构造特征及其与油气关系[D]. 北京:中国地质大学, 2006: 20-22. Bai Zhongfeng. Struetura1 Characteristics and the Relation with the Petruleum and Gas in Guizhong Depression[D]. Beijing: China University of Geosciences , 2006: 20-22.[78] 张鹏飞. 中扬子地区古生代构造古地理格局及其演化[D]. 北京: 中国石油大学, 2009: 121-147. Zhang Pengfei. Pattern and Evolution of Paleozoic Tectono-Palaeogeography in the Middle Yangtze Region[D]. Beijing: China University of Petroleum, 2009: 121-147.[79] Guo L Z, Shi Y S, Lu H F, et al. The Pre-Devonian Tectonic Patterns and Evolution of South China[J]. Journal of Southeast Asian Earth Science, 1989, 3(1/2/3/4): 87-93.[80] 郝杰, 杨美芳, 李继亮. 东南地区磨拉石地层及其大地构造意义[M]//李继亮.东南大陆岩石圈结构与地质演化. 北京: 冶金工业出版社, 1993: 55-58. Hao Jie,Yang Meifang,Li Jiliang.The Molasse Formation and Geotectonic Significance in Southeast China[M]//Li Jiliang.The Sructure of Continental Lithosphere and Geological Evolution of Southeast China. Beijing: Metallurgical Industry Press, 1993: 55-58.[81] 龚由勋, 孙存礼. 赣西南加里东造山带磨拉石相沉积的发现[J]. 中国区域地质, 1996(2): 108-113. Gong Youxun, Sun Cunli. The Discovery of Molasse Facies Deposits of the Caledonides in South Western Jiangxi[J]. Regional Geology of China, 1996(2): 108-113.[82] 陈旭, 戎嘉余. 从生物地层学到大地构造学: 以华南奥陶系和志留系为例[J]. 现代地质, 1999, 13(4): 385-388. Chen Xu, Rong Jiayu. From Biostratigraphy to Tectonics: With Ordovician and Silurian of South China as an Example[J]. Geoscience, 1999, 13(4): 385-388.[83] 吴浩若. 广西加里东运动构造古地理问题[J]. 古地理学报, 2000, 2(1): 70-76. Wu Haoruo. A Discussion on the Tectonic Palaeogeography Related to the Caledonian Movement in Guangxi[J]. Journal of Palaeogeography, 2000, 2(1): 70-76.[84] Burrett C, Zaw K, Meffre S, et al. The Configuration of Greater Gondwana: Evidence from LA ICPMS, U-Pb Geochronology of Detrital Zircons from the Palaeozoic and Mesozoic of Southeast Asia and China[J]. Gondwana Research, 2014, 26(1):31-51.[85] Wilde S A. Evolution of the Western Margin of Australia During the Rodinian and Gondwanan Supercontinent Cycles[J]. Gondwana Research, 1999, 2(3): 481-499.[86] Wilde S A, Zhang X Z, Wu F Y. Extension of a Newly Identified 500 Ma Metamorphic Terrane in North East China: Further U-Pb SHRIMP Dating of the Mashan Complex, Heilongjiang Province, China[J]. Tectonophysics, 2000, 328(1/2): 115-30.[87] Wilde S A, Wu F Y. The Mashan Complex: SHRIMP U-Pb Zircon Evidence for a Late Pan-African Metamorphic Event in NE China and Its Implication for Global Continental Reconstructions[J]. Geochimica, 2001 , 30(1): 35-50.[88] Wilde S A, Zhou X, Nemchin A A, et al. Mesozoic Crust-Mantle Interaction Beneath the North China Craton: A Consequence of the Dispersal of Gondwanaland and Accretion of Asia[J]. Geology, 2003, 31(9): 817-820.[89] Zhou J B, Wilde S A, Zhao G C, et al. Pan-African Metamorphic and Magmatic Rocks of the Khanka Massif, NE China: Further Evidence Regarding Their Affinity[J]. Geological Magazine, 2010, 147(5): 737-749.[90] Zhou J B, Wilde S A, Zhao G C, et al. New SHRIMP U-Pb Zircon Ages from the Heilongjiang High-Pressure Belt: Constraints on the Mesozoic Evolution of NE China[J]. American Journal of Science, 2010, 310(9): 1024-1053.[91] Wilde S A, Zhou J B. The Late Paleozoic to Mesozoic Evolution of the Eastern Margin of the Central Asian Orogenic Belt in China[J]. Journal of Asian Earth Sciences, 2015, 113: 909-921.[92] Isozaki Y, Itaya T. Pre-Jurassic Klippe in Northern Chichibu Belt in West-Central Shikoku, Southwest Japan:Kurosegawa Terrane as a Tectonic Outlier of the Pre-Jurassic Rocks of the Inner Zone[J]. Journal of the Geological Society of Japan, 1991, 97(431): 50.[93] Isozaki Y, Kase T. The Occurrence of the Large Gastropod "Pleurotomaria"Yokoyamai Hayasaka from the Capitanian (Permian) Iwaizaki Limestone in Northeast Japan[J]. Paleontological Research, 2014, 18(4): 250-257.[94] Isozaki Y, Aoki K, Nakama T, et al. New Insight into a Subduction-Related Orogen: A Reappraisal of the Geotectonic Framework and Evolution of the Japanese Islands[J]. Gondwana Research, 2010, 18(1): 82-105.[95] Isozaki Y, Maruyama S, Nakama T, et al. Growth and Shrinkage of an Active Continental Margin: Updated Geotectonic History of the Japanese Islands[J]. Journal of Geography, 2011, 120(1): 65-99.[96] Isozaki Y, Aoki K, Sakata S, et al. The Eastern Extension of Paleozoic South China in NE Japan Evidenced by Detrital Zircon[J]. GFF, 2014, 136(1): 116-119.[97] Aoki K, Isozaki Y, Yamamoto A, et al. Mid-Paleozoic Arc Granitoids in SW Japan with Neoproterozoic Xenocrysts from South China: New Zircon U-Pb Ages by LA-ICP-MS[J]. Journal of Asian Earth Sciences, 2015, 97: 125-135.[98] 白立新, 朱日祥, 郭斌, 等. 扬子地块中寒武世古地磁新结果[J]. 中国科学: D辑, 1998(增刊1): 57-62. Bai Lixin, Zhu Rixiang, Guo Bin, et al. New Paleomagnetic Result from the Middle Cambrian in the Southern Yangtze Block[J]. Science in China: Series D, 1998(Sup.1): 57-62.[99] 朱日祥, 杨振宇, 吴汉宁, 等. 中国主要地块显生宙古地磁视极移曲线与地块运动[J]. 中国科学:D辑, 1998, 28(增刊):1-16. Zhu Rixiang, Yang Zhenyu, Wu Hanning, et al. The Apparent Polar Wander Paths of Paleomagnetismand Block Movementof Major Blocks in China Since Phanerozoic[J]. Science in China: Series D, 1998, 28(Sup.):1-16.[100] 张伯友, 俞鸿年. 粤西海西印支碰撞带深层次推覆构造[M]. 北京: 地质出版社, 1994: 120-122. Zhang Boyou, Yu Hongnian. The Deep-Level Nappe Structureof Collision Belt from Hercynian to Indosinian Epoch in Weatern Guangdong[M]. Beijing: Geological Publishing House, 1994: 120-122.[101] 吴浩若, 邝国敦, 王忠诚. 志留纪以来的云开地块[J]. 古地理学报, 2001, 3(3): 32-40. Wu Haoruo, Kuang Guodun, Wang Zhongcheng. The Yunkai Block Since Silurian[J]. Journal of Palaeogeography, 2001, 3(3): 32-40.[102] 白立新, 朱日祥. 扬子地块古生代大地构造演化及古地磁学研究综述[J]. 地球物理学进展, 1996, 11(3): 109-116. Bai Lixin, Zhu Rixiang. A Review of the Tectonic Evolution and Paleomagnetic Research for the Yangtze Block During Paleozoic[J]. Progress in Geophysics, 1996, 11(3): 109-116.[103] 舒良树. 华夏古陆探讨[C]//中国古陆块构造演化与超大陆旋回专题学术会议论文集. 北京:北京大学,2000: 37-38. Shu Liangshu. Discussion on the Cathaysian Oldland[C]//Conference Proceedings of Tectonic Evolution of Chinese Paleo-Continental Block and Supercontinent Cycle. Beijing: Peking University, 2000: 37-38. |
| [1] | 贾莹刚, 赵军, 蒋磊, 关力伟, 王小玄, 何亮. 伊犁地块北缘早古生代构造属性:来自温泉地区闪长岩的证据[J]. 吉林大学学报(地球科学版), 2019, 49(4): 1015-1038. |
| [2] | 赵希林, 姜杨, 邢光福, 于胜尧, 彭银彪, 黄文成, 王存智, 靳国栋. 陈蔡早古生代俯冲增生杂岩对华夏与扬子地块拼合过程的指示意义[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1135-1153. |
| [3] | 齐忠友, 冯志强, 温泉波, 张铁安, 刘宾强, 李小玉, 杜兵盈. 东北地区嫩江东北部早古生代闪长岩的成因探讨:锆石U-Pb年代学和地球化学证据[J]. 吉林大学学报(地球科学版), 2017, 47(1): 113-125. |
| [4] | 李三忠, 杨朝, 赵淑娟, 李玺瑶, 索艳慧, 郭玲莉, 余珊, 戴黎明, 李少俊, 牟墩玲. 全球早古生代造山带(Ⅱ):俯冲-增生型造山[J]. 吉林大学学报(地球科学版), 2016, 46(4): 968-1004. |
| [5] | 李三忠, 杨朝, 赵淑娟, 刘鑫, 余珊, 李玺瑶, 郭玲莉, 索艳慧, 戴黎明, 郭润华, 张国伟. 全球早古生代造山带(Ⅳ): 板块重建与Carolina超大陆[J]. 吉林大学学报(地球科学版), 2016, 46(4): 1026-1041. |
| [6] | 李三忠, 杨朝, 赵淑娟, 李玺瑶, 郭玲莉, 余珊, 刘鑫, 索艳慧, 兰浩圆. 全球早古生代造山带(Ⅰ):碰撞型造山[J]. 吉林大学学报(地球科学版), 2016, 46(4): 945-967. |
| [7] | 曹颖, 王建, 刘建国, 包真艳, 宋樾, 李爱. 西昆仑早古生代岩浆弧大同岩体中埃达克质岩石的成因及地质意义[J]. 吉林大学学报(地球科学版), 2016, 46(2): 425-442. |
| [8] | 周建波, 曾维顺, 曹嘉麟, 韩杰, 郭晓丹. 中国东北地区的构造格局与演化：从500 Ma到180 Ma[J]. J4, 2012, 42(5): 1298-1316. |
| [9] | 李三忠, 王涛, 金宠, 戴黎明, 刘鑫, 周小军, 王岳军, 张国伟. 雪峰山基底隆升带及其邻区印支期陆内构造特征与成因[J]. J4, 2011, 41(1): 93-105. |
| [10] | 覃小锋，夏 斌，李 江，黎春泉，陆济璞，许 华，周府生，胡贵昂，李 乾. 阿尔金南缘构造带西段新元古代-早古生代变质岩系的变质作用[J]. J4, 2007, 37(5): 856-0867. |
| [11] | 刘建峰，迟效国，周燕，王铁夫，金巍，周建波，董春艳，黎广荣. 小兴安岭东北部金林岩体全岩-角闪石Rb-Sr年龄[J]. J4, 2005, 35(06): 690-0693. |
|