A tentative discussion on some tectonic problems in the east of South China continent
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摘要:
华南大陆的结构、属性、过程与动力学一直是地质学家关注的热点。本文以钦杭构造带东段为主要研究地区,通过精细的构造解析、变质变形研究、年代学分析,结合反射地震剖面,探讨了华南大陆东部几个科学问题。(1)江南造山带形成于新元古代华夏板块与扬子板块的“软碰撞”作用,可划分为扬子板块南缘、扬子—华夏汇聚带和华夏板块北缘3个构造单元,江南断裂带和武夷山—遂昌断裂带分别为江南造山带的北界和南界。(2)扬子—华夏板块汇聚带由多个小板块拼合而成,其间有多条缝合带,大约900 Ma开始汇聚,760 Ma全面闭合,850~780 Ma为活动高峰期,具有递变式的汇聚拼合过程,由南向北发展,先斜向俯冲,后右旋走滑,最晚集中在中部活动。(3)华南大陆东部为中生代奠定的构造格架,主要构造为一系列北东走向褶皱和逆冲断层,大量地壳范围内的叠瓦状逆冲推覆构造,由南向北逆冲,可下切到中—下地壳。(4)华南大陆燕山晚期区域性伸展构造广泛发育,存在“华南热隆”构造,震旦系内的滑覆构造典型,同期大规模岩浆活动、火山活动和大规模的热液成矿。(5)华南大陆构造演化为:850 Ma扬子—华夏板块递进式汇聚,760 Ma全面拼合,江南造山带形成;600 Ma华南大陆盖层发育;430 Ma钦杭构造带受南部构造影响;220 Ma钦杭构造带受北部远程构造影响;160 Ma逆冲推覆构造产生;140 Ma大规模伸展,构造-岩浆-成矿关系密切;随后江南持续隆升,华南强烈热隆。
Abstract:The structure, properties, processes and dynamics of the south China continent have always been the focus among geologists. In this paper, the eastern part of the Qinghang tectonic belt was taken as the main research area. Based on detailed structural analysis, metamorphism and deformation research, chronology analysis and reflection seismic profile, the authors investigated several scientific problems in the eastern part of the south China continent. (1) The Jiangnan orogenic belt was formed by the "soft collision" between the Cathaysia plate and the Yangtze plate in late Proterozoic, which can be divided into three tectonic units:the southern margin of the Yangtze plate, the Yangtze-Cathaysia convergence belt and the northern margin of the Cathaysia plate. The Jiangnan fault belt and The Wuyishan-Suichang fault belt are the northern and southern boundary of the Jiangnan orogenic belt, respectively. (2) The Yangtze-Cathaysia convergence belt is composed of several small plates and suture zones. The convergence between them was progressive from south to north. It was shown as oblique subduction at first, followed by dextral strikeslipping, and the activity was concentrated in the middle at the latest. It began at about 900 Ma, reached its climax in 850~780 Ma and was closed completely at about 760 Ma. (3) The tectonic framework of the east of South China continent was established in the Mesozoic. The main structure was a series of NE-striking folds and thrust faults. A large number of imbricated thrusting nappe structures with thrusting movement from south to north originated from the middle-lower crust scale. (4) The regional extensional structures were widely developed in the east of the South China continent in late Yanshanian which led to the formation of "the South China thermal upwelling". It developed typical sliding nappe structures in the Sinian strata. The large-scale magmatic activity, volcanic activity and large-scale hydrothermal mineralization took place at the same time. (5) The tectonic evolution of the South China continent is as follows:The peak of progressive convergence between the Yangtze-Cathaysia plate took place at about 850 Ma. Plates were closed completely and the Jiangnan orogenic belt was formed at about 760 Ma. Then the development of cover of South China continent began at 600 Ma. The Qinhang tectonic belt was affected by the southern structure and the remote effect of the north structures at 430 Ma and 220 Ma, respectively. Thrust nappe structure was widely developed at 160 Ma, while widespread extensional structures was developed at 140 Ma. The tectonic-magma-mineralization had close relationship. Then the Jiangnan belt continued to uplift and the South China became a thermo-upwelling.
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Charvet J, Shu L S, Shi Y S, Guo L Z, Faure M. 1996. The building of south China:collision of Yangzi and Cathaysia blocks, problems and tentative answers[J]. Journal of Asian Earth Sciences, 13(3/5):223-235. http://cn.bing.com/academic/profile?id=d166d38bc0de52efc8172709e658b04d&encoded=0&v=paper_preview&mkt=zh-cn
Cheng Guanghua, Wang Yinggeng. 2000. The strcutura dramework of the eastern section of Jiangnan orogen[J]. Anhui Geology, 1-8 (in Chinese with English abstract).
Deng Guohui, Liu Chungen, Feng Ye. 2005. Tectonic Features and Evolution of the Proterozoic Orogenic Belt between Northeastern Jiangxi and Southern Anhui[J]. Acta Geoscientica Sinica, 26(1):9-16 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200501002
Gao J, Klemd R, Long L L, Xiong X M, Qian Q. 2008. Adakitic signature formed by fractional crystallization:An interpretation for the Neo-Proterozoic meta-plagiogranites of the NE Jiangxi ophiolitic mélange belt, South China[J]. Bulletin of Mineralogy Petrology and Geochemistry, 110(s1):277-293. http://cn.bing.com/academic/profile?id=92c6d1f6eb35e57b6a89f056b4358808&encoded=0&v=paper_preview&mkt=zh-cn
Gao Linzhi, Liu Yanxue, Ding Xiaozhong, Zhang Chuanheng, Wang Ziqiang, Chen Jun, Liu Yaorong. 2012. SHRIMP dating of Cangshuipu in the middle part of the Jiangnan Orogen and its implication for tectonic evolutions[J]. Geology in China, 12-20 (in Chinese with English abstract).
Greentree M R, Li Z X, Li X H, Wu H C. 2006. Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia[J]. Precambrian Research, 151(1/2):79-100. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-j.precamres.2006.08.002/
Guo Lingzhi, Shi Yangshen, Ma Ruishi, Ye Shangfu, Lu Huafu. 1984.Tectonsratigrahic terranes of southeast China[J]. Journal of Nanjing University (Natural Science), 20(4):130-137 (in Chinese with English abstract).
Haynes S J. 1990. Structural Reconnaissance of the Jiangnan Geanticline: A Suspect Terrane of Compressional Tectonic Character[M].
Hsü K J, Li J L, Chen H H, Wang Q C, Sun S, Sengor A M C. 1990.Tectonics of South China:Key to understanding West Pacific geology[J]. Tectonophysics, 183(1):9-39. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-0040-1951(90)90186-C/
Hsü K J, Sun S, Li J L, Chen H H, Pen H P, Sengor A M C. 1988.Mesozoic overthrust tectonics in south China[J]. Geology, 16(5):418-421. doi: 10.1130/0091-7613(1988)016<0418:MOTISC>2.3.CO;2
Li Jianghai, Mu Jian. 1999. Tectonic constraints from Chinese Cratonic Blocks for the reconstruction of Rodinia[J]. Chinese Journal of Geology, 259-272 (in Chinese with English abstract).
Li L M, Lin S F, Xing G F, Davis D W, Jiang Y, Davis W, Zhang Y J. 2016. Ca. 830 Ma back-arc type volcanic rocks in the eastern part of the Jiangnan orogen:Implications for the Neoproterozoic tectonic evolution of South China Block[J]. Precambrian Research, 275:209-224. doi: 10.1016/j.precamres.2016.01.016
Li W X, Li X H, Li Z X. 2008. Middle Neoproterozoic syn-rifting volcanic rocks in Guangfeng, South China:Petrogenesis and tectonic significance[J]. Geological Magazine, 145(4):475-489. doi: 10.1017/S0016756808004561
Li X H, Li W X, Li Z X, Lo C H, Wang J, Ye M F, Yang Y H. 2009.Amalgamation between the Yangtze and Cathaysia Blocks in South China:Constraints from SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu volcanic rocks[J]. Precambrian Research, 174(1):117-128. http://cn.bing.com/academic/profile?id=959853511f4100fdd7f5f258a2dac3ff&encoded=0&v=paper_preview&mkt=zh-cn
Li X H, Li Z X, Ge W C, Zhou H W, Li W X, Liu Y, Wingate M T D. 2003. Neoproterozoic granitoids in South China:crustal melting above a mantle plume at ca. 825 Ma?[J]. Precambrian Research, 122(1/4):45-83. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-S0301-9268(02)00207-3/
Li X H, Zhao J X, Mcculloch M T, Zhou G Q, Xing F M. 1998.Geochemical and Sm-Nd isotopic study of Neoproterozoic ophiolites from southeastern China:Petrogenesis and tectonic implications[J]. Precambrian Research, 81(1/2):129-144. https://www.sciencedirect.com/science/article/pii/S0301926896000320
Li Xianhua, Li Wuxian, He Bing. 2012. Building of the South China Block and its relevance to assembly and breakup of Rodinia supercontinent:observations, jnterpretations and tests[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 31(6)543-559 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=6a1e4e2f209d3b50381daf40cd48123a&encoded=0&v=paper_preview&mkt=zh-cn
Li Xianhua, Wang Yixian, Zhao Zhenhua, Chen Duofu. 1998.SHRIMP U-Pb Zircon Geochronology for amphibolite from the Precambrian basement in SW Zhejiang and NW Fujian Province[J]. Geochimica, 27(4):327-334 (in Chinese with English abstract).
Li Xianhua. 2000. Geochemical characteristics and tectonic significance of siliceous rocks in the ophiolite melange belt of Northeast Jiangxi[J]. Science in China (Series D), 30(3):284-290(in Chinese with English abstract).
Li Yuan, Xie Hangqiang, Song Zhirui. 2017. SHRIMP U-Pb Zircon Ages of the Northeastern Jiangxi Ophiolites and the Zhangcun Group and a Discussion on the Tectonic Evolution of the Jiangnan Orogen[J]. Geological Review, 63(4):854-868 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201704002
Li Z X, Li X H, Kinny P D, Wang J, Zhang S, Zhou H. 2003.Geochronology of Neoproterozoic syn-rift magmatism in the Yangtze Craton, South China and correlations with other continents:evidence for a mantle superplume that broke up Rodinia[J]. Precambrian Research, 122(1/4):85-109. http://cn.bing.com/academic/profile?id=f37b2e324eb8eddd96446f3e3d501681&encoded=0&v=paper_preview&mkt=zh-cn
Li Z X, Li X H, Wartho J A, Clark C, Li W X, Zhang C L, Bao C. 2010. Magmatic and metamorphic events during the Early Paleozoic Wuyi-Yunkai orogeny, southeastern South China:New age constraints and Pressure-temperature conditions[J]. GSA Bull., 122:772-793. doi: 10.1130/B30021.1
Li Z X, Li X H, Zhou H W, Kinny P D. 2002. Grenvillian continental collision in south China:New SHRIMP U-Pb zircon results and implications for the configuration of Rodinia[J]. Geology, 30(2):163-166. http://cn.bing.com/academic/profile?id=f5261d0e7ca878742e27aff0501c1a9a&encoded=0&v=paper_preview&mkt=zh-cn
Lin W, Faure M, Monié P, SchäRer Urs, Zhang L S, Sun Y. 2000.Tectonics of SE China:New insights from the Lushan massif(Jiangxi Province)[J]. Tectonics, 19(5):852-871. doi: 10.1029/2000TC900009
Mao Jinwen, Chen Maohong, Yuan Shunda, Guo Chunli. 2011.Geological Characteristics of the Qinhang (or Shihang) Metallogenic Belt in South China and Spatial-Temporal Distribution Regularity of Mineral Deposits[J]. Acta Geologica Sinica, 85(5):636-658 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=2d160079e40c461e3997fb4697306618&encoded=0&v=paper_preview&mkt=zh-cn
Shu Liangshu, Lu Huafu, Jia Dong, Charvet Jacques, Faure Michel. 1999. 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 Science), 35(5):668-674(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900493792
Shu Liangshu, Shi Yangshen, Guo Lingzhi. 1995. Plate-body Tectonics and Collision Orogeny in the Middle of Jiangnan Orogen[M]. Nanjing:Nanjing University Press (in Chinese with English abstract).
Shu Liangshu, Xiang Lei, Yao Jinlong. 2012. An analysis of principlal features of tectonic evolution in South China Block[C]//Symposium on Tectonic Geology and Geodynamics (in Chinese).
http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201207004.htm Wan Y S, Liu D Y, Xu M H, Zhuang J M, Song B, Shi Y R, Du L L. 2007. SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in Northwestern Fujian, Cathaysia block, China:Tectonic implications and the need to redefine lithostratigraphic units[J]. Gondwana Research, 12:166-183. doi: 10.1016/j.gr.2006.10.016
Wang Chunzhi, Xing Guangfu, Yu Minggang, Huang Zhizhong, Hong Wentao, Zhao Xilin, Zhou Xiaohua, Duan Zheng, Jü Dongmei. 2015. Timing and tectonic of the ophiolite in northeast Jiangxi:Constrains from zircon U-Pb age, Hf isotope and geochemistry of the Zhangshudun gabbro[J]. Acta Petrologica et Mineralogica, 34(3):309-321 (in Chinese with English abstract).
Wang X L, Zhao G C, Zhou J C, Liu Y S, Hu J. 2008. Geochronology and Hf isotopes of zircon from volcanic rocks of the Shuangqiaoshan Group, South China:Implications for the Neoproterozoic tectonic evolution of the eastern Jiangnan orogen[J]. Gondwana Research, 14(3):355-367. doi: 10.1016/j.gr.2008.03.001
Wang X L, Zhou J C, Griffin W L, Wang R C, Qiu J S, O'Reilly S Y, Xu X S, Liu X M, Zhang G L. 2007. Detrital zircon geochronology of Precambrian basement sequences in the Jiangnan orogen:Dating the assembly of the Yangtze and Cathaysia Blocks[J]. Precambrian Research, 159(1):117-131. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-j.precamres.2007.06.005/
Wang Xiaolei, Zhou Jincheng, Chen Xin, Zhang Fengfeng, Sun Ziming. 2017. Formation and evolution of the Jiangnan orogen[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 36(5):714-735 (in Chinese with English abstract).
Wang Ziqiang, Gao Linzhi, Ding Xiaozhong, Huang Zhizhong. 2012.Tectonic environment of the, metamorphosed basement in the Jiangnan orogen and its evolutional features[J]. Geological Review, 58(3):401-413 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000003559
Xin Y J, Li J H, Dong S W, Zhang Y Q, Wang W B, Sun H S. 2017.Neoproterozoic post-collisional extension of the central Jiangnan Orogen:Geochemical, geochronological, and Lu-Hf isotopic constraints from the ca. 820-800 Ma magmatic rocks[J]. Precambrian Research, 294:91-110. doi: 10.1016/j.precamres.2017.03.018
Xing Fengming, Xu Xiang. 1992. Sm-Nd isotopic age of proterozoic ophiolites in northeastern Jiangxi and its geological significance[J]. Acta Petrologica et Mineralogica, 11(2):120-124 (in Chinese with English abstract).
Xu Bei. 1990. The Late proterozoic trech-basin-arc system in northeastern Jiangxi-southern Anhui Provinces[J]. Acta Geologica Sinica, 64(1):33-42 (in Chinese with English abstract).
Xu Xianbing, Tang Shuai, Li Yuan, Zhang Zejun. 2015. Characteristics of Neoproterozoic-early Mesozoic multiphase orogenic activities of eastern Jiangnan Orogen[J]. Geology in China, 42(1):33-50 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi2015010004
Xue Huaiming, Ma Fang, Song Yongqin, Xie Yaping. 2010.Geochronology and geochemisty of the Neoproterozoic granitoid association from eastern segment of the Jiangnan orogen. China:Constraints on the ttaling and process of amalgamation between the Yangtze and Cathaysia blocks[J]. Acta Prtrologica Sinica, 26(11):3215-3244 (in Chinese with English abstract). https://www.researchgate.net/publication/279629265_Geochronology_and_geochemisty_of_the_Neoproterozoic_granitoid_association_from_eastern_segment_of_the_Jiangnan_orogen_China_Constraints_on_the_timing_and_process_of_amalgamation_between_the_Yangtze_an
Yang Minggui, Huang Shuibao, Lou Fasheng, Tang Weixin, Mao Subin. 2009. Lithospheric structure and large-scale metallogenic process in Southeast China continental area[J]. Geology in China, 36(3):528-543 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200903004
Ye M F, Li X H, Li W X, Liu Y, Li Z X. 2007. SHRIMP zircon U-Pb geochronological and whole-rock geochemical evidence for an early Neoproterozoic Sibaoan magmatic arc along the southeastern margin of the Yangtze Block[J]. Gondwana Research, 12(1/2):144-156. http://d.old.wanfangdata.com.cn/NSTLQK/10.1016-j.gr.2006.09.001/
Yin C Q, Lin S, Davis D W, Xing G F, Davis W J, Cheng G H, Xiao W J, Li L M. 2013. Tectonic evolution of the southeastern margin of the Yangtze Block:Constraints from SHRIMP U-Pb and LAICP-MS Hf isotopic studies of zircon from the eastern Jiangnan Orogenic Belt and implications for the tectonic interpretation of South China[J]. Precambrian Research, 236(5):145-156. https://www.sciencedirect.com/science/article/pii/S0301926813002337
Zhang C L, Santosh M, Zou H B, Li H K, Huang W C.2013. The Fuchuan ophiolite in Jiangnan Orogen:Geochemistry, zircon U-Pb geochronology, Hf isotope and implications for the Neoproterozoic assembly of South China[J]. Lithos, 179(10):263-274. http://cn.bing.com/academic/profile?id=a3104e99659c02c5052afea28ccc8b6f&encoded=0&v=paper_preview&mkt=zh-cn
Zhang C L, Zou H B, Zhu Q B, Chen X Y. 2015. Late Mesoproterozoic to early Neoproterozoic ridge subduction along southern margin of the Jiangnan Orogen:New evidence from the Northeastern Jiangxi Ophiolite (NJO), South China[J]. Precambrian Research, 268:1-15. doi: 10.1016/j.precamres.2015.07.005
Zhang Guowei, Guo Anlin, Wang Yuejun, Li Sanzhong, Dong Yunpeng, Liu Shaofeng, He Dengfa, Cheng Shunyou, Lu Rukui, Yao Anping. 2013. Structure and problems of south China continent[J]. Scientia Sinica Terrae, 1553-1582 (in Chinese with English abstract).
Zhao Jianxin, Li Xianhua, M T McCulloch, Zhou Guoqing, Xing Fengming. 1995. Peteogenesis of ophilites from south Ahui and northeast Jiangxi, and their tectonic implications:Chemical and Sm-Nd isotopic constraints[J]. Geochimica, 24(4):311-326 (in Chinese with English abstract).
Zhou Jincheng, Wang Xiaolei, Qiu Jiansheng. 2009. Some Neoproterozoic geological events involved in the development of the Jiangnan orogen[J]. Geological Journal of China Universities, 15(4):453-459 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200904003
Zhou Xinmin, Wang Dezi. 1988. The peraluminous granodiorites with low initial 87Sr/86Sr ration and their genesis in southern Anhui province, eastern China[J]. Acta Petrologica Sinica, 51(3):2141-2145 (in Chinese with English abstract). http://www.oalib.com/paper/1469151
Zhou Xinmin, Yang Jiedong. 1989. Sm-Nd isochron age and its geological significance of ophiolite suite in fuchuan, Shexian Anhui province[J]. Chinese Science Bulletin, 16:1243-1245 (in Chinese with English abstract). https://link.springer.com/article/10.1360%2F02tb9415
程光华, 汪应庚. 2000.江南东段构造格架[J].安徽地质, 10(1):1-8. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK200000657889
邓国辉, 刘春根, 冯晔. 2005.赣东北-皖南元古代造山带构造格架及演化[J].地球学报, 26(1):9-16. doi: 10.3321/j.issn:1006-3021.2005.01.002
高林志, 刘燕学, 丁孝忠, 张传恒, 王自强, 陈俊, 刘耀荣. 2012.江南古陆中段沧水铺群锆石U-Pb年龄和构造演化意义[J].中国地质, 39(1):12-20. doi: 10.3969/j.issn.1000-3657.2012.01.002 http://geochina.cgs.gov.cn/geochina/ch/reader/view_abstract.aspx?file_no=20120102&flag=1
郭令智, 央申, 马瑞士, 叶尚夫, 卢夏华. 1984.中国东南部地体构造的研究[J].南京大学学报(自然科学), 20(4):130-137. http://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ198404014.htm
李江海, 穆剑. 1999.我国境内格林威尔期造山带的存在及其对中元古代末期超大陆再造的制约[J].地质科学, 34(3):259-272. doi: 10.3321/j.issn:0563-5020.1999.03.001
李献华, 李武显, 何斌. 2012.华南陆块的形成与Rodinia超大陆聚合-裂解——观察、解释与检验[J].矿物岩石地球化学通报, 31(6):543-559. doi: 10.3969/j.issn.1007-2802.2012.06.002
李献华, 王一先, 赵振华, 陈多福, 张宏. 1998.闽浙古元古代斜长角闪岩的离子探针锆石U-Pb年代学[J].地球化学, 27(4):327-334. doi: 10.3321/j.issn:0379-1726.1998.04.006
李献华. 2000.赣东北蛇绿混杂岩带中硅质岩的地球化学特征及构造意义[J].中国科学:地球科学, 30(3):284. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200003008
李源, 颉颃强, 宋志瑞. 2017.赣东北蛇绿岩和张村岩群的锆石SHRIMP U-Pb年龄及对江南造山带构造演化的讨论[J].地质论评, 63(4):854-868. http://d.old.wanfangdata.com.cn/Periodical/dzlp201704002
毛景文, 陈懋弘, 袁顺达, 郭春丽. 2011.华南地区钦杭成矿带地质特征和矿床时空分布规律[J].地质学报, 85(5):636-658. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201105004
舒良树, 卢华复, 贾东, 夏菲, 福赫. 1999.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(自然科学版), 35(6):668-674. http://www.cnki.com.cn/Article/CJFDTotal-NJDZ199906002.htm
舒良树, 向磊, 姚金龙. 2012.华南构造演化基本特征分析[C]//构造地质与地球动力学学术研讨会.
舒良树, 施央申, 郭令智. 1995.江南中段板块-地体构造与碰撞造山运动[M].南京:南京大学出版社.
王存智, 邢光福, 余明刚, 黄志忠, 洪文涛, 赵希林, 周效华, 段政, 鞠冬梅. 2015.赣东北蛇绿岩形成时代及构造环境——樟树墩辉长岩锆石U-Pb年龄、Hf同位素和地球化学约束[J].岩石矿物学杂志, 34(3):309-321. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201503004
王孝磊, 周金城, 陈昕, 张凤凤, 孙梓铭. 2017.江南造山带的形成与演化[J].矿物岩石地球化学通报, 36(5):1007-2802. http://d.old.wanfangdata.com.cn/Periodical/kwysdqhxtb201705003
王自强, 高林志, 丁孝忠, 黄志忠. 2012."江南造山带"变质基底形成的构造环境及演化特征[J].地质论评, 58(3):401-413. doi: 10.3969/j.issn.0371-5736.2012.03.001
邢凤鸣, 徐祥, 陈江峰, 周泰禧. 1992.赣东北元古代蛇绿岩Sm-Nd同位素年龄及地质意义[J].岩石矿物学杂志, 11(2):120-124. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW199202002.htm
徐备. 1990.论赣东北-皖南晚元古代沟弧盆体系[J].地质学报, 64(1):33-42. http://www.cnki.com.cn/Article/CJFD1990-DZXE199001003.htm
徐先兵, 汤帅, 李源, 章泽军. 2015.江南造山带东段新元古代至早中生代多期造山作用特征[J].中国地质, 42(1):33-50. doi: 10.3969/j.issn.1000-3657.2015.01.004 http://geochina.cgs.gov.cn/geochina/ch/reader/view_abstract.aspx?file_no=20150103&flag=1
薛怀民, 马芳, 宋永勤, 谢亚平. 2010.江南造山带东段新元古代花岗岩组合的年代学和地球化学:对扬子与华夏地块拼合时间与过程的约束[J].岩石学报, 26(11):3215-3244. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201011006
杨明桂, 黄水保, 楼法生, 唐维新, 毛索斌. 2009.中国东南陆区岩石圈结构与大规模成矿作用[J].中国地质, 36(3):528-543. doi: 10.3969/j.issn.1000-3657.2009.03.004 http://geochina.cgs.gov.cn/geochina/ch/reader/view_abstract.aspx?file_no=20090304&flag=1
张国伟, 郭安林, 王岳军, 李三忠, 董云鹏, 刘少峰, 何登发, 程顺有, 鲁如魁, 姚安平. 2013.中国华南大陆构造与问题[J].中国科学:地球科学, 43(10):1553-1582. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201310003
赵建新, 李献华, M T McCulloch, 周国庆, 邢凤鸣. 1995.皖南和赣东北蛇绿岩成因及其构造意义:元素和Sm-Nd同位素制约[J].地球化学, 24(4):311-326. doi: 10.3321/j.issn:0379-1726.1995.04.001
周金城, 王孝磊, 邱检生. 2009.江南造山带形成过程中若干新元古代地质事件[J].高校地质学报, 15(4):453-459. doi: 10.3969/j.issn.1006-7493.2009.04.003
周新民, 王德滋. 1988.皖南低87Sr/86Sr初始比的过铝花岗闪长岩及其成因[J].岩石学报, 51(3):2141-2145. http://www.cnki.com.cn/Article/CJFDTotal-YSXB198803004.htm
周新民, 邹海波, 杨杰东, 王银喜. 1989.安徽歙县伏川蛇绿岩套的Sm-Nd等时线年龄及其地质意义[J].科学通报, 16:1243-1245. doi: 10.3321/j.issn:0023-074X.1989.16.003