福建基础地质调查研究进展与方向
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摘要
近10年来,福建省基础地质调查研究工作取得重大进展,梳理总结主要有6个方面:(1)古元古代麻源岩群等结晶基底组成物质具多样性,是由不同时代、不同成因的变质杂岩组成("麻源变质杂岩");(2)造山带混杂岩填图方法将新元古代马面山(岩)群解体为"基质"和"岩块",提出"晚古生代马面山俯冲增生杂岩"认识;(3)加里东期构造活动对前泥盆纪基底影响(改造)深远而又强烈,加东期变形-变质-深熔及岩浆作用具有一致性;(4)应用锆石定年,在闽西南及闽北地区确认大量印支期(中-晚三叠世)花岗质岩体;(5)应用紫金山、马坑、上房等矿集区研究资料,构建了精细的晚中生代成矿系列与岩浆序列(四期);(6)确定了长乐—南澳构造岩浆带岩石组合、形成时代,精确划分4个造山阶段(对应四期构造-岩浆演化),反演了地壳隆升过程与机制。福建省所处特殊的地理和构造位置,是研究华南地质的关键窗口,在古老岩石和物质组成、新元古代-早古生代构造演化、晚古生代构造-岩浆热事件、中生代造山作用机制、中-新生代构造域转换、地壳生长与循环再造等一系列重大问题研究方面有独特的优势。
In the past ten years,great progress has been made in the basic geological investigation and research in Fujian Province,and there are six main aspects in combing and summing up:(1)The composition of crystalline basement of Paleoproterozoic igneous group is diverse,is composed of metamorphic complex of different ages( " ma-yuan metamorphic complex").(2)The mapping method of melange rocks in orogenic belts disintegrates the Neoproterozoic Mamianshan(rock)group into " matrix" and " rock block",and puts forward the understanding of " late Paleozoic Maomanshan subduction and accretive complex".(3)The Caledonian tectonic activity affected the pre Devonian basement(transformation)profoundly and strongly,and the eastern Canadian deformation metamorphism and deep penetration is consistent with magmatism.(4)Using zircon dating,a large number of Indosinian(Middlelate Triassic)granitic intrusions were confirmed in southwestern Fujian and northern Fujian.(5)The fine late Mesozoic metallogenic series and magmatic series(stage 4)were constructed by using the data of Zijinshan,Makeng and Shangfang ore concentration areas.(6)The rock assemblage of the Changle-Nanao tectonic magmatic belt was determined and its forming age was determined.Four orogenic stages(corresponding to the four stages of tectonicmagmatic evolution)were accurately divided into four orogenic stages and the crustal uplift process and mechanism were inversed.The special geographical and tectonic location of Fujian Province is the key window to study the geology of South China.In ancient rock and material composition,Neoproterozoic early Paleozoic tectonic evolution,late Paleozoic tectonic-magmatic thermal event,Mesozoic orogenic mechanism,The Meso-Cenozoic tectonic domain transformation,crustal growth and recycling have unique advantages in a series of important problems.
In the past ten years,great progress has been made in the basic geological investigation and research in Fujian Province,and there are six main aspects in combing and summing up:(1)The composition of crystalline basement of Paleoproterozoic igneous group is diverse,is composed of metamorphic complex of different ages( " ma-yuan metamorphic complex").(2)The mapping method of melange rocks in orogenic belts disintegrates the Neoproterozoic Mamianshan(rock)group into " matrix" and " rock block",and puts forward the understanding of " late Paleozoic Maomanshan subduction and accretive complex".(3)The Caledonian tectonic activity affected the pre Devonian basement(transformation)profoundly and strongly,and the eastern Canadian deformation metamorphism and deep penetration is consistent with magmatism.(4)Using zircon dating,a large number of Indosinian(Middlelate Triassic)granitic intrusions were confirmed in southwestern Fujian and northern Fujian.(5)The fine late Mesozoic metallogenic series and magmatic series(stage 4)were constructed by using the data of Zijinshan,Makeng and Shangfang ore concentration areas.(6)The rock assemblage of the Changle-Nanao tectonic magmatic belt was determined and its forming age was determined.Four orogenic stages(corresponding to the four stages of tectonicmagmatic evolution)were accurately divided into four orogenic stages and the crustal uplift process and mechanism were inversed.The special geographical and tectonic location of Fujian Province is the key window to study the geology of South China.In ancient rock and material composition,Neoproterozoic early Paleozoic tectonic evolution,late Paleozoic tectonic-magmatic thermal event,Mesozoic orogenic mechanism,The Meso-Cenozoic tectonic domain transformation,crustal growth and recycling have unique advantages in a series of important problems.
引文
[1]福建省地质矿产局.福建省区域地质志.北京:地质出版社.1985.
2 金文山,孙大中,赵风清,等.华南大陆深部地壳结构及其演化.北京:地质出版社,1997.
3 张国伟,郭安林,王岳军,等.中国华南大陆构造与问题.中国科学:地球科学,2013,43.
4 福建省地质调查研究院.中国区域地质志·福建卷.北京:地质出版社,2016.
5 Li L M,Sun M,Wang Y,et al.Geochronological and Geochemical study of Palaeoproterozoic gneissic granites and clinopyroxenite xenoliths from NW Fujian,SE China:implications for the crustal evolution of the Cathaysia Block.J.Asian Earth Sci.,2011,41.
6 陈润生.闽北建瓯上房钨矿床成矿作用特征及矿床成因研究.中国地质大学(武汉),2013.
7 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.高校地质学报,2008,(1).
8 Wan Y S,Liu D Y,Xu M H,et al.SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in North western Fujian,Cathaysia Block,China:tectonic implications and the need to redefine lithostratigraphic units.Gondwana Research,2007,12.
9 Chen C H,Lee C Y,Liu Y H,et al.Precambrian protoliths and Phanerozoic overprinting on the Wuyishan terrain(South China):New evidence from a combination of LA-ICPMS zircon and EMP monazite geochronology.Precambrian Research,2018.
10 于津海,周新民,O'Reilly Y S,等.南岭东段基底麻粒岩相变质岩的形成时代和原岩性质.科学通报,2005,50(18).
11 于津海,魏震洋,等.华夏地块:一个由古老物质组成的年轻陆块.高校地质学报,2006,12(4).
12 李献华,等.闽浙古元古代斜长角闪岩的离子探针锆石U-Pb年代学.地球化学,1998,27(4).
13 杨振升,徐仲元,刘正宏,等.高级变质岩区地质调查与综合研究方法.北京:地质出版社,2008.
14 周祖翼.东南沿海基底研究述评.福建地质,1989,8(1).
15 汪相,陈洁,等.浙西南淡竹花岗闪长岩中锆石的成因研究及其地质意义.地质论评.2008,54(3).
16 Liu R,Zhou H,Zhang L,et al.Paleoproterozoic reworking of ancient crust in the Cathaysia Block,South China:evidence from zircon trace elements,U-Pb and Lu-Hf isotopes.Chin.Sci.Bull.,2009,54.
17 Yu J H,Wang L J,O'Reilly S Y,et al.A Paleoproterozoic orogeny recorded in a long-lived cratonic remnant(Wuyishan terrane),eastern Cathaysia Block,China.Precambrian Research,2009,174.
18 Liu Q,Yu J H.,O'Reilly S Y,Zhou M F,et al.Origin and geological significance of Paleoproterozoic granites in the northeastern Cathaysia Block,South China.Precambr.Res.,2014,248.
19 Zhang D,Wu G.Geochronology of the Neoproterozoic Mamianshan group in the Cathaysia block,China and its tectonic significance(Abs.).In:The 33rd IGCAugust 6-14,2008.Oslo,Norway.
20 Wu G,Yu X,et al.Neoproterozoic tectonic setting of Southeast China:new constraints from SHRIMP U-Pb zircon ages and petrographic studies on the Mamianshan Group.Acta Geol.Sin.,2010,84.
21 Li X H.Timing of the Cathaysia Block formation:constraints from SHRIMP UPb zircon geochronology.Episodes,1997,20.
22 Li Z X,Li X H,Kinny P D.Geochronology of Neoprotero-zoic syn-rift magmatism in the Yangtze Craton,South China and correlations with other continents:evidence for a mantle super-plume that broke up Rodinia.Precambrian Res,2003,122.
23 Wang X C,Li X H,Li W X,Li Z X.Variable involvements of mantle plumes in the genesis of mid-Neoproterozoic basaltic rock,in Sonth China:A review.Gondwana Res.,2009,15.
24 Shu L S,Faure M,YuJH,et al.Geochronological and geochemical features of the Cathaysia block(South China):new evidence for the Neoproterozoic breakup ofRodinia Precambrian Research,2011,187.
25 Guo L Z,Shi Y S,Lu H F,et al.The pre-Devonian tectonic patterns and evolution of South China.Journal of Southeast Asian Earth Sciences,1989,3.
26 汪新,杨树锋,施建宁,等.浙江龙泉碰撞混杂岩的发现及其对华南碰撞造山带研究的意义.南京大学学报(自然科学),1988,24(3).
27 陈迪云,聂淦波,王勇.龙泉—南平一带蛇绿岩的地球化学特征.地质地球化学,1993,3(1).
28 任胜利,李继亮,周新华,等.闽北政和洋后变质超镁铁岩的岩石地球化学及矿物化学研究.地球化学,1997,26(4).
29 张福勤,谢鸿森,许祖鸣.华南前寒武纪镁铁-超镁铁杂岩的岩石大地构造格架.李继亮主编.东南大陆岩石圈结构与地质演化.北京:冶金工业出版社,1993.
30 Li W X,Li X H,Li Z X.Neoproterozoic bimodal magmatism in the Cathaysia Block of South China and its tectonic significance.Precambr.Res.2005,136.
31 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.高校地质学报,2006,12(4).
32 舒良树.华南构造演化的基本特征.地质通报,2012,31.
33 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错石LA-ICP-MS U-Pb年代学:对武夷山加里东运动时代的制约.地质论评,2009,55(2).
34 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 pressure-temperature conditions.Geological Society of America Bulletin,2010,122.
35 Zhao G C,Cawood P A.Tectonothermal evolution of the Mayuan assemblage in the Cathaysia Block:implications for Neoproterozoic collision-related assembly of the South China craton.Am J Sci,1999,299.
36 Zhao G C,Cawood P A.Precambrian geology of China.Precambrian Research,2012.
37 于津海,王丽娟,等.华夏地块显生宙的变质作用期次和特征.高校地质学报,2007,13(3).
38 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 WuyiYunkai domains.Lithos,2011,127.
39 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 amphibolite and granulite.Lithos,2012,150.
40 Zeng W,Zhang L,Zhou H W,et al.Caledonian reworking of Paleoproterozoic basement in the Cathaysia Block:constraints from zircon U-Pb dating,Hf isotopes and trace elements.Chin.Sci.Bull.2008,53.
41 刘锐,张利,周汉文,等.闽西北加里东期混合岩及花岗岩的成因:同变形地壳深熔作用.岩石学报,2008,24(6).
42 Liu R,Zhou H W,Zhang L,et al..Zircon U-Pb ages and Hf isotope compositions of the Mayuan migmatite complex,NW Fujian Province,Southeast China:constraints on the timing and nature of a regional tectonothermal event associated with the Caledonian orogeny.Lithos,2010,119.
43 Wang D,Zheng J,Ma Q,et al.Early Paleozoic crustal anatexis in the intraplate Wuyi-Yunkai orogen,South China.Lithos 2013,175-176.
44 刘锐.华夏地块前海西期地壳深熔作用——以浙闽地区为例.中国地质大学(武汉):博士论文,2009.
45 魏春景.变质作用P-T-t轨迹的研究方法与进展.地学前缘,2011,18(2).
46 Faure M,Shu L S,Wang B,et al.Intracontinental subduction:apossible mechanism for the Early Paleozoic Orogen of SE China.Terra Nova,2009,21.
47 Wang Y J,Fan W M,Zhang G W,et al.Phanerozoic tectonics of the South China Block:Key observations and controversies.Gondwana Res,2013,23.
48 舒良树,于津海,贾东,等.华南东段早古生代造山带研究.地质通报,2008,27(10).
49 Charvet J,Shu L S,Faure M,et al.Structural development of the Lower Paleozoic belt of South China:Genesis of an intracontinental orogen.J.Asian Earth Sci.,2010,39.
50 Charvet J.The Neoproterozoic-Early Paleozoic tectonic evolution of the South China Block:an overview.Journal of Asian Earth Sciences,2013,74.
51 Zhang Y,Shu L,Chen X Y.Study of geochemistry,geochronology and petrogenesis of the Early Paleozoic granitic plutons in the central-southern Jiangxi Province.Science in China(Earth Sciences),2011,54(10).
52 Shu L S,Wang B,Cawood P A,et al.Early Paleozoic and early Mesozoic intraplate tectonic and magmatic events in the Cathaysia Block,South China.Tectonics,2015,34.
53 Wang Y,Zhang F,Fan W,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.Tectonics,2010,29(6).
54 周新民.对华南花岗岩研究的若干思考.高校地质学报,2003,9(4).
55 孙涛.新编华南花岗岩分布图及其说明.地质通报,2006,(3).
56 Zhou X M,Sun T,Shen W Z,et al.Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:A response to tectonic evolution.Episodes,2006,29(1).
57 王丽娟,于津海,徐夕生,等.闽西南古田—小陶花岗质杂岩体的形成时代和成因.岩石学报,2007,23.
58 Wang KX,Sun T,Chen PR,et al.The geochronological and geochemical constraints on the petrogenesis of the Early Mesozoic A-type granite and diabase in northwestern Fujian province.Lithos.2013,179.
59 李万友,马昌前,刘园园,等.浙江印支期铝质A型花岗岩的发现及其地质意义.中国科学:地球科学,2012,42(2).
60 向庭富,孙涛,陈培荣,等.闽西北罗古岩岩体印支期年龄的厘定及其岩石成因和构造意义.高校地质学报.2013,19(2).
61 高万里,王宗秀,李春麟,等.浙东南印支期花岗岩的错石U-Pb年代学、地球化学及构造意义.地质学报,2014,88 (6).
62 Gao W,Wang Z,Li C.Triassic magmatism in the eastern part of the South China Block:geochronological and petrogenetic constraints from Indosinian granites.Geosci.Front.,2017,8.
63 陈润生.福建建瓯上房花岗岩热液锆石U-Pb年龄及地质学意义.福建地质,2014,34(2).
64 陈润生,李建威,曹康,等.闽北上房白钨矿锆石U-Pb和辉钼矿Re-Os定年及其地质意义.地球科学—中国地质大学学报,2012,38(2).
65 黄文婷,李晶,梁华英,等.福建紫金山矿田罗卜岭铜钼矿化斑岩LA-ICP-MS锆石U-Pb年龄及成矿岩浆高氧化特征研究,岩石学报,2013,29(1).
66 赵希林,毛建仁,陈荣,等.闽西南地区才溪岩体错石S11R1MP定年及其地球化学特征.岩石矿物学杂志,2007,26(3).
67 江思宏,梁清玲,王少怀,等.福建紫金山铜金矿科学基地研究.北京:地质出版社,2017.
68 张承帅.福建马坑铁矿床地质与地球化学.北京:中国地质大学:博士论文,2012.
69 王登红,陈郑辉,陈毓川,等.我国重要矿产地成岩成矿年代学研究新数据.地质学报,2010,84(7).
70 张达,吴淦国,狄永军,等.福建漳平洛阳铁矿床成岩成矿年代学及其地质意义.地球科学-中国地质大学学报,2012,37(6).
71 毛建仁,陶奎元,李寄喝,等.闽西南晚中生代四方岩体同位素年代学、地球化学及其构造意义.岩石学报,2002,18(4).
72 梁清玲,江思宏,王少怀,等.福建紫金山矿田罗卜岭斑岩型铜铝矿床辉铝矿Re-0s定年及地质意义.地质学报,2012,86(7).
73 邱检生,肖娥,胡建,等.福建北东沿海高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约.岩石学报,2008,24(11).
74 李良林,周汉文,陈植华,等.福建太姥山地区和鼓山地区A型花岗岩对比及其地球动力学意义.现代地质,2013,27(3).
75 赵芝,陈郑辉,王成辉,等.闽东大湾钼铍矿的辉钼矿Re-Os同位素年龄——兼论福建省钼矿时空分布及构造背景,矿床地质,2012,36(3).
76 Shen LW,Yu JH,O'Reilly S Y,et al.Widespread Paleoproterozoic basement in the eastern Cathaysia Block:Evidence from metasedimentary rocks of the Pingtan-Dongshan metamorphic belt,in southeastern China.Precambrian Research.2016,285.
77 冯艳芳,邓晋福、肖庆辉,等,长乐—南澳构造带花岗岩类年代学、岩石组合与构造演化,北京:地质出版社,2013.
78 刘潜,于津海,苏斌,等.福建锦城187 Ma花岗岩的发现构造演化的制约.对华南沿海早侏罗世构造演化的制约.岩石学报,2011,27(12).
79 Liu Q,Yu J H,Wang Q,et al.Ages and geochemistry of granites in the Pingtan-Dongshan Metamorphic Belt,Coastal South China:new constraints on Late Mesozoic magmatic evolution.Lithos,2012,150(5).
80 石建基.闽南沿海地区变质变形侵入岩时序划分及其地质意义.福建地质,2010,29(4).
81 Cui J J,Zhang Y Q,Dong S W,et al.Zircon U-Pb geochronology of the Mesozoic metamorphic rocks and granitoids in the coastal tectonic zone of SE China:constraints on the timing of Late Mesozoic orogeny.J.Asian Earth Sci.,2013,62.
82 Chen C H,Lee C Y,Shinjo R.The epilog of the western paleo-Pacific subduction:inferred from spatial and temporal variations and geochemistry of the Late Cretaceous to Early Cenozoic silicic magmatism in coastal South China.J.Asian Earth Sci.,2016,115.
83 Lan CY,Chung SL and Mertzman SA.Mineralogy and geochemistry of granitic rocky from Chinmen,Liehyu and Dadan islands,Fujian.Journal of the Geological Society of China,1997,40(3).
84 Chen C H,Lee C Y,Lu H Y,Hsieh P S.Generation of Late Cretaceous silicic rocks in SE China:age,major element and numerical simulation constraints.J.Asian Earth Sci.,2008,31(4-6).
85 Xing G F,Wang X L,Wan Y S,et al.Diversity in early crustal evolution:4100Ma zircons inthe Cathaysia Block of southern China.Scientific Reports,2015,4.
86 Yu J H,O'Reilly Y S,Wang L J,et al.Finding of ancient materials in Cathaysia and implication for the formation of Precambrian crust.Chin.Sci.Bull.,2007,52.
87 Yao J,Shu L,Santosh M.Detrital zircon U-Pb geochronology,Hf-isotopes and geochemistry-New clues for the Precambrian crustal evolution of Cathaysia Block,South China.Gondwana Res.,2011,20.
88 李献华,李武显,何斌.华南陆块的形成与Rodinia超大陆聚合-裂解_观察、解释与检验.矿物岩石地球化学通报,2012,31(6).
89 Yu J H,O'Reilly S Y,Zhou M F,et al.U-Pb geochronology and Hf-Nd isotopic geochemistry of the Badu Complex,Southeastern China:implications for the Precambrian crustal evolution and paleogeography of the Cathaysia Block.Precambr.Res.,2012,3-4.
90 Xu Y,Wang C Y,Zhao T.Using detrital zircons from river sands to constrain major tectono-thermal events of the Cathaysia Block,SE China.J.Asian Earth Sci.,2016,124.
91 Li X H,Li Z X,He B.The Early Permian active continental margin and crustal growth of the Cathaysia Block:in situ U-Pb,Lu-Hf and O isotope analyses of detrital zircons.Chem.Geol.,2012,328.
92 Yui T F,Maki K C Y,Hirata T,Chu H T.Detrital zircons from the Tananao Metamorphic Complex of Taiwan:A preliminary study.Geol Soc China Annual Meeting,Tainan,ROC.2010,214.
93 Shao WY,Chung SL,Chen WS.Old continental zircons from a young oceanic arc,eastern Taiwan:Implications for Luzon subduction initiation and Asian accretionary orogeny.Geology,2015,43(6).
94 向磊,舒良树.华南东段前泥盆纪构造演化:来自碎屑锆石的证据.中国科学(地球科学),2010,40(10).
95 Yao J,Shu L,Santosh M.Detrital zircon U-Pb geochronology,Hf-isotopes and geochemistry-New clues for the Precambrian crustal evolution of Cathaysia Block,South China.Gondwana Res.,2011,20.
96 Li X H,Li Z X,Ge W,et al.Neoproterozoic granitoids in SouthChina:crustal melting above a mantle plume at ca.825 Ma?Pre-cambrian Res,2003,122.
97 Li X H,Li W X,Li Z X,et al.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.Precambrian Research,2009,174.
98 Li Z X,Li X,Zhou H,Kinny P D.Grenvillian continental collision in south China:new SHRIMP U-Pb zircon results and implications for the configuration of Rodinia.Geology,2002,30.
99 Lin SF,Xing GF,Davis D W,at al.Appalachian-style multi-terrane Wilson cycle model for the assembly of South China.GSA,2018.
100 Wang YJ,Zhang AM,Cawood FA,et al.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,2013,231.
101 Cawood P A,Wang Y,Xu Y,Zhao G.Locating South China in Rodinia and Gondwana:a fragment of greater India lithosphere?Geology,2013,41.
102 Duan L,Meng Q R.,Wu G L,et al.Detrital zircon evidence for the linkage of the South China block with Gondwanaland in early Palaeozoic time.Geol.Mag,2012,149.
103 Wang W,Zeng M F,Zhou M F,et al.provenance and tectonic setting of Neoproterozoic to early Paleozoic sequences in southeastern South China Block:Constraints on its linkage to western Australia-East Antarctica.Precambrian Research,2018,309.
104 Yang Z,Sun Z,Yang T,Pei J.A long connection(750-380Ma)between South China and Australia:paleomagnetic constraints.Earth Planet.Sci.Lett,2004,220.
105 Yu J H,Liu Q,Hu X M,et al.Late Paleozoic magmatism in South China:Oceanic subduction or intracontinental orogeny?Chin Sci Bull,2012,57.
106 韩发,葛朝华.福建马坑铁矿床海相火山热液-沉积成因-地质地球化学特征.中国地质科学院矿床地质研究所所刊,1983,7(2).
107 王森,张达,吕良冀,等.闽西南晚古生代以来伸展构造演化:中基性岩墙群的年代学、地球化学制约,大地构造与成矿学,2015,39(5).
108 Zhou X M,Li W X.Origin of Late Mesozoic igneous rocks in Southeastern China:implications for lithosphere subduction and underplating of mafic magmas.Tectonophysics,2000,326(3/4).
109 Li Z X,Li X H.Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China:a flat-slab subduction model.Geology,2007,35.
110 Yui T F,Okamoto K.Late Triassic_Late Cretaceous aocretion-subduction in the Taiwan region along the eastern margin of South China-Evidence from zircon SHRIMP dating.Int Geol Rev,2009,51.
111 邵磊,尤洪庆,郝沪军,等.南海东北部中生界岩石学特征及沉积环境.地质评论,2007,53.
112 汪品先.追踪边缘海的生命史:“南海深部计划”的科学目标.科学通报,2012,57(20).
113 闵慧,任建业,高金耀,等.南海北部古俯冲带的位置及其对南海扩张的控制.大地构造与成矿学,2010,34(4).
114 金庆焕,高天钧,等.台湾海峡中、新生代地质构造及油气地质.福州:福建科学技术出版社,1993.
115 Li C F,Xu X,Lin J..Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Ex-pedition 349.Geochem Geophys Geosyst,2014,15.
116 Huang C Y,Yuan P,and Tsao S J.Temporal and spatial records of active arc-continent collision in Taiwan:A synthesis:Geological Society of America Bulletin,2006,118.
117 Yu H S.Paired and Foreland Basin:Insight s on Late Cenozoic Orogeny and Foreland Sedimentation in Taiwan Region7th Chinese Geophysical Societ y Symposium,Programme Preceedings.1998.
118 Yu J H,O'Reilly S Y,Wang L J,Griffin W L,Zhou M F,Zhang M,Shu L S.Components and episodic growth of Precambrian crust in the Cathaysia Block,South China:evidence from U-Pb ages and Hf isotopes of zircons in Neoproterozoic sediments.Precambrian Research,2010,181.
119 Li X H.,Li Z X,Li W X.Detrital zircon U-Pb age and Hf isotope constrains on the generation and reworking of Precambrian continental crust in the Cathaysia Block,South China:a synthesis.Gondwana Res,2014.25.
120 Kemp A I,Hawkesworth C,Paterson B A,Kinny P D..Episodic growth of the Gondwana supercontinent from hafnium and oxygen isotopes in zircon.Nature,2006,439.
121 Zheng Y F,Zhang S B,Zhao Z F,et al.Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China:Implications for growth and reworking of continental crust.Lithos,2007,96.
(1)福建省地质调查研究院,1∶5万镇前、东游、岭下、双溪幅区域地质调查报告,2013。
(2)福建省地质调查研究院,1∶5万建瓯市、南雅、玉山、西溪幅区域地质调查报告,2017。
(3)福建省地质调查研究院,1∶5万麻沙、建阳市、徐市幅区域地质调查报告,2011。
(1)福建省地质调查研究院,1∶5万二十八都、官路幅区域地质调查报告,2018。
(2)福建省地质调查研究院,1∶5万建瓯市、南雅、玉山、西溪幅区域地质调查报告,2017。
(3)福建省地质调查研究院,1∶5万长汀、南岩、策田、濯田幅区域地质调查报告,2016
(1)福建省地质调查研究院,福建省重要矿产资源潜力评价成果报告,2013。
(2)福建省地质调查研究院,1∶5万建瓯市、南雅、玉山、西溪幅区域地质调查报告,2017。
(1)福建省地质调查研究院和1∶5万新泉、梅村、古田、湖洋幅区域地质调查报告,2013。
(2)福建省地质调查研究院,1∶5万赖源、双洋、白沙、钱坂幅区域地质调查报告,2015。
(3)福建省地质调查研究院,1∶5万隔川、连城县、朋口、湖峰幅区域地质调查报告,2016。
(1)福建省地质调查研究院,1∶5万长汀、南岩、策田、濯田幅区域地质调查报告,2016。
(1)福建省闽北地质大队,1∶5万新桥、屏山、溪南、一都幅区域地质调查报告,2015。
(2)福建省地质调查研究院,1∶5万镇前、东游、岭下、双溪幅区域地质调查报告2013。
(1)福建省地质调查研究院,1∶5万建瓯市、南雅、玉山、西溪幅幅区域地质调查报告,2017。
(1)福建省地质调查研究院,1∶5万长汀、南岩、策田、濯田幅区域地质调查报告,2016。
(2)福建省地质调查研究院,1∶5万隔川、连城县、朋口、湖峰幅区域地质调查报告,2016。
(3)福建省地质调查研究院,1∶5万建瓯市、南雅、玉山、西溪幅区域地质调查报告,2017。
(1)福建省第四地质大队,闽东地区中生代火山岩基底构造与成矿作用关系研究报告,2017。
2 金文山,孙大中,赵风清,等.华南大陆深部地壳结构及其演化.北京:地质出版社,1997.
3 张国伟,郭安林,王岳军,等.中国华南大陆构造与问题.中国科学:地球科学,2013,43.
4 福建省地质调查研究院.中国区域地质志·福建卷.北京:地质出版社,2016.
5 Li L M,Sun M,Wang Y,et al.Geochronological and Geochemical study of Palaeoproterozoic gneissic granites and clinopyroxenite xenoliths from NW Fujian,SE China:implications for the crustal evolution of the Cathaysia Block.J.Asian Earth Sci.,2011,41.
6 陈润生.闽北建瓯上房钨矿床成矿作用特征及矿床成因研究.中国地质大学(武汉),2013.
7 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.高校地质学报,2008,(1).
8 Wan Y S,Liu D Y,Xu M H,et al.SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in North western Fujian,Cathaysia Block,China:tectonic implications and the need to redefine lithostratigraphic units.Gondwana Research,2007,12.
9 Chen C H,Lee C Y,Liu Y H,et al.Precambrian protoliths and Phanerozoic overprinting on the Wuyishan terrain(South China):New evidence from a combination of LA-ICPMS zircon and EMP monazite geochronology.Precambrian Research,2018.
10 于津海,周新民,O'Reilly Y S,等.南岭东段基底麻粒岩相变质岩的形成时代和原岩性质.科学通报,2005,50(18).
11 于津海,魏震洋,等.华夏地块:一个由古老物质组成的年轻陆块.高校地质学报,2006,12(4).
12 李献华,等.闽浙古元古代斜长角闪岩的离子探针锆石U-Pb年代学.地球化学,1998,27(4).
13 杨振升,徐仲元,刘正宏,等.高级变质岩区地质调查与综合研究方法.北京:地质出版社,2008.
14 周祖翼.东南沿海基底研究述评.福建地质,1989,8(1).
15 汪相,陈洁,等.浙西南淡竹花岗闪长岩中锆石的成因研究及其地质意义.地质论评.2008,54(3).
16 Liu R,Zhou H,Zhang L,et al.Paleoproterozoic reworking of ancient crust in the Cathaysia Block,South China:evidence from zircon trace elements,U-Pb and Lu-Hf isotopes.Chin.Sci.Bull.,2009,54.
17 Yu J H,Wang L J,O'Reilly S Y,et al.A Paleoproterozoic orogeny recorded in a long-lived cratonic remnant(Wuyishan terrane),eastern Cathaysia Block,China.Precambrian Research,2009,174.
18 Liu Q,Yu J H.,O'Reilly S Y,Zhou M F,et al.Origin and geological significance of Paleoproterozoic granites in the northeastern Cathaysia Block,South China.Precambr.Res.,2014,248.
19 Zhang D,Wu G.Geochronology of the Neoproterozoic Mamianshan group in the Cathaysia block,China and its tectonic significance(Abs.).In:The 33rd IGCAugust 6-14,2008.Oslo,Norway.
20 Wu G,Yu X,et al.Neoproterozoic tectonic setting of Southeast China:new constraints from SHRIMP U-Pb zircon ages and petrographic studies on the Mamianshan Group.Acta Geol.Sin.,2010,84.
21 Li X H.Timing of the Cathaysia Block formation:constraints from SHRIMP UPb zircon geochronology.Episodes,1997,20.
22 Li Z X,Li X H,Kinny P D.Geochronology of Neoprotero-zoic syn-rift magmatism in the Yangtze Craton,South China and correlations with other continents:evidence for a mantle super-plume that broke up Rodinia.Precambrian Res,2003,122.
23 Wang X C,Li X H,Li W X,Li Z X.Variable involvements of mantle plumes in the genesis of mid-Neoproterozoic basaltic rock,in Sonth China:A review.Gondwana Res.,2009,15.
24 Shu L S,Faure M,YuJH,et al.Geochronological and geochemical features of the Cathaysia block(South China):new evidence for the Neoproterozoic breakup ofRodinia Precambrian Research,2011,187.
25 Guo L Z,Shi Y S,Lu H F,et al.The pre-Devonian tectonic patterns and evolution of South China.Journal of Southeast Asian Earth Sciences,1989,3.
26 汪新,杨树锋,施建宁,等.浙江龙泉碰撞混杂岩的发现及其对华南碰撞造山带研究的意义.南京大学学报(自然科学),1988,24(3).
27 陈迪云,聂淦波,王勇.龙泉—南平一带蛇绿岩的地球化学特征.地质地球化学,1993,3(1).
28 任胜利,李继亮,周新华,等.闽北政和洋后变质超镁铁岩的岩石地球化学及矿物化学研究.地球化学,1997,26(4).
29 张福勤,谢鸿森,许祖鸣.华南前寒武纪镁铁-超镁铁杂岩的岩石大地构造格架.李继亮主编.东南大陆岩石圈结构与地质演化.北京:冶金工业出版社,1993.
30 Li W X,Li X H,Li Z X.Neoproterozoic bimodal magmatism in the Cathaysia Block of South China and its tectonic significance.Precambr.Res.2005,136.
31 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.高校地质学报,2006,12(4).
32 舒良树.华南构造演化的基本特征.地质通报,2012,31.
33 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错石LA-ICP-MS U-Pb年代学:对武夷山加里东运动时代的制约.地质论评,2009,55(2).
34 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 pressure-temperature conditions.Geological Society of America Bulletin,2010,122.
35 Zhao G C,Cawood P A.Tectonothermal evolution of the Mayuan assemblage in the Cathaysia Block:implications for Neoproterozoic collision-related assembly of the South China craton.Am J Sci,1999,299.
36 Zhao G C,Cawood P A.Precambrian geology of China.Precambrian Research,2012.
37 于津海,王丽娟,等.华夏地块显生宙的变质作用期次和特征.高校地质学报,2007,13(3).
38 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 WuyiYunkai domains.Lithos,2011,127.
39 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 amphibolite and granulite.Lithos,2012,150.
40 Zeng W,Zhang L,Zhou H W,et al.Caledonian reworking of Paleoproterozoic basement in the Cathaysia Block:constraints from zircon U-Pb dating,Hf isotopes and trace elements.Chin.Sci.Bull.2008,53.
41 刘锐,张利,周汉文,等.闽西北加里东期混合岩及花岗岩的成因:同变形地壳深熔作用.岩石学报,2008,24(6).
42 Liu R,Zhou H W,Zhang L,et al..Zircon U-Pb ages and Hf isotope compositions of the Mayuan migmatite complex,NW Fujian Province,Southeast China:constraints on the timing and nature of a regional tectonothermal event associated with the Caledonian orogeny.Lithos,2010,119.
43 Wang D,Zheng J,Ma Q,et al.Early Paleozoic crustal anatexis in the intraplate Wuyi-Yunkai orogen,South China.Lithos 2013,175-176.
44 刘锐.华夏地块前海西期地壳深熔作用——以浙闽地区为例.中国地质大学(武汉):博士论文,2009.
45 魏春景.变质作用P-T-t轨迹的研究方法与进展.地学前缘,2011,18(2).
46 Faure M,Shu L S,Wang B,et al.Intracontinental subduction:apossible mechanism for the Early Paleozoic Orogen of SE China.Terra Nova,2009,21.
47 Wang Y J,Fan W M,Zhang G W,et al.Phanerozoic tectonics of the South China Block:Key observations and controversies.Gondwana Res,2013,23.
48 舒良树,于津海,贾东,等.华南东段早古生代造山带研究.地质通报,2008,27(10).
49 Charvet J,Shu L S,Faure M,et al.Structural development of the Lower Paleozoic belt of South China:Genesis of an intracontinental orogen.J.Asian Earth Sci.,2010,39.
50 Charvet J.The Neoproterozoic-Early Paleozoic tectonic evolution of the South China Block:an overview.Journal of Asian Earth Sciences,2013,74.
51 Zhang Y,Shu L,Chen X Y.Study of geochemistry,geochronology and petrogenesis of the Early Paleozoic granitic plutons in the central-southern Jiangxi Province.Science in China(Earth Sciences),2011,54(10).
52 Shu L S,Wang B,Cawood P A,et al.Early Paleozoic and early Mesozoic intraplate tectonic and magmatic events in the Cathaysia Block,South China.Tectonics,2015,34.
53 Wang Y,Zhang F,Fan W,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.Tectonics,2010,29(6).
54 周新民.对华南花岗岩研究的若干思考.高校地质学报,2003,9(4).
55 孙涛.新编华南花岗岩分布图及其说明.地质通报,2006,(3).
56 Zhou X M,Sun T,Shen W Z,et al.Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:A response to tectonic evolution.Episodes,2006,29(1).
57 王丽娟,于津海,徐夕生,等.闽西南古田—小陶花岗质杂岩体的形成时代和成因.岩石学报,2007,23.
58 Wang KX,Sun T,Chen PR,et al.The geochronological and geochemical constraints on the petrogenesis of the Early Mesozoic A-type granite and diabase in northwestern Fujian province.Lithos.2013,179.
59 李万友,马昌前,刘园园,等.浙江印支期铝质A型花岗岩的发现及其地质意义.中国科学:地球科学,2012,42(2).
60 向庭富,孙涛,陈培荣,等.闽西北罗古岩岩体印支期年龄的厘定及其岩石成因和构造意义.高校地质学报.2013,19(2).
61 高万里,王宗秀,李春麟,等.浙东南印支期花岗岩的错石U-Pb年代学、地球化学及构造意义.地质学报,2014,88 (6).
62 Gao W,Wang Z,Li C.Triassic magmatism in the eastern part of the South China Block:geochronological and petrogenetic constraints from Indosinian granites.Geosci.Front.,2017,8.
63 陈润生.福建建瓯上房花岗岩热液锆石U-Pb年龄及地质学意义.福建地质,2014,34(2).
64 陈润生,李建威,曹康,等.闽北上房白钨矿锆石U-Pb和辉钼矿Re-Os定年及其地质意义.地球科学—中国地质大学学报,2012,38(2).
65 黄文婷,李晶,梁华英,等.福建紫金山矿田罗卜岭铜钼矿化斑岩LA-ICP-MS锆石U-Pb年龄及成矿岩浆高氧化特征研究,岩石学报,2013,29(1).
66 赵希林,毛建仁,陈荣,等.闽西南地区才溪岩体错石S11R1MP定年及其地球化学特征.岩石矿物学杂志,2007,26(3).
67 江思宏,梁清玲,王少怀,等.福建紫金山铜金矿科学基地研究.北京:地质出版社,2017.
68 张承帅.福建马坑铁矿床地质与地球化学.北京:中国地质大学:博士论文,2012.
69 王登红,陈郑辉,陈毓川,等.我国重要矿产地成岩成矿年代学研究新数据.地质学报,2010,84(7).
70 张达,吴淦国,狄永军,等.福建漳平洛阳铁矿床成岩成矿年代学及其地质意义.地球科学-中国地质大学学报,2012,37(6).
71 毛建仁,陶奎元,李寄喝,等.闽西南晚中生代四方岩体同位素年代学、地球化学及其构造意义.岩石学报,2002,18(4).
72 梁清玲,江思宏,王少怀,等.福建紫金山矿田罗卜岭斑岩型铜铝矿床辉铝矿Re-0s定年及地质意义.地质学报,2012,86(7).
73 邱检生,肖娥,胡建,等.福建北东沿海高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约.岩石学报,2008,24(11).
74 李良林,周汉文,陈植华,等.福建太姥山地区和鼓山地区A型花岗岩对比及其地球动力学意义.现代地质,2013,27(3).
75 赵芝,陈郑辉,王成辉,等.闽东大湾钼铍矿的辉钼矿Re-Os同位素年龄——兼论福建省钼矿时空分布及构造背景,矿床地质,2012,36(3).
76 Shen LW,Yu JH,O'Reilly S Y,et al.Widespread Paleoproterozoic basement in the eastern Cathaysia Block:Evidence from metasedimentary rocks of the Pingtan-Dongshan metamorphic belt,in southeastern China.Precambrian Research.2016,285.
77 冯艳芳,邓晋福、肖庆辉,等,长乐—南澳构造带花岗岩类年代学、岩石组合与构造演化,北京:地质出版社,2013.
78 刘潜,于津海,苏斌,等.福建锦城187 Ma花岗岩的发现构造演化的制约.对华南沿海早侏罗世构造演化的制约.岩石学报,2011,27(12).
79 Liu Q,Yu J H,Wang Q,et al.Ages and geochemistry of granites in the Pingtan-Dongshan Metamorphic Belt,Coastal South China:new constraints on Late Mesozoic magmatic evolution.Lithos,2012,150(5).
80 石建基.闽南沿海地区变质变形侵入岩时序划分及其地质意义.福建地质,2010,29(4).
81 Cui J J,Zhang Y Q,Dong S W,et al.Zircon U-Pb geochronology of the Mesozoic metamorphic rocks and granitoids in the coastal tectonic zone of SE China:constraints on the timing of Late Mesozoic orogeny.J.Asian Earth Sci.,2013,62.
82 Chen C H,Lee C Y,Shinjo R.The epilog of the western paleo-Pacific subduction:inferred from spatial and temporal variations and geochemistry of the Late Cretaceous to Early Cenozoic silicic magmatism in coastal South China.J.Asian Earth Sci.,2016,115.
83 Lan CY,Chung SL and Mertzman SA.Mineralogy and geochemistry of granitic rocky from Chinmen,Liehyu and Dadan islands,Fujian.Journal of the Geological Society of China,1997,40(3).
84 Chen C H,Lee C Y,Lu H Y,Hsieh P S.Generation of Late Cretaceous silicic rocks in SE China:age,major element and numerical simulation constraints.J.Asian Earth Sci.,2008,31(4-6).
85 Xing G F,Wang X L,Wan Y S,et al.Diversity in early crustal evolution:4100Ma zircons inthe Cathaysia Block of southern China.Scientific Reports,2015,4.
86 Yu J H,O'Reilly Y S,Wang L J,et al.Finding of ancient materials in Cathaysia and implication for the formation of Precambrian crust.Chin.Sci.Bull.,2007,52.
87 Yao J,Shu L,Santosh M.Detrital zircon U-Pb geochronology,Hf-isotopes and geochemistry-New clues for the Precambrian crustal evolution of Cathaysia Block,South China.Gondwana Res.,2011,20.
88 李献华,李武显,何斌.华南陆块的形成与Rodinia超大陆聚合-裂解_观察、解释与检验.矿物岩石地球化学通报,2012,31(6).
89 Yu J H,O'Reilly S Y,Zhou M F,et al.U-Pb geochronology and Hf-Nd isotopic geochemistry of the Badu Complex,Southeastern China:implications for the Precambrian crustal evolution and paleogeography of the Cathaysia Block.Precambr.Res.,2012,3-4.
90 Xu Y,Wang C Y,Zhao T.Using detrital zircons from river sands to constrain major tectono-thermal events of the Cathaysia Block,SE China.J.Asian Earth Sci.,2016,124.
91 Li X H,Li Z X,He B.The Early Permian active continental margin and crustal growth of the Cathaysia Block:in situ U-Pb,Lu-Hf and O isotope analyses of detrital zircons.Chem.Geol.,2012,328.
92 Yui T F,Maki K C Y,Hirata T,Chu H T.Detrital zircons from the Tananao Metamorphic Complex of Taiwan:A preliminary study.Geol Soc China Annual Meeting,Tainan,ROC.2010,214.
93 Shao WY,Chung SL,Chen WS.Old continental zircons from a young oceanic arc,eastern Taiwan:Implications for Luzon subduction initiation and Asian accretionary orogeny.Geology,2015,43(6).
94 向磊,舒良树.华南东段前泥盆纪构造演化:来自碎屑锆石的证据.中国科学(地球科学),2010,40(10).
95 Yao J,Shu L,Santosh M.Detrital zircon U-Pb geochronology,Hf-isotopes and geochemistry-New clues for the Precambrian crustal evolution of Cathaysia Block,South China.Gondwana Res.,2011,20.
96 Li X H,Li Z X,Ge W,et al.Neoproterozoic granitoids in SouthChina:crustal melting above a mantle plume at ca.825 Ma?Pre-cambrian Res,2003,122.
97 Li X H,Li W X,Li Z X,et al.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.Precambrian Research,2009,174.
98 Li Z X,Li X,Zhou H,Kinny P D.Grenvillian continental collision in south China:new SHRIMP U-Pb zircon results and implications for the configuration of Rodinia.Geology,2002,30.
99 Lin SF,Xing GF,Davis D W,at al.Appalachian-style multi-terrane Wilson cycle model for the assembly of South China.GSA,2018.
100 Wang YJ,Zhang AM,Cawood FA,et al.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,2013,231.
101 Cawood P A,Wang Y,Xu Y,Zhao G.Locating South China in Rodinia and Gondwana:a fragment of greater India lithosphere?Geology,2013,41.
102 Duan L,Meng Q R.,Wu G L,et al.Detrital zircon evidence for the linkage of the South China block with Gondwanaland in early Palaeozoic time.Geol.Mag,2012,149.
103 Wang W,Zeng M F,Zhou M F,et al.provenance and tectonic setting of Neoproterozoic to early Paleozoic sequences in southeastern South China Block:Constraints on its linkage to western Australia-East Antarctica.Precambrian Research,2018,309.
104 Yang Z,Sun Z,Yang T,Pei J.A long connection(750-380Ma)between South China and Australia:paleomagnetic constraints.Earth Planet.Sci.Lett,2004,220.
105 Yu J H,Liu Q,Hu X M,et al.Late Paleozoic magmatism in South China:Oceanic subduction or intracontinental orogeny?Chin Sci Bull,2012,57.
106 韩发,葛朝华.福建马坑铁矿床海相火山热液-沉积成因-地质地球化学特征.中国地质科学院矿床地质研究所所刊,1983,7(2).
107 王森,张达,吕良冀,等.闽西南晚古生代以来伸展构造演化:中基性岩墙群的年代学、地球化学制约,大地构造与成矿学,2015,39(5).
108 Zhou X M,Li W X.Origin of Late Mesozoic igneous rocks in Southeastern China:implications for lithosphere subduction and underplating of mafic magmas.Tectonophysics,2000,326(3/4).
109 Li Z X,Li X H.Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China:a flat-slab subduction model.Geology,2007,35.
110 Yui T F,Okamoto K.Late Triassic_Late Cretaceous aocretion-subduction in the Taiwan region along the eastern margin of South China-Evidence from zircon SHRIMP dating.Int Geol Rev,2009,51.
111 邵磊,尤洪庆,郝沪军,等.南海东北部中生界岩石学特征及沉积环境.地质评论,2007,53.
112 汪品先.追踪边缘海的生命史:“南海深部计划”的科学目标.科学通报,2012,57(20).
113 闵慧,任建业,高金耀,等.南海北部古俯冲带的位置及其对南海扩张的控制.大地构造与成矿学,2010,34(4).
114 金庆焕,高天钧,等.台湾海峡中、新生代地质构造及油气地质.福州:福建科学技术出版社,1993.
115 Li C F,Xu X,Lin J..Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Ex-pedition 349.Geochem Geophys Geosyst,2014,15.
116 Huang C Y,Yuan P,and Tsao S J.Temporal and spatial records of active arc-continent collision in Taiwan:A synthesis:Geological Society of America Bulletin,2006,118.
117 Yu H S.Paired and Foreland Basin:Insight s on Late Cenozoic Orogeny and Foreland Sedimentation in Taiwan Region7th Chinese Geophysical Societ y Symposium,Programme Preceedings.1998.
118 Yu J H,O'Reilly S Y,Wang L J,Griffin W L,Zhou M F,Zhang M,Shu L S.Components and episodic growth of Precambrian crust in the Cathaysia Block,South China:evidence from U-Pb ages and Hf isotopes of zircons in Neoproterozoic sediments.Precambrian Research,2010,181.
119 Li X H.,Li Z X,Li W X.Detrital zircon U-Pb age and Hf isotope constrains on the generation and reworking of Precambrian continental crust in the Cathaysia Block,South China:a synthesis.Gondwana Res,2014.25.
120 Kemp A I,Hawkesworth C,Paterson B A,Kinny P D..Episodic growth of the Gondwana supercontinent from hafnium and oxygen isotopes in zircon.Nature,2006,439.
121 Zheng Y F,Zhang S B,Zhao Z F,et al.Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China:Implications for growth and reworking of continental crust.Lithos,2007,96.
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