海南荔枝沟中三叠世酸性火山岩年代学、地球化学特征及其构造意义
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摘要
海南岛位于印支与华南陆块的交界地带,构造演化复杂,因此海南岛的拼合历史和构造属性一直备受争议.在海南岛三亚荔枝沟地区新识别出的酸性火山岩对于探讨海南岛早中生代的构造属性具有重要指示意义.LA-ICP-MS锆石U-Pb定年结果显示该套酸性火山岩中流纹岩的成岩年龄为241±6Ma(MSWD=0.9).地球化学特征表明该套火山岩样品的SiO_2含量介于72.34%～77.83%,具较高的Al_2O_3(10.51%～13.53%)、K_2O(2.85%～4.85%)、Na_2O(1.75%～3.79%)含量和A/CNK比值(0.99～2.07),为过铝质钙碱性酸性火山岩.样品稀土元素含量为REE=87×10~(-6)～177×10~(-6),富集轻稀土元素,显示右倾岛弧型稀土元素配分模式,Eu负异常明显.样品富集大离子亲石元素,亏损高场强元素,ε_(Nd)(t)变化于-12.1～-11.3之间,可被解释为变沉积物部分熔融后经历分离结晶作用的产物.区域对比研究表明该套酸性火山岩可与三江地区的金沙江-哀牢山-松马构造带的中三叠世岩浆岩进行类比,应形成于印支与华南陆块汇聚的构造背景.
Hainan Island,which is located between the Indochina and South China blocks,has undergone multiphased structural overprinting and complex tectonic evolution.However,the Late Paleozoic tectonic regime and amalgamation process of the South China with Indochina blocks are still controversial.The newly-identified felsic volcanic rocks in the Lizhigou area are important for understanding the Early Mesozoic tectonic evolution in Hainan.LA-ICP-MS zircon U-Pb dating results show that the representative rhyolite samples yield a weighted mean ~(206)Pb/~(238)U age of 241±6 Ma(MSWD=0.9).These samples contain SiO_2 ranging from 72.34%to 77.83%,Al_2O_3 from 10.51%to 13.53%,K_2 O from 2.85%to 4.85%and Na_2 O from 1.75%to3.79%.The A/CNK values range from 0.99 to 2.07.These samples have REE concentrations of 87×10~(-6) to 177×10~(-6),and Eu/Eu*of 0.49-0.65.They are characterized by subparallel right-sloping REE pattern and enrichment in LREEs and LILEs,and depletion in HFSEs,similar to those of arc volcanics.Theirε_(Nd)(t)values range from-12.1 to-11.3.These felsic volcanic rocks are the products of partial melting of metasediments with significant fractionation crystallization.In combination with other available data,it is inferred that the Lizhigou felsic volcanic rocks can be compared with the Middle-Late Triassic igneous rocks along the Jinshajiang-Ailaoshan-Songma zone,and formed during the assemblage of the South China with Indochina blocks related to East Paleotethyan consumption.
Hainan Island,which is located between the Indochina and South China blocks,has undergone multiphased structural overprinting and complex tectonic evolution.However,the Late Paleozoic tectonic regime and amalgamation process of the South China with Indochina blocks are still controversial.The newly-identified felsic volcanic rocks in the Lizhigou area are important for understanding the Early Mesozoic tectonic evolution in Hainan.LA-ICP-MS zircon U-Pb dating results show that the representative rhyolite samples yield a weighted mean ~(206)Pb/~(238)U age of 241±6 Ma(MSWD=0.9).These samples contain SiO_2 ranging from 72.34%to 77.83%,Al_2O_3 from 10.51%to 13.53%,K_2 O from 2.85%to 4.85%and Na_2 O from 1.75%to3.79%.The A/CNK values range from 0.99 to 2.07.These samples have REE concentrations of 87×10~(-6) to 177×10~(-6),and Eu/Eu*of 0.49-0.65.They are characterized by subparallel right-sloping REE pattern and enrichment in LREEs and LILEs,and depletion in HFSEs,similar to those of arc volcanics.Theirε_(Nd)(t)values range from-12.1 to-11.3.These felsic volcanic rocks are the products of partial melting of metasediments with significant fractionation crystallization.In combination with other available data,it is inferred that the Lizhigou felsic volcanic rocks can be compared with the Middle-Late Triassic igneous rocks along the Jinshajiang-Ailaoshan-Songma zone,and formed during the assemblage of the South China with Indochina blocks related to East Paleotethyan consumption.
引文
Bureau of Geology and Mineral Resources of Guangdong Province,1988.Regional Geology of Guangdong Province.Geological Publishing House,Beijing(in Chinese).
Chen,X.Y.,Wang,Y.J.,Fan,W.M.,et al.,2011.Zircon LA-ICP-MS U-Pb Dating of Granitic Gneisses from Wuzhishan Area,Hainan,and Geological Significances.Geochimica,40(5):454-463(in Chinese with English abstract).
Chen,X.Y.,Wang,Y.J.,Han,H.P.,et al.,2014.Geochemical and Geochronological Characteristics of Triassic Basic Dikes in SW Hainan Island and Its Tectonic Implications.Journal of Jilin University(Earth Science Edition),44(3):835-847(in Chinese with English abstract).
Chen,X.Y.,Wang,Y.J.,Wei,M.,et al.,2006.Microstructural Characteristics of the NW-Trending Shear Zones of Gong'ai Region in Hainan Island and Its 40 Ar-39 Ar Geochronological Constraints.Geotectonica et Metallogenia,30(3):312-319(in Chinese with English abstract).
Ellis,D.J.,Thompson,A.B.,1986.Subsolidus and Partial Melting Reactions in the Quartz-Excess CaO+MgO+Al2O3+SiO2+H2O System under Water-Excess and Water-Deficient Conditions to 10kb:Some Implications for the Origin of Peraluminous Melts from Mafic Rocks.Journal of Petrology,27(1):91-121.
Fan,W.M.,Wang,Y.J.,Zhang,A.M.,et al.,2010.Permian Arc-back-Arc Basin Development along the Ailaoshan Tectonic Zone:Geochemical,Isotopic and Geochronological Evidence from the Mojiang Volcanic Rocks,Southwest China.Lithos,119(3-4):553-568.https://doi.org/10.1016/j.lithos.2010.08.010
He,H.Y.,Wang,Y.J.,Qian,X.,et al.,2018.The BangxiChenxing Tectonic Zone in Hainan Island(South China)as the Eastern Extension of the Song Ma-Ailaoshan Zone:Evidence of Late Paleozoic and Triassic Igneous Rocks.Journal of Asian Earth Sciences,164:274-291.
He,H.Y.,Wang,Y.J.,Zhang,Y.H.,et al.,2017.Fingerprints of the Paleotethyan Back-Arc Basin in Central Hainan,South China:Geochronological and Geochemical Constraints on the Carboniferous Metabasites.International Journal of Earth Sciences,107(2):553-570.
Healy,B.,Collins,W.J.,Richards,S.W.,2004.A Hybrid Origin for Lachlan S-Type Granites:The Murrumbidgee Batholith Example.Lithos,78(1-2):197-216.https://doi.org/10.1016/j.lithos.2004.04.047
Hu,N.,Zhang,R.J.,Feng,S.N.,2002.Study on DevonianCarboniferous Boundary in Hainan Island,South China.Chinese Journal of Geology,37(3):313-319,387(in Chinese with English abstract).
Jian,P.,Liu,D.Y.,Kr9ner,A.,et al.,2009.Devonian to Permian Plate Tectonic Cycle of the Paleo-Tethys Orogen in Southwest China(II):Insights from Zircon Ages of Ophiolites,Arc/back-Arc Assemblages and withinPlate Igneous Rocks and Generation of the Emeishan CFB Province.Lithos,113(3-4):767-784.https://doi.org/10.1016/j.lithos.2009.04.006
Lepvrier,C.,Maluski,H.,van Tich,V.,et al.,2004.The Early Triassic Indosinian Orogeny in Vietnam(Truong Son Belt and Kontum Massif);Implications for the Geodynamic Evolution of Indochina.Tectonophysics,393(1-4):87-118.https://doi.org/10.1016/j.tecto.2004.07.030
Li,S.B.,He,H.Y.,Qian,X.,et al.,2018.Carboniferous Arc Setting in Central Hainan:Geochronological and Geochemical Evidences on the Andesitic and Dacitic Rocks.Journal of Earth Science,29(2):265-279.https://doi.org/10.1007/s12583-017-0936-0
Li,S.X.,Yun,Y.,Fan,Y.,et al.,2005.Zircon U-Pb Age and Its Geological Significance for Qiongzhong Pluton in Qiongzhong Area,Hainan Island.Geotectonica et Metallogenia,29(2):227-233,241(in Chinese with English abstract).
Li,X.H.,Li,Z.X.,Li,W.X.,et al.,2006.Initiation of the Indosinian Orogeny in South China:Evidence for a Permian Magmatic Arc on Hainan Island.The Journal of Geology,114(3):341-353.https://doi.org/10.1086/501222
Li,X.H.,Qi,C.S.,Liu,Y.,et al.,2005.Petrogenesis of the Neoproterozoic Bimodal Volcanic Rocks along the Western Margin of the Yangtze Block:New Constraints from Hf Isotopes and Fe/Mn Ratios.Chinese Science Bulletin,50(21):2481-2486.
Li,X.H.,Zhou,H.W.,Chung,S.L.,et al.,2002.Geochemical and Sm-Nd Isotopic Characteristics of Metabasites from Central Hainan Island,South China and Their Tectonic Significance.The Island Arc,11(3):193-205.https://doi.org/10.1046/j.1440-1738.2002.00365.x
Li,X.H.,Zhou,H.W.,Ding,S.J.,et al.,2000.Mid Ocean Ridge Metabasic Volcanic Rocks of Hainan Island:Paleo-Tethyan Oceanic Crust Slices?Chinese Science Bulletin,45(1):84-89(in Chinese).
Liu,H.C.,Wang,Y.J.,Cawood,P.A.,et al.,2015.Record of Tethyan Ocean Closure and Indosinian Collision along the Ailaoshan Suture Zone(SW China).Gondwana Research,27(3):1292-1306.
Liu,H.C.,Wang,Y.J.,Fan,W.M.,et al.,2014.Petrogenesis and Tectonic Implications of Late-Triassic HighεNd(t)-εHf(t)Granites in the Ailaoshan Tectonic Zone(SWChina).Science China Earth Sciences,57(9):2181-2194.https://doi.org/10.1007/s11430-014-4854-z
Liu,H.C.,Wang,Y.J.,Guo,X.F.,et al.,2017.Late Triassic Post-Collisional Slab Break-off along the Ailaoshan Suture:Insights from OIB-Like Amphibolites and Associated Felsic Rocks.International Journal of Earth Sciences,106(4):1359-1373.
Liu,Y.,Liu,H.C.,Li,X.H.,1996.Simultaneous and Precise Determination of 40Trace Elements in Rock Samples Using ICP-MS.Geochimica,25(6):552-558(in Chinese with English abstract).
Long,W.G.,Fu,C.R.,Zhu,Y.H.,2002.Disintegration of the Baoban Group in Huangzhuling Area of Eastern Hainan Island.Journal of Stratigraphy,26(3):212-215(in Chinese with English abstract).
Long,W.G.,Tong,J.N.,Zhu,Y.H.,et al.,2007.Discovery of the Permian in the Danzhou-Tunchang Area of Hainan Island and Its Geological Significance.Geology and Mineral Resources of South China,23(1):38-45(in Chinese with English abstract).
Ludwig,K.R.,2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center,California,Berkeley.
Ma,D.Q.,Huang,X.D.,Xiao,Z.F.,et al.,1998.Crystallized Basement in Hainan Island:Sequence and Epoch of the Baoban Group.China University of Geosciences Press,Wuhan,1-52(in Chinese).
Maitre,R.W.L.,Bateman,P.,Dudek,A.,et al.,1989.A Classification of Igneous Rocks and Glossary of Terms.Blackwell Science Publication,Oxford.
Pati1o Douce,A.E.,Humphreys,E.D.,Dana Johnston,A.,1990.Anatexis and Metamorphism in Tectonically Thickened Continental Crust Exemplified by the Sevier Hinterland,Western North America.Earth and Planetary Science Letters,97(3-4):290-315.https://doi.org/10.1016/0012-821x(90)90048-3
Pati1o Douce,A.E.,Johnston,A.D.,1991.Phase Equilibria and Melt Productivity in the Pelitic System:Implications for the Origin of Peraluminous Granitoids and Aluminous Granulites.Contributions to Mineralogy and Petrology,107(2):202-218.https://doi.org/10.1007/bf00310707
Pearce,J.A.,1996.Sources and Settings of Granitic Rocks.Episodes,19:120-125.
Peng,T.P.,Wang,Y.J.,Fan,W.M.,et al.,2006.SHRIMP Ziron U-Pb Geochronology of Early Mesozoic Felsic Igneous Rocks from the Southern Lancangjiang and Its Tectonic Implications.Science China Earth Sciences,49(10):1032-1042.https://doi.org/10.1007/s11430-006-1032-y
Peng,T.P.,Wilde,S.A.,Wang,Y.J.,et al.,2013.Mid-Triassic Felsic Igneous Rocks from the Southern Lancangjiang Zone,SW China:Petrogenesis and Implications for the Evolution of Paleo-Tethys.Lithos,168-169:15-32.https://doi.org/10.1016/j.lithos.2013.01.015
Shen,B.Y.,Liu,B.,Liu,H.L.,et al.,2016.Xiaomei Ductile Shear Zone on Hainan Island in a Nanoscale Perspective.Earth Science,41(9):1489-1498(in Chinese with English abstract).
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Sylvester,P.J.,1998.Post-Collisional Strongly Peraluminous Granites.Lithos,45(1-4):29-44.https://doi.org/10.1016/s0024-4937(98)00024-3
Tang,L.M.,2010.Magmatic Evidence of Two Tectonic Extension Events during the Mesozoic in Hainan Island&Geodynamic Implications(Dissertation).Zhejiang University,Hangzhou(in Chinese with English abstract).
Tang,L.M.,Chen,H.L.,Dong,C.W.,et al.,2013.Middle Triassic Post-Orogenic Extension on Hainan Island:Chronology and Geochemistry Constraints of Bimodal Intrusive Rocks.Science China Earth Science,43(3):433-445(in Chinese).
Wang,B.D.,Wang,L.Q.,Chen,J.L.,et al.,2014.Triassic Three-Stage Collision in the Paleo-Tethys:Constraints from Magmatism in the Jiangda-Deqen-Weixi Continental Margin Arc,SW China.Gondwana Research,26(2):475-491.https://doi.org/10.1016/j.gr.2013.07.023
Wang,Y.J.,Fan,W.M.,Sun,M.,et al.,2007.Geochronological,Geochemical and Geothermal Constraints on Petrogenesis of the Indosinian Peraluminous Granites in the South China Block:A Case Study in the Hunan Province.Lithos,96(3-4):475-502.https://doi.org/10.1016/j.lithos.2006.11.010
Wang,Y.J.,He,H.Y.,Cawood,P.A.,et al.,2016.Geochronological,Elemental and Sr-Nd-Hf-O Isotopic Constraints on the Petrogenesis of the Triassic Post-Collisional Granitic Rocks in NW Thailand and Its Paleotethyan Implications.Lithos,266-267:264-286.
Wang,Y.J.,Li,S.B.,Ma,L.Y.,et al.,2015.Geochronological and Geochemical Constraints on the Petrogenesis of Early Eocene Metagabbroic Rocks in Nabang(SWYunnan)and Its Implications on the Neotethyan Slab Subduction.Gondwana Research,27(4):1474-1486.
Wang,Y.J.,Qian,X.,Cawood,P.A.,et al.,2018.Closure of the East Paleotethyan Ocean and Amalgamation of the Eastern Cimmerian and Southeast Asia Continental Fragments.Earth-Science Reviews,186:195-230.
Wang,Y.J.,Zhang,A.M.,Cawood,P.A.,et al.,2013.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
Wang,Y.J.,Zhang,A.M.,Fan,W.M.,et al.,2010.Petrogenesis of Late Triassic Post-Collisional Basaltic Rocks of the Lancangjiang Tectonic Zone,Southwest China,and Tectonic Implications for the Evolution of the Eastern Paleotethys:Geochronological and Geochemical Constraints.Lithos,120(3-4):529-546.https://doi.org/10.1016/j.lithos.2010.09.012
Wang,X.F.,Ma,D.Q.,Jiang,D.H.,1991.Geology of Hainan Island:Structural Geology.Geological Publishing House,Beijing,10-100(in Chinese).
Wen,S.N.,Liang,X.Q.,Fan,W.M.,et al.,2013.Zircon U-Pb Ages,Hf Isotopic Composition of Zhizhong Granitic Intrusion in Ledong Area of Hainan Island and Their Tectonic Implications.Geotectonica et Metallogenia,37(2):294-307(in Chinese with English abstract).
Whalen,J.B.,Currie,K.L.,Chappell,B.W.,1987.A-Type Granites:Geochemical Characteristics,Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419.https://doi.org/10.1007/bf00402202
Wright,J.B.,1969.A Simple Alkalinity Ratio and Its Application to Questions of Non-Orogenic Granite Genesis.Geological Magazine,106(4):370.https://doi.org/10.1017/s0016756800058222
Xia,X.P.,Sun,M.,Zhao,G.C.,et al.,2004.Spot Zircon U-Pb Isotope Analysis by ICP-MS Coupled with a Frequency Quintupled(213nm)Nd-YAG Laser System.Geochemical Journal,38(2):191-200.https://doi.org/10.2343/geochemj.38.191
Xia,B.D.,Shi,G.Y.,Fang,Z.,et al.,1991.The Late Palaeozoic Rifting in Hainan Island,China.Acta Geologica Sinica,65(2):103-115(in Chinese with English abstract).
Xia,B.D.,Yu,J.H.,Fang,Z.,et al.,1990.Geochemical Characteristics and Origin of the Hercynian-Indosinian Granites of Hainan Island,China.Geochimica,19(4):365-373(in Chinese with English abstract).
Xie,C.F.,Zhu,J.C.,Zhao,Z.J.,et al.,2005.Zircon SHRIMPU-Pb Age Dating of Garnet-Acmite Syenite:Constraints on the Hercynian-Indosinian Tectonic Evolution of Hainan Island.Geological Journal of China Universities,11(1):47-57(in Chinese with English abstract).
Yang,J.H.,Wu,F.Y.,Chung,S.L.,et al.,2006.A Hybrid Origin for the Qianshan A-Type Granite,Northeast China:Geochemical and Sr-Nd-Hf Isotopic Evidence.Lithos,89(1-2):89-106.https://doi.org/10.1016/j.lithos.2005.10.002
Zen,E.A.,1986.Aluminum Enrichment in Silicate Melts by Fractional Crystallization:Some Mineralogic and Petrographic Constraints.Journal of Petrology,27(5):1095-1117.https://doi.org/10.1093/petrology/27.5.1095
Zhang,F.F.,Wang,Y.J.,Chen,X.Y.,et al.,2011.Triassic High-Strain Shear Zones in Hainan Island(South China)and Their Implications on the Amalgamation of the Indochina and South China Blocks:Kinematic and40 Ar/39 Ar Geochronological Constraints.Gondwana Research,19(4):910-925.https://doi.org/10.1016/j.gr.2010.11.002
Zhong,C.T.,Deng,J.F.,Wan,Y.S.,et al.,2007.Magma Recording of Paleoproterozoic Orogeny in Central Segment of Northern Margin of North China Craton:Geochemical Characteristics and Zircon SHRIMP Dating of S-Type Granitoids.Geochimica,36(6):585-600(in Chinese with English abstract).
Zhou,Z.M.,Xie,C.F.,Xu,Q.,et al.,2011.Geological and Geochemical Characteristics of Middle Triassic SyeniteGranite Suite in Hainan Island and Its Geotectonic Implications.Geological Review,57(4):515-531(in Chinese with English abstract).
Zi,J.W.,Cawood,P.A.,Fan,W.M.,et al.,2012.Generation of Early Indosinian Enriched Mantle-Derived Granitoid Pluton in the Sanjiang Orogen(SW China)in Response to Closure of the Paleo-Tethys.Lithos,140-141:166-182.https://doi.org/10.1016/j.lithos.2012.02.006
陈新跃,王岳军,范蔚茗,等,2011.海南五指山地区花岗片麻岩锆石LA-ICP-MS U-Pb年代学特征及其地质意义.地球化学,40(5):454-463.
陈新跃,王岳军,韩会平,等,2014.琼西南三叠纪基性岩脉年代学、地球化学特征及其构造意义.吉林大学学报(地球科学版),44(3):835-847.
陈新跃,王岳军,韦牧,等,2006.海南公爱NW向韧性剪切带构造特征及其40 Ar-39 Ar年代学约束.大地构造与成矿学,30(3):312-319.
广东省地质矿产局,1988.广东省区域地质志.北京:地质出版社.
胡宁,张仁杰,冯少南,2002.海南岛泥盆-石炭系界线研究.地质科学,37(3):313-319,387.
李孙雄,云平,范渊,等,2005.海南岛琼中地区琼中岩体锆石U-Pb年龄及其地质意义.大地构造与成矿学,29(2):227-233,241.
李献华,周汉文,丁式江,等,2000.海南岛洋中脊型变质基性岩:古特提斯洋壳的残片?科学通报,45(1):84-89.
刘颖,刘海臣,李献华,1996.用ICP-MS准确测定岩石样品中的40余种微量元素.地球化学,25(6):552-558.
龙文国,符策锐,朱耀河,2002.海南岛东部黄竹岭地区“抱板群”的解体.地层学杂志,26(3):212-215.
龙文国,童金南,朱耀河,等,2007.海南儋州-屯昌地区二叠纪地层的发现及其意义.华南地质与矿产,23(1):38-45.
马大铨,黄香定,肖志发,等,1998.海南岛结晶基底-抱板群层序与时代.武汉:中国地质大学出版,1-52.
沈宝云,刘兵,刘海龄,等,2016.海南岛小妹韧性剪切带的纳米尺度.地球科学,41(9):1489-1498.
唐立梅,2010.海南岛中生代两期构造伸展作用的岩浆记录及其大陆动力学意义(博士学位论文).杭州:浙江大学.
唐立梅,陈汉林,董传万,等,2013.海南岛中三叠世造山后伸展作用:双峰式侵入岩的年代学及地球化学制约.中国科学:地球科学,43(3):433-445.
汪啸风,马大铨,蒋大海,1991.海南岛地质(三)---构造地质.北京:地质出版社,10-100.
温淑女,梁新权,范蔚茗,等,2013.海南岛乐东地区志仲岩体锆石U-Pb年代学、Hf同位素研究及其构造意义.大地构造与成矿学,37(2):294-307.
夏邦栋,施光宇,方中,等,1991.海南岛晚古生代裂谷作用.地质学报,65(2):103-115.
夏邦栋,于津海,方中,等,1990.海南岛海西-印支期花岗岩的地球化学特征及成因.地球化学,19(4):365-373.
谢才富,朱金初,赵子杰,等,2005.三亚石榴霓辉石正长岩的锆石SHRIMP U-Pb年龄:对海南岛海西-印支期构造演化的制约.高校地质学报,11(1):47-57.
钟长汀,邓晋福,万渝生,等,2007.华北克拉通北缘中段古元古代造山作用的岩浆记录:S型花岗岩地球化学特征及锆石SHRIMP年龄.地球化学,36(6):585-600.
周佐民,谢才富,徐倩,等,2011.海南岛中三叠世正长岩-花岗岩套的地质地球化学特征与构造意义.地质论评,57(4):515-531.
Chen,X.Y.,Wang,Y.J.,Fan,W.M.,et al.,2011.Zircon LA-ICP-MS U-Pb Dating of Granitic Gneisses from Wuzhishan Area,Hainan,and Geological Significances.Geochimica,40(5):454-463(in Chinese with English abstract).
Chen,X.Y.,Wang,Y.J.,Han,H.P.,et al.,2014.Geochemical and Geochronological Characteristics of Triassic Basic Dikes in SW Hainan Island and Its Tectonic Implications.Journal of Jilin University(Earth Science Edition),44(3):835-847(in Chinese with English abstract).
Chen,X.Y.,Wang,Y.J.,Wei,M.,et al.,2006.Microstructural Characteristics of the NW-Trending Shear Zones of Gong'ai Region in Hainan Island and Its 40 Ar-39 Ar Geochronological Constraints.Geotectonica et Metallogenia,30(3):312-319(in Chinese with English abstract).
Ellis,D.J.,Thompson,A.B.,1986.Subsolidus and Partial Melting Reactions in the Quartz-Excess CaO+MgO+Al2O3+SiO2+H2O System under Water-Excess and Water-Deficient Conditions to 10kb:Some Implications for the Origin of Peraluminous Melts from Mafic Rocks.Journal of Petrology,27(1):91-121.
Fan,W.M.,Wang,Y.J.,Zhang,A.M.,et al.,2010.Permian Arc-back-Arc Basin Development along the Ailaoshan Tectonic Zone:Geochemical,Isotopic and Geochronological Evidence from the Mojiang Volcanic Rocks,Southwest China.Lithos,119(3-4):553-568.https://doi.org/10.1016/j.lithos.2010.08.010
He,H.Y.,Wang,Y.J.,Qian,X.,et al.,2018.The BangxiChenxing Tectonic Zone in Hainan Island(South China)as the Eastern Extension of the Song Ma-Ailaoshan Zone:Evidence of Late Paleozoic and Triassic Igneous Rocks.Journal of Asian Earth Sciences,164:274-291.
He,H.Y.,Wang,Y.J.,Zhang,Y.H.,et al.,2017.Fingerprints of the Paleotethyan Back-Arc Basin in Central Hainan,South China:Geochronological and Geochemical Constraints on the Carboniferous Metabasites.International Journal of Earth Sciences,107(2):553-570.
Healy,B.,Collins,W.J.,Richards,S.W.,2004.A Hybrid Origin for Lachlan S-Type Granites:The Murrumbidgee Batholith Example.Lithos,78(1-2):197-216.https://doi.org/10.1016/j.lithos.2004.04.047
Hu,N.,Zhang,R.J.,Feng,S.N.,2002.Study on DevonianCarboniferous Boundary in Hainan Island,South China.Chinese Journal of Geology,37(3):313-319,387(in Chinese with English abstract).
Jian,P.,Liu,D.Y.,Kr9ner,A.,et al.,2009.Devonian to Permian Plate Tectonic Cycle of the Paleo-Tethys Orogen in Southwest China(II):Insights from Zircon Ages of Ophiolites,Arc/back-Arc Assemblages and withinPlate Igneous Rocks and Generation of the Emeishan CFB Province.Lithos,113(3-4):767-784.https://doi.org/10.1016/j.lithos.2009.04.006
Lepvrier,C.,Maluski,H.,van Tich,V.,et al.,2004.The Early Triassic Indosinian Orogeny in Vietnam(Truong Son Belt and Kontum Massif);Implications for the Geodynamic Evolution of Indochina.Tectonophysics,393(1-4):87-118.https://doi.org/10.1016/j.tecto.2004.07.030
Li,S.B.,He,H.Y.,Qian,X.,et al.,2018.Carboniferous Arc Setting in Central Hainan:Geochronological and Geochemical Evidences on the Andesitic and Dacitic Rocks.Journal of Earth Science,29(2):265-279.https://doi.org/10.1007/s12583-017-0936-0
Li,S.X.,Yun,Y.,Fan,Y.,et al.,2005.Zircon U-Pb Age and Its Geological Significance for Qiongzhong Pluton in Qiongzhong Area,Hainan Island.Geotectonica et Metallogenia,29(2):227-233,241(in Chinese with English abstract).
Li,X.H.,Li,Z.X.,Li,W.X.,et al.,2006.Initiation of the Indosinian Orogeny in South China:Evidence for a Permian Magmatic Arc on Hainan Island.The Journal of Geology,114(3):341-353.https://doi.org/10.1086/501222
Li,X.H.,Qi,C.S.,Liu,Y.,et al.,2005.Petrogenesis of the Neoproterozoic Bimodal Volcanic Rocks along the Western Margin of the Yangtze Block:New Constraints from Hf Isotopes and Fe/Mn Ratios.Chinese Science Bulletin,50(21):2481-2486.
Li,X.H.,Zhou,H.W.,Chung,S.L.,et al.,2002.Geochemical and Sm-Nd Isotopic Characteristics of Metabasites from Central Hainan Island,South China and Their Tectonic Significance.The Island Arc,11(3):193-205.https://doi.org/10.1046/j.1440-1738.2002.00365.x
Li,X.H.,Zhou,H.W.,Ding,S.J.,et al.,2000.Mid Ocean Ridge Metabasic Volcanic Rocks of Hainan Island:Paleo-Tethyan Oceanic Crust Slices?Chinese Science Bulletin,45(1):84-89(in Chinese).
Liu,H.C.,Wang,Y.J.,Cawood,P.A.,et al.,2015.Record of Tethyan Ocean Closure and Indosinian Collision along the Ailaoshan Suture Zone(SW China).Gondwana Research,27(3):1292-1306.
Liu,H.C.,Wang,Y.J.,Fan,W.M.,et al.,2014.Petrogenesis and Tectonic Implications of Late-Triassic HighεNd(t)-εHf(t)Granites in the Ailaoshan Tectonic Zone(SWChina).Science China Earth Sciences,57(9):2181-2194.https://doi.org/10.1007/s11430-014-4854-z
Liu,H.C.,Wang,Y.J.,Guo,X.F.,et al.,2017.Late Triassic Post-Collisional Slab Break-off along the Ailaoshan Suture:Insights from OIB-Like Amphibolites and Associated Felsic Rocks.International Journal of Earth Sciences,106(4):1359-1373.
Liu,Y.,Liu,H.C.,Li,X.H.,1996.Simultaneous and Precise Determination of 40Trace Elements in Rock Samples Using ICP-MS.Geochimica,25(6):552-558(in Chinese with English abstract).
Long,W.G.,Fu,C.R.,Zhu,Y.H.,2002.Disintegration of the Baoban Group in Huangzhuling Area of Eastern Hainan Island.Journal of Stratigraphy,26(3):212-215(in Chinese with English abstract).
Long,W.G.,Tong,J.N.,Zhu,Y.H.,et al.,2007.Discovery of the Permian in the Danzhou-Tunchang Area of Hainan Island and Its Geological Significance.Geology and Mineral Resources of South China,23(1):38-45(in Chinese with English abstract).
Ludwig,K.R.,2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center,California,Berkeley.
Ma,D.Q.,Huang,X.D.,Xiao,Z.F.,et al.,1998.Crystallized Basement in Hainan Island:Sequence and Epoch of the Baoban Group.China University of Geosciences Press,Wuhan,1-52(in Chinese).
Maitre,R.W.L.,Bateman,P.,Dudek,A.,et al.,1989.A Classification of Igneous Rocks and Glossary of Terms.Blackwell Science Publication,Oxford.
Pati1o Douce,A.E.,Humphreys,E.D.,Dana Johnston,A.,1990.Anatexis and Metamorphism in Tectonically Thickened Continental Crust Exemplified by the Sevier Hinterland,Western North America.Earth and Planetary Science Letters,97(3-4):290-315.https://doi.org/10.1016/0012-821x(90)90048-3
Pati1o Douce,A.E.,Johnston,A.D.,1991.Phase Equilibria and Melt Productivity in the Pelitic System:Implications for the Origin of Peraluminous Granitoids and Aluminous Granulites.Contributions to Mineralogy and Petrology,107(2):202-218.https://doi.org/10.1007/bf00310707
Pearce,J.A.,1996.Sources and Settings of Granitic Rocks.Episodes,19:120-125.
Peng,T.P.,Wang,Y.J.,Fan,W.M.,et al.,2006.SHRIMP Ziron U-Pb Geochronology of Early Mesozoic Felsic Igneous Rocks from the Southern Lancangjiang and Its Tectonic Implications.Science China Earth Sciences,49(10):1032-1042.https://doi.org/10.1007/s11430-006-1032-y
Peng,T.P.,Wilde,S.A.,Wang,Y.J.,et al.,2013.Mid-Triassic Felsic Igneous Rocks from the Southern Lancangjiang Zone,SW China:Petrogenesis and Implications for the Evolution of Paleo-Tethys.Lithos,168-169:15-32.https://doi.org/10.1016/j.lithos.2013.01.015
Shen,B.Y.,Liu,B.,Liu,H.L.,et al.,2016.Xiaomei Ductile Shear Zone on Hainan Island in a Nanoscale Perspective.Earth Science,41(9):1489-1498(in Chinese with English abstract).
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Sylvester,P.J.,1998.Post-Collisional Strongly Peraluminous Granites.Lithos,45(1-4):29-44.https://doi.org/10.1016/s0024-4937(98)00024-3
Tang,L.M.,2010.Magmatic Evidence of Two Tectonic Extension Events during the Mesozoic in Hainan Island&Geodynamic Implications(Dissertation).Zhejiang University,Hangzhou(in Chinese with English abstract).
Tang,L.M.,Chen,H.L.,Dong,C.W.,et al.,2013.Middle Triassic Post-Orogenic Extension on Hainan Island:Chronology and Geochemistry Constraints of Bimodal Intrusive Rocks.Science China Earth Science,43(3):433-445(in Chinese).
Wang,B.D.,Wang,L.Q.,Chen,J.L.,et al.,2014.Triassic Three-Stage Collision in the Paleo-Tethys:Constraints from Magmatism in the Jiangda-Deqen-Weixi Continental Margin Arc,SW China.Gondwana Research,26(2):475-491.https://doi.org/10.1016/j.gr.2013.07.023
Wang,Y.J.,Fan,W.M.,Sun,M.,et al.,2007.Geochronological,Geochemical and Geothermal Constraints on Petrogenesis of the Indosinian Peraluminous Granites in the South China Block:A Case Study in the Hunan Province.Lithos,96(3-4):475-502.https://doi.org/10.1016/j.lithos.2006.11.010
Wang,Y.J.,He,H.Y.,Cawood,P.A.,et al.,2016.Geochronological,Elemental and Sr-Nd-Hf-O Isotopic Constraints on the Petrogenesis of the Triassic Post-Collisional Granitic Rocks in NW Thailand and Its Paleotethyan Implications.Lithos,266-267:264-286.
Wang,Y.J.,Li,S.B.,Ma,L.Y.,et al.,2015.Geochronological and Geochemical Constraints on the Petrogenesis of Early Eocene Metagabbroic Rocks in Nabang(SWYunnan)and Its Implications on the Neotethyan Slab Subduction.Gondwana Research,27(4):1474-1486.
Wang,Y.J.,Qian,X.,Cawood,P.A.,et al.,2018.Closure of the East Paleotethyan Ocean and Amalgamation of the Eastern Cimmerian and Southeast Asia Continental Fragments.Earth-Science Reviews,186:195-230.
Wang,Y.J.,Zhang,A.M.,Cawood,P.A.,et al.,2013.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
Wang,Y.J.,Zhang,A.M.,Fan,W.M.,et al.,2010.Petrogenesis of Late Triassic Post-Collisional Basaltic Rocks of the Lancangjiang Tectonic Zone,Southwest China,and Tectonic Implications for the Evolution of the Eastern Paleotethys:Geochronological and Geochemical Constraints.Lithos,120(3-4):529-546.https://doi.org/10.1016/j.lithos.2010.09.012
Wang,X.F.,Ma,D.Q.,Jiang,D.H.,1991.Geology of Hainan Island:Structural Geology.Geological Publishing House,Beijing,10-100(in Chinese).
Wen,S.N.,Liang,X.Q.,Fan,W.M.,et al.,2013.Zircon U-Pb Ages,Hf Isotopic Composition of Zhizhong Granitic Intrusion in Ledong Area of Hainan Island and Their Tectonic Implications.Geotectonica et Metallogenia,37(2):294-307(in Chinese with English abstract).
Whalen,J.B.,Currie,K.L.,Chappell,B.W.,1987.A-Type Granites:Geochemical Characteristics,Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419.https://doi.org/10.1007/bf00402202
Wright,J.B.,1969.A Simple Alkalinity Ratio and Its Application to Questions of Non-Orogenic Granite Genesis.Geological Magazine,106(4):370.https://doi.org/10.1017/s0016756800058222
Xia,X.P.,Sun,M.,Zhao,G.C.,et al.,2004.Spot Zircon U-Pb Isotope Analysis by ICP-MS Coupled with a Frequency Quintupled(213nm)Nd-YAG Laser System.Geochemical Journal,38(2):191-200.https://doi.org/10.2343/geochemj.38.191
Xia,B.D.,Shi,G.Y.,Fang,Z.,et al.,1991.The Late Palaeozoic Rifting in Hainan Island,China.Acta Geologica Sinica,65(2):103-115(in Chinese with English abstract).
Xia,B.D.,Yu,J.H.,Fang,Z.,et al.,1990.Geochemical Characteristics and Origin of the Hercynian-Indosinian Granites of Hainan Island,China.Geochimica,19(4):365-373(in Chinese with English abstract).
Xie,C.F.,Zhu,J.C.,Zhao,Z.J.,et al.,2005.Zircon SHRIMPU-Pb Age Dating of Garnet-Acmite Syenite:Constraints on the Hercynian-Indosinian Tectonic Evolution of Hainan Island.Geological Journal of China Universities,11(1):47-57(in Chinese with English abstract).
Yang,J.H.,Wu,F.Y.,Chung,S.L.,et al.,2006.A Hybrid Origin for the Qianshan A-Type Granite,Northeast China:Geochemical and Sr-Nd-Hf Isotopic Evidence.Lithos,89(1-2):89-106.https://doi.org/10.1016/j.lithos.2005.10.002
Zen,E.A.,1986.Aluminum Enrichment in Silicate Melts by Fractional Crystallization:Some Mineralogic and Petrographic Constraints.Journal of Petrology,27(5):1095-1117.https://doi.org/10.1093/petrology/27.5.1095
Zhang,F.F.,Wang,Y.J.,Chen,X.Y.,et al.,2011.Triassic High-Strain Shear Zones in Hainan Island(South China)and Their Implications on the Amalgamation of the Indochina and South China Blocks:Kinematic and40 Ar/39 Ar Geochronological Constraints.Gondwana Research,19(4):910-925.https://doi.org/10.1016/j.gr.2010.11.002
Zhong,C.T.,Deng,J.F.,Wan,Y.S.,et al.,2007.Magma Recording of Paleoproterozoic Orogeny in Central Segment of Northern Margin of North China Craton:Geochemical Characteristics and Zircon SHRIMP Dating of S-Type Granitoids.Geochimica,36(6):585-600(in Chinese with English abstract).
Zhou,Z.M.,Xie,C.F.,Xu,Q.,et al.,2011.Geological and Geochemical Characteristics of Middle Triassic SyeniteGranite Suite in Hainan Island and Its Geotectonic Implications.Geological Review,57(4):515-531(in Chinese with English abstract).
Zi,J.W.,Cawood,P.A.,Fan,W.M.,et al.,2012.Generation of Early Indosinian Enriched Mantle-Derived Granitoid Pluton in the Sanjiang Orogen(SW China)in Response to Closure of the Paleo-Tethys.Lithos,140-141:166-182.https://doi.org/10.1016/j.lithos.2012.02.006
陈新跃,王岳军,范蔚茗,等,2011.海南五指山地区花岗片麻岩锆石LA-ICP-MS U-Pb年代学特征及其地质意义.地球化学,40(5):454-463.
陈新跃,王岳军,韩会平,等,2014.琼西南三叠纪基性岩脉年代学、地球化学特征及其构造意义.吉林大学学报(地球科学版),44(3):835-847.
陈新跃,王岳军,韦牧,等,2006.海南公爱NW向韧性剪切带构造特征及其40 Ar-39 Ar年代学约束.大地构造与成矿学,30(3):312-319.
广东省地质矿产局,1988.广东省区域地质志.北京:地质出版社.
胡宁,张仁杰,冯少南,2002.海南岛泥盆-石炭系界线研究.地质科学,37(3):313-319,387.
李孙雄,云平,范渊,等,2005.海南岛琼中地区琼中岩体锆石U-Pb年龄及其地质意义.大地构造与成矿学,29(2):227-233,241.
李献华,周汉文,丁式江,等,2000.海南岛洋中脊型变质基性岩:古特提斯洋壳的残片?科学通报,45(1):84-89.
刘颖,刘海臣,李献华,1996.用ICP-MS准确测定岩石样品中的40余种微量元素.地球化学,25(6):552-558.
龙文国,符策锐,朱耀河,2002.海南岛东部黄竹岭地区“抱板群”的解体.地层学杂志,26(3):212-215.
龙文国,童金南,朱耀河,等,2007.海南儋州-屯昌地区二叠纪地层的发现及其意义.华南地质与矿产,23(1):38-45.
马大铨,黄香定,肖志发,等,1998.海南岛结晶基底-抱板群层序与时代.武汉:中国地质大学出版,1-52.
沈宝云,刘兵,刘海龄,等,2016.海南岛小妹韧性剪切带的纳米尺度.地球科学,41(9):1489-1498.
唐立梅,2010.海南岛中生代两期构造伸展作用的岩浆记录及其大陆动力学意义(博士学位论文).杭州:浙江大学.
唐立梅,陈汉林,董传万,等,2013.海南岛中三叠世造山后伸展作用:双峰式侵入岩的年代学及地球化学制约.中国科学:地球科学,43(3):433-445.
汪啸风,马大铨,蒋大海,1991.海南岛地质(三)---构造地质.北京:地质出版社,10-100.
温淑女,梁新权,范蔚茗,等,2013.海南岛乐东地区志仲岩体锆石U-Pb年代学、Hf同位素研究及其构造意义.大地构造与成矿学,37(2):294-307.
夏邦栋,施光宇,方中,等,1991.海南岛晚古生代裂谷作用.地质学报,65(2):103-115.
夏邦栋,于津海,方中,等,1990.海南岛海西-印支期花岗岩的地球化学特征及成因.地球化学,19(4):365-373.
谢才富,朱金初,赵子杰,等,2005.三亚石榴霓辉石正长岩的锆石SHRIMP U-Pb年龄:对海南岛海西-印支期构造演化的制约.高校地质学报,11(1):47-57.
钟长汀,邓晋福,万渝生,等,2007.华北克拉通北缘中段古元古代造山作用的岩浆记录:S型花岗岩地球化学特征及锆石SHRIMP年龄.地球化学,36(6):585-600.
周佐民,谢才富,徐倩,等,2011.海南岛中三叠世正长岩-花岗岩套的地质地球化学特征与构造意义.地质论评,57(4):515-531.