福建石狮白垩纪花岗岩与中基性脉岩的年代学与地球化学
|
摘要
在我国华南地区广泛发育了白垩纪岩浆活动,形成了大面积的花岗岩和多期侵位的中基性和酸性脉岩。其中中基性脉岩被认为是华南白垩纪多期伸展作用的标志之一。本文对采自福建沿海石狮地区的石狮和东埔两地的花岗岩和侵入的中基性脉岩进行了锆石U-Pb年代学和Hf同位素以及岩石元素地球化学研究。石狮地区的花岗岩和花岗闪长岩为中钾-高钾钙碱性、弱过铝质岩石,2个锆石U-Pb年龄分别为105.3±1.0Ma和105.1±0.5Ma,2个花岗岩的锆石εHf(t)为-0.9~+2.0;侵入的脉岩为辉绿岩和闪长岩,属于准铝质中钾-高钾钙碱性岩石,2个闪长岩的锆石U-Pb年龄分别89.5±1.5Ma和96.1±1.2Ma,脉岩的εHf(t)为+1.3~+5.0。石狮地区花岗岩和脉岩显示轻重稀土中等分馏和弱的Eu异常,花岗岩稀土总量明显低于脉岩,岩石大离子亲石元素富集、高场强元素亏损,显示岛弧岩浆岩的地球化学特征;微量元素判别(Ta/Hf-Th/Hf,Zr-Zr/Y)表明石狮地区的岩脉产于大陆边缘裂谷环境或板内构造环境,脉岩应是古太平洋俯冲的大陆边缘背景之上,俯冲结束后转入大陆边缘伸展作用的标志。福建沿海厦门-石狮-晋江地区的伸展作用发生在87~96Ma,与华南区域上多期伸展作用中~90Ma的伸展作用吻合。
The Cretaceous magmatism have been widely taken place in South China,and have created large scale distribution of granitoids and intruded mafic,intermediate and acid dikes,in which the mafic dikes are representative or response to the Cretaceous crustal extension tectonic activity in South China. This paper carried out the research of zircon U-Pb geochronology and Hf isotopes,and elemental geochemistry on the samples collected from the localities of Shishi and Dongfu from Shishi area,coastal Fujian Province.The granite and granodiorite are mediate- to high-K potassic calc-alkaline,and peraluminous,with U-Pb ages of 105. 3 ± 1. 0Ma and105. 1 ± 0. 5Ma. Their zircon εHf( t) range from- 0. 9 to + 2. 0. The dikes are diabase and diorites,showing metaluminous,mediateto high-K potassic calc-alkaline features. Two diorites yield zircon U-Pb ages of 89. 5 ± 1. 5Ma and 96. 1 ± 1. 2Ma. The εHf( t) of diorite are in the rage of + 1. 3 to + 5. 0. Both granitoids and dikes in the Shishi area show medium scale fractionation of light rare earth elements( REE) relative to heavy REE,and less Eu anomaly. The total REE of granitoids are less than that of the dikes. The rocks show significant enrichment of large ion lithosphile element( LILE) and depletion of high field stretch element( HFSE),which is the distinct characteristic of rocks from arc-related magmatism. The discrimination geochemical diagrams( Ta / Hf-Th / Hf,Zr-Zr / Y)suggest that the dikes from this study generated from the tectonic settings of continental margin rift or within plate environments. The dikes maybe intruded within the tectonic transition from continental subduction-related tectonic to continental extension settings,which is the index for the extension. The extension should have occurred during 87 ~ 96 Ma in the coastal Fujian Province,including Xiamen,Shishi,and Jinjiang areas,which is consistent to the regional ~ 90 Ma extension,in the multi-stage extension in the Cretaceous evolution in the whole South China.
The Cretaceous magmatism have been widely taken place in South China,and have created large scale distribution of granitoids and intruded mafic,intermediate and acid dikes,in which the mafic dikes are representative or response to the Cretaceous crustal extension tectonic activity in South China. This paper carried out the research of zircon U-Pb geochronology and Hf isotopes,and elemental geochemistry on the samples collected from the localities of Shishi and Dongfu from Shishi area,coastal Fujian Province.The granite and granodiorite are mediate- to high-K potassic calc-alkaline,and peraluminous,with U-Pb ages of 105. 3 ± 1. 0Ma and105. 1 ± 0. 5Ma. Their zircon εHf( t) range from- 0. 9 to + 2. 0. The dikes are diabase and diorites,showing metaluminous,mediateto high-K potassic calc-alkaline features. Two diorites yield zircon U-Pb ages of 89. 5 ± 1. 5Ma and 96. 1 ± 1. 2Ma. The εHf( t) of diorite are in the rage of + 1. 3 to + 5. 0. Both granitoids and dikes in the Shishi area show medium scale fractionation of light rare earth elements( REE) relative to heavy REE,and less Eu anomaly. The total REE of granitoids are less than that of the dikes. The rocks show significant enrichment of large ion lithosphile element( LILE) and depletion of high field stretch element( HFSE),which is the distinct characteristic of rocks from arc-related magmatism. The discrimination geochemical diagrams( Ta / Hf-Th / Hf,Zr-Zr / Y)suggest that the dikes from this study generated from the tectonic settings of continental margin rift or within plate environments. The dikes maybe intruded within the tectonic transition from continental subduction-related tectonic to continental extension settings,which is the index for the extension. The extension should have occurred during 87 ~ 96 Ma in the coastal Fujian Province,including Xiamen,Shishi,and Jinjiang areas,which is consistent to the regional ~ 90 Ma extension,in the multi-stage extension in the Cretaceous evolution in the whole South China.
引文
Acocella V.2014.Structural control on magmatism along divergent andconvergent plate boundaries:Overview,model,problems.EarthScience Reviews,136:226-288
Aguillón-Robles A,Tristán-González M,Aguirre-Díaz GDJ,LópezDoncel RA,Bellon H and Martínez-Esparza G.2014.Eocene toQuaternary mafic-intermediate volcanism in San Luis Potosí,centralMexico:The transition from Farallon plate subduction to intra-platecontinental magmatism.Journal of Volcanology and GeothermalResearch,276:152-172
Boynton WV.1984.Geochemistry of the rare earth elements:Meteoritestudies.In:Henderson P(ed.).Rare Earth ElementGeochemistry.Amsterdam:Elsevier,63-114
Chen NH,Dong JJ,Chen JY,Dong CW and Shen ZY.2014.Geometryand emplacement of the Late Cretaceous mafic dyke swarms on theislands in Zhejiang Province,Southeast China:Insights from highresolution satellite images.Journal of Asian Earth Sciences,79A:302-311
Chen R and Zhou JC.2001.Mineral chemistry and40Ar-39Ar ages ofhornblende gabbro from Tong’an,Fujian Province and theirgeological significance.Geological Review,47(6):602-607(inChinese with English Abstract)
Dai BZ,Jiang SY,Jiang YH,Zhao KD and Liu DY.2008.Geochronology,geochemistry and Hf-Sr-Nd isotopic compositions ofHuziyan mafic xenoliths,southern Hunan Province,South China:Petrogenesis and implications for lower crust evolution.Lithos,102(1-2):65-87
Dong CW,Li WH,Chen XM,Xu XS and Zhou XM.1998.LateMesozoic magma mixing in SE-Fujian:Petrologic evidence from thePingtan igneous complex.Progress in Natural Science,8(2):196-201
Dong CW,Zhang DR,Xu XS,Yan Q and Zhu GQ.2006.SHRIMP UPb dating and lithogeochemistry of basic-intermediate dike swarmsfrom Jinjiang,Fujian Province.Acta Petrologica Sinica,22(6):1696-1702(in Chinese with English Abstract)
Dong CW,Yan Q,Zhang DR,Du ZY and Zhu GQ.2010.LateMesozoic extension in the coastal area of Zhejiang and Fujianprovinces:A petrologic indicator from the Dongji Island mafic dikeswarms.Acta Petrologica Sinica,26(4):1195-1203(in Chinesewith English abstract)
Dong CW,Zhou C,Gu HY,Ma XX and LüQ.2011.The agedifference,geochemistry and petrogenesis of mafic dikes and hostgranites form Meizhou Island in Fujian Province.Journal of JilinUniversity(Earth Science Edition),41(3):735-744(in Chinesewith English abstract)
Ge XY,Li XH and Zhou HW.2003.Geochronologic,geochemistry andSr-Nd isotopes of the Late Cretaceous mafic dike swarms in southernHainan Island.Geochimica,32(1):11-20(in Chinese withEnglish abstract)
Griffin WL,Pearson NJ,Belousova E,Jackson SE,van Achterbergh E,O’Reilly SY and Shee SR.2000.The Hf isotope composition ofcratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts inkimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Guo F,Fan WM,Li CW,Zhao L,Li HX and Yang JH.2012.Multistage crust-mantle interaction in SE China:Temporal,thermal andcompositional constraints from the Mesozoic felsic volcanic rocks ineastern Guangdong-Fujian provinces.Lithos,150:62-84
Hoskin PWO and Schaltegger U.2003.The composition of zircon andigneous and metamorphic petrogenesis.Reviews in Mineralogy andGeochemistry,53(1):27-62
Hu RZ,Bi XW,Peng JT,Liu S,Zhong H,Zhao JH and Jiang GH.2007.Some problems concerning relationship between MesozoicCenozoic lithospheric extension and uranium matallogenesis in SouthChina.Mineral Deposits,26(2):139-152(in Chinese withEnglish abstract)
Hua RM.2005.Differences between rock-forming and related ore-formingtimes for the Mesozoic granitoids of crust remelting types in theNanling range,South China,and its geological significance.Geological Review,51(6):633-639(in Chinese with Englishabstract)
Jia DC,Hu RZ and Xie GQ.2002.Trace element geochemicalcharacteristics and genesis of Mesozoic mafic dikes in NortheastHunan Province.Geology-Geochemistry,30(3):33-39(inChinese with English abstract)
Li HM,Dong CW,Xu XS and Zhou XM.1995.Single zircon U-Pbdating of Quanzhou gabbro:Origin of magma in the southeast ofFujian Province.Chinese Science Bulletin,40(2):158-160(inChinese)
Li XH,Hu RZ and Rao B.1997.Geochronology and geochemistry ofCretaceous mafic dikes from northern Guangdong,SE China.Geochimica,26(2):14-31(in Chinese with English Abstract)
Li XH.2000.Cretaceous magmatism and lithospheric extension inSoutheast China.Journal of Asian Earth Sciences,18(3):293-305
Liu YS,Hu ZC,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrousminerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.2010.Continental and oceanic crust recycling-induced melt-peridotiteinteractions in the Trans-North China orogen:U-Pb dating,Hfisotopes and trace elements in zircons from mantle xenoliths.Journalof Petrology,51(1-2):537-571
Mao JW,Xie GQ,Guo CL,Yuan HD,Cheng YB and Chen YC.2008.Spatial-temporal distribution of Mesozoic ore deposits in South Chinaand their metallogenic settings.Geological Journal of ChinaUniversities,14(4):510-526(in Chinese with English abstract)
Pearce JA and Norry MJ.1979.Petrogenetic implications of Ti,Zr,Y,and Nb Variations in volcanic rocks.Contributions to Mineralogy andPetrology,69(1):33-37
Peccerillo A and Taylor SR.1976.Geochemistry of Eocene calc-alkalinevolcanic rocks from Kastamonu area,Northern Turkey.Contributionto Mineralogy and Petrology,58(1):63-81
Qin SC,Fan WM,Guo F,Li CW and Gao XF.2010.Petrogenesis ofLate Mesozoic diabase dikes in Zhejiang-Fujian provinces:Constraints from Ar-Ar dating and geochemistry.Acta PetrologicaSinica,26(11):3295-3306(in Chinese with English abstract)
Qiu JS,Xiao E,Hu J,Xu XS,Jiang SY and Li Z.2008.Petrogenesis ofhighly fractionated I-type granites in the coastal area of northeasternFujian Province:Constraints from zircon U-Pb geochronology,geochemistry and Nd-Hf iotopes.Acta Petrologica Sinica,24(11):2468-2484(in Chinese with English abstract)
Qiu JS,Li Z,Liu L and Zhao JL.2012.Petrogeniesis of the Zhangpucomposite granite pluton in Fujian Province:Constraints from zirconU-Pb ages,elemental geochemistry and Nd-Hf isotopes.ActaGeologica Sinica,86(4):561-576(in Chinese with Englishabstract)
Sheng D.2012.Chronology and geochemistry of intermediate dikes,hostgranitoids and enclaves in the Xiamen-Zhangzhou area.MasterDegree Thesis.Beijing:China University of Geosciences(inChinese with English summary)
Shu LS.2006.Predevonian tectonic evolution of South China:FromCathaysian block to Caledonian Period folded orogenic belt.Geological Journal of China Universities,12(4):418-431(inChinese with English abstract)
Shu LS,Zhou XM,Deng P and Yu XQ.2006.Principal geologicalfeatures of Nanling tectonic belt,South China.Geological Review,52(2):251-265(in Chinese with English abstract)
Soderlund U,Patchett PJ,Vervoort JD and Isachen CE.2004.The176Ludecay constant determined by Lu-Hf and U-Pb isotope systematics ofPrecambrian mafic intrusions.Earth and Planetary Science Letters,219(3-4):311-324
Sun SS and McD onough WF.1989.Chemical and isotopic systematics ofoceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the OceanBasins.Geological Society,London,Special Publication,42(1):313-345
Sun T and Zhou XM.2002.Late Mesozoic extension in SoutheasternChina:Petrologic symbols.Journal of Nanjing University(NaturalScience),38(6):737-746(in Chinese with English abstract)
Sun T.2006.A new map showing the distribution of granites in SouthChina and its explanatory notes.Geological Bulletin of China,25(3):332-335(in Chinese with English abstract)
Tang LM,Chen HL,Dong CW,Shen ZY,Cheng XG and Fu LL.2010.Late Mesozoic tectonic extension in SE China:Evidence from thebasic dike swarms in Hainan Island,China.Acta Petrologica Sinica,26(4):1204-1216(in Chinese with English abstract)
Wang DZ.2004.The study of granitic rocks in South China:Lookingback and forward.Geological Journal of China Universities,10(3):306-314(in Chinese with English abstract)
Wang DZ and Zhou JC.2005.New progress in studying the large igneousprovinces.Geological Journal of China Universities,11(1):1-8(in Chinese with English abstract)
Wang FY,Ling MX,Ding X,Hu YH,Zhou JB,Yang XY,Liang HY,Fan WM and Sun WD.2011.Mesozoic large magmatic events andmineralization in SE China:Oblique subduction of the pacific plate.International Geology Review,53(5-6):704-726
Wang Q,Zhao ZH,Jian P,Xiong XL,Bao ZW,Dai TM,Xu JF and MaJL.2005.Geochronology of Cretaceous A-type granitoids or alkalineintrusive rocks in the hinterland,South China:Constraints for lateMesozoic tectonic evolution.Acta Petrologica Sinica,21(3):795-808(in Chinese with English Abstract)
Wang T.2000.Origin of hybrid granitoids and implications forcontinental dynamics.Acta Petrologica Sinica,16(2):161-168(in Chinese with English abstract)
Wang YL,Zhang CJ and Xiu SZ.2001.Th/Hf-Ta/Hf identification oftectonic setting of basalts.Acta Petrologica Sinica,17(3):413-421(in Chinese with English abstract)
Wilson M.2001.Igneous Petrogenesis.London:KluwerAcademic Publishers
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on thepetrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Xie GQ,Hu RZ and Jia DC.2002.Geological and geochemicalcharacteristics and its significance of mafic dikes from NorthwestJiangxi Province.Geochimica,31(4):329-337(in Chinese withEnglish abstract)
Xu XS,Zhou XM and Wang DZ.1999.Crust-mantle interaction andgenesis of granite:A case study of coastal area of southeasternChina.Geological Journal of China Universities,5(3):241-250(in Chinese with English abstract)
Xu XS and Xie X.2005.Late Mesozoic-Cenozoic basaltic rock and crustmantle interaction,SE China.Geological Journal of ChinaUniversities,11(3):318-334(in Chinese with English abstract)
Xu XS.2008.Several problems worthy to be noticed in the research ofgranites and volcanic rocks in SE China.Geological Journal of ChinaUniversities,14(3):283-294(in Chinese with English abstract)
Xu XS and He ZY.2012.Progress in granite studies.Bulletin ofMineralogy,Petrology and Geochemistry,31(3):205-209(inChinese with English abstract)
Yang JB.2012.Petrology,geochemistry,and petrogenesis of Mesozoicgranites of Quanzhou in the southeast coast,Fujian Province.MasterDegree Thesis.Beijing:China University of Geosciences(inChinese with English summary)
Yang JB,Sheng D,Zhao ZD,Ding C,Zhou HF,Cui YY,Jiang T andHu ZC.2013.Petrogenesis and implications of granites andassociated dioritic enclaves in Jiaomei area,Zhangzhou,FujianProvince.Acta Petrologica Sinica,29(11):4004-4010(inChinese with English abstract)
Yang YF,Dong CW,Yan Q,Li NM,Zhu GQ and Song YQ.2010a.Late Mesozoic extension in the coastal area of Zhejiang and Fujianprovinces:An indicator form the basic-intermediate dikes,coastlandof Fujian Province.Journal of Mineralogy and Petrology,30(2):87-94(in Chinese with English abstract)
Yang YF,Yang JJ,Li NM,Yan Q,Zhan X and Dong CW.2010b.SHRIMP U-Pb zircon dating of the basic-Intermediate dikes from thecoastland of Fujian Province.Geological Science and TechnologyInformation,29(5):23-29(in Chinese with English Abstract)
Zhang GS,Wen HJ,Hu RZ,Qiu YZ and Xu C.2007.Genesis anddynamic setting of mafic dikes in southeastern Fujian:Evidence fromSr-Nd isotopic and major and trace element geochemistry.ActaPetrologica Sinica,23(4):794-803(in Chinese with Englishabstract)
Zhao JH.2004.Chronology and geochemistry of mafic rocks from FujianProvince:Implications for the mantle evolution of SE China sinceLate Mesozoic.Ph.D.Dissertation.Beijing:Graduate School ofChinese Academy of Sciences(in Chinese with English summary)
Zhou XM and Li WX.2000.Origin of Late Mesozoic igneous rocks inSoutheastern China:Implications for lithosphere subduction andunderplating of mafic magmas.Tectonophysics,326(3-4):269-287
Zhou XM.2003.My thinking about granite genesis of South China.Geological Journal of China Universities,9(4):556-565(inChinese with English abstract)
Zhou XM,Sun T,Shen WZ,Shu LS and Niu YL.2006.Petrogenesis ofMesozoic granitoids and volcanic rocks in South China:A response totectonic evolution.Episodes,29(1):26-32
陈荣,周金城.2001.福建同安角闪辉长岩的矿物化学、40Ar-39Ar年龄及地质意义.地质论评,47(6):602-607
董传万,张登荣,徐夕生,闫强,竺国强.2006.福建晋江中-基性岩墙群的锆石SHRIMP U-Pb定年和岩石地球化学.岩石学报,22(6):1696-1702
董传万,闫强,张登荣,杜振永,竺国强.2010.浙闽沿海晚中生代伸展构造的岩石学标志:东极岛镁铁质岩墙群.岩石学报,26(4):1195-1203
董传万,周超,顾红艳,马骁雄,吕青.2011.福建湄洲岛镁铁质岩墙群与寄主花岗岩的形成时差、地球化学及成因.吉林大学学报,41(3):735-744
葛小月,李献华,周汉文.2003.琼南晚白垩世基性岩墙群的年代学、元素地球化学和Sr-Nd同位素研究.地球化学,32(1):11-20
胡瑞忠,毕献武,彭建堂,刘燊,钟宏,赵军红,蒋国豪.2007.华南地区中生代以来岩石圈伸展及其与铀成矿关系研究的若干问题.矿床地质,26(2):139-152
华仁民.2005.南岭中生代陆壳重熔型花岗岩类成岩-成矿的时间差及其地质意义.地质评论,51(6):633-639
贾大成,胡瑞忠,谢桂青.2002.湘东北中生代基性岩脉微量元素地球化学特征及岩石成因.地质地球化学,30(3):33-39
李惠民,董传万,徐夕生,周新民.1995.泉州辉长岩中单粒锆石UPb法定年:闽东南基性岩浆岩的起源.科学通报,40(2):158-160
李献华,胡瑞中,饶冰.1997.粤北白垩纪基性岩脉的年代学和地球化学.地球化学,26(2):14-31
毛景文,谢桂青,郭春丽,袁顺达,程彦博,陈毓川.2008.华南地区中生代主要金属矿床时空分布规律和成矿环境.高校地质学报,14(4):510-526
秦社彩,范蔚茗,郭锋,李超文,高晓峰.2010.浙闽晚中生代辉绿岩脉的岩石成因:年代学与地球化学制约.岩石学报,26(11):3295-3306
邱检生,肖娥,胡建,徐夕生,蒋少涌,李真.2008.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NdHf同位素制约.岩石学报,24(11):2468-2484
邱检生,李振,刘亮,赵娇龙.2012.福建漳浦复式花岗岩体的成因:锆石U-Pb年代学、元素地球化学及Nd-Hf同位素制约.地质学报,86(4):561-576
盛丹.2012.厦门-漳州地区白垩纪中基性岩脉群、花岗岩类及其包体的年代学和地球化学.硕士学位论文.北京:中国地质大学
舒良树.2006.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,12(4):418-431
舒良树,周新民,邓平,余心起.2006.南岭构造带的基本地质特征.地质评论,52(2):251-265
孙涛,周新民.2002.中国东南部晚中生代伸展应力体制的岩石学标志.南京大学学报(自然科学版),38(6):737-746
孙涛.2006.新编华南花岗岩分布图及其说明.地质通报,25(3):332-335
唐立梅,陈汉林,董传万,沈忠悦,程晓敢,付璐露.2010.中国东南部晚中生代构造伸展作用———来自海南岛基性岩墙群的证据.岩石学报,26(4):1204-1216
王德滋.2004.华南花岗岩研究的回顾与展望.高校地质学报,10(3):305-314
王德滋,周金城.2005.大火成岩省研究新进展.高校地质学报,11(1):1-8
王强,赵振华,简平,熊小林,包志伟,戴橦谟,许继峰,马金龙.2005.华南腹地白垩纪A型花岗岩类或碱性侵入岩年代学及其对华南晚中生代构造演化的制约.岩石学报,21(3):795-808
王涛.2000.花岗岩混合成因研究及大陆动力学意义.岩石学报,16(2):161-168
汪云亮,张成江,修淑芝.2001.玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别.岩石学报,17(3):413-421
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
谢桂青,胡瑞忠,贾大成.2002.赣西北基性岩脉的地质地球化学特征及其意义.地球化学,31(4):329-337
徐夕生,周新民,王德滋.1999.壳幔作用与花岗岩成因———以中国东南沿海为例.高校地质学报,5(3):241-250
徐夕生,谢昕.2005.中国东南部晚中生代-新生代玄武岩与壳幔作用.高校地质学报,11(3):318-334
徐夕生.2008.华南花岗岩-火山岩成因研究的几个问题.高校地质学报,14(3):283-294
徐夕生,贺振宇.2012.花岗岩研究进展.矿物岩石地球化学通报,31(3):205-209
杨金豹.2012.福建东南沿海泉州地区中生代花岗岩的岩石学、地球化学和岩石成因.硕士学位论文.北京:中国地质大学
杨金豹,盛丹,赵志丹,丁聪,周红芳,崔圆圆,蒋婷,胡兆初.2013.福建漳州角美花岗岩与闪长质包体的岩石成因及意义.岩石学报,29(11):4004-4010
杨永峰,董传万,闫强,李南美,竺国强,宋元青.2010a.浙闽沿海晚中生代伸展构造作用:来自福建沿海中-基性岩墙群的证据.矿物岩石,30(2):87-94
杨永峰,杨俊杰,李南美,闫强,占玄,董传万.2010b.福建沿海中-基性岩墙群锆石SHRIMP U-Pb定年.地质科技情报,29(5):23-29
张贵山,温汉捷,胡瑞忠,裘愉卓,许成.2007.闽东南基性岩脉成因及动力学背景研究:Sr-Nd同位素、元素地球化学.岩石学报,23(4):794-803
赵军红.2004.福建省基性岩的年代学和地球化学:晚中生代以来中国东南部地幔演化.博士学位论文.北京:中国科学院研究生院
周新民.2003.对华南花岗岩研究的若干思考.高校地质学报,9(4):556-565
1福建省地质测量队.1972.1∶20万泉州幅地质图
Aguillón-Robles A,Tristán-González M,Aguirre-Díaz GDJ,LópezDoncel RA,Bellon H and Martínez-Esparza G.2014.Eocene toQuaternary mafic-intermediate volcanism in San Luis Potosí,centralMexico:The transition from Farallon plate subduction to intra-platecontinental magmatism.Journal of Volcanology and GeothermalResearch,276:152-172
Boynton WV.1984.Geochemistry of the rare earth elements:Meteoritestudies.In:Henderson P(ed.).Rare Earth ElementGeochemistry.Amsterdam:Elsevier,63-114
Chen NH,Dong JJ,Chen JY,Dong CW and Shen ZY.2014.Geometryand emplacement of the Late Cretaceous mafic dyke swarms on theislands in Zhejiang Province,Southeast China:Insights from highresolution satellite images.Journal of Asian Earth Sciences,79A:302-311
Chen R and Zhou JC.2001.Mineral chemistry and40Ar-39Ar ages ofhornblende gabbro from Tong’an,Fujian Province and theirgeological significance.Geological Review,47(6):602-607(inChinese with English Abstract)
Dai BZ,Jiang SY,Jiang YH,Zhao KD and Liu DY.2008.Geochronology,geochemistry and Hf-Sr-Nd isotopic compositions ofHuziyan mafic xenoliths,southern Hunan Province,South China:Petrogenesis and implications for lower crust evolution.Lithos,102(1-2):65-87
Dong CW,Li WH,Chen XM,Xu XS and Zhou XM.1998.LateMesozoic magma mixing in SE-Fujian:Petrologic evidence from thePingtan igneous complex.Progress in Natural Science,8(2):196-201
Dong CW,Zhang DR,Xu XS,Yan Q and Zhu GQ.2006.SHRIMP UPb dating and lithogeochemistry of basic-intermediate dike swarmsfrom Jinjiang,Fujian Province.Acta Petrologica Sinica,22(6):1696-1702(in Chinese with English Abstract)
Dong CW,Yan Q,Zhang DR,Du ZY and Zhu GQ.2010.LateMesozoic extension in the coastal area of Zhejiang and Fujianprovinces:A petrologic indicator from the Dongji Island mafic dikeswarms.Acta Petrologica Sinica,26(4):1195-1203(in Chinesewith English abstract)
Dong CW,Zhou C,Gu HY,Ma XX and LüQ.2011.The agedifference,geochemistry and petrogenesis of mafic dikes and hostgranites form Meizhou Island in Fujian Province.Journal of JilinUniversity(Earth Science Edition),41(3):735-744(in Chinesewith English abstract)
Ge XY,Li XH and Zhou HW.2003.Geochronologic,geochemistry andSr-Nd isotopes of the Late Cretaceous mafic dike swarms in southernHainan Island.Geochimica,32(1):11-20(in Chinese withEnglish abstract)
Griffin WL,Pearson NJ,Belousova E,Jackson SE,van Achterbergh E,O’Reilly SY and Shee SR.2000.The Hf isotope composition ofcratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts inkimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Guo F,Fan WM,Li CW,Zhao L,Li HX and Yang JH.2012.Multistage crust-mantle interaction in SE China:Temporal,thermal andcompositional constraints from the Mesozoic felsic volcanic rocks ineastern Guangdong-Fujian provinces.Lithos,150:62-84
Hoskin PWO and Schaltegger U.2003.The composition of zircon andigneous and metamorphic petrogenesis.Reviews in Mineralogy andGeochemistry,53(1):27-62
Hu RZ,Bi XW,Peng JT,Liu S,Zhong H,Zhao JH and Jiang GH.2007.Some problems concerning relationship between MesozoicCenozoic lithospheric extension and uranium matallogenesis in SouthChina.Mineral Deposits,26(2):139-152(in Chinese withEnglish abstract)
Hua RM.2005.Differences between rock-forming and related ore-formingtimes for the Mesozoic granitoids of crust remelting types in theNanling range,South China,and its geological significance.Geological Review,51(6):633-639(in Chinese with Englishabstract)
Jia DC,Hu RZ and Xie GQ.2002.Trace element geochemicalcharacteristics and genesis of Mesozoic mafic dikes in NortheastHunan Province.Geology-Geochemistry,30(3):33-39(inChinese with English abstract)
Li HM,Dong CW,Xu XS and Zhou XM.1995.Single zircon U-Pbdating of Quanzhou gabbro:Origin of magma in the southeast ofFujian Province.Chinese Science Bulletin,40(2):158-160(inChinese)
Li XH,Hu RZ and Rao B.1997.Geochronology and geochemistry ofCretaceous mafic dikes from northern Guangdong,SE China.Geochimica,26(2):14-31(in Chinese with English Abstract)
Li XH.2000.Cretaceous magmatism and lithospheric extension inSoutheast China.Journal of Asian Earth Sciences,18(3):293-305
Liu YS,Hu ZC,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrousminerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Liu YS,Gao S,Hu ZC,Gao CG,Zong KQ and Wang DB.2010.Continental and oceanic crust recycling-induced melt-peridotiteinteractions in the Trans-North China orogen:U-Pb dating,Hfisotopes and trace elements in zircons from mantle xenoliths.Journalof Petrology,51(1-2):537-571
Mao JW,Xie GQ,Guo CL,Yuan HD,Cheng YB and Chen YC.2008.Spatial-temporal distribution of Mesozoic ore deposits in South Chinaand their metallogenic settings.Geological Journal of ChinaUniversities,14(4):510-526(in Chinese with English abstract)
Pearce JA and Norry MJ.1979.Petrogenetic implications of Ti,Zr,Y,and Nb Variations in volcanic rocks.Contributions to Mineralogy andPetrology,69(1):33-37
Peccerillo A and Taylor SR.1976.Geochemistry of Eocene calc-alkalinevolcanic rocks from Kastamonu area,Northern Turkey.Contributionto Mineralogy and Petrology,58(1):63-81
Qin SC,Fan WM,Guo F,Li CW and Gao XF.2010.Petrogenesis ofLate Mesozoic diabase dikes in Zhejiang-Fujian provinces:Constraints from Ar-Ar dating and geochemistry.Acta PetrologicaSinica,26(11):3295-3306(in Chinese with English abstract)
Qiu JS,Xiao E,Hu J,Xu XS,Jiang SY and Li Z.2008.Petrogenesis ofhighly fractionated I-type granites in the coastal area of northeasternFujian Province:Constraints from zircon U-Pb geochronology,geochemistry and Nd-Hf iotopes.Acta Petrologica Sinica,24(11):2468-2484(in Chinese with English abstract)
Qiu JS,Li Z,Liu L and Zhao JL.2012.Petrogeniesis of the Zhangpucomposite granite pluton in Fujian Province:Constraints from zirconU-Pb ages,elemental geochemistry and Nd-Hf isotopes.ActaGeologica Sinica,86(4):561-576(in Chinese with Englishabstract)
Sheng D.2012.Chronology and geochemistry of intermediate dikes,hostgranitoids and enclaves in the Xiamen-Zhangzhou area.MasterDegree Thesis.Beijing:China University of Geosciences(inChinese with English summary)
Shu LS.2006.Predevonian tectonic evolution of South China:FromCathaysian block to Caledonian Period folded orogenic belt.Geological Journal of China Universities,12(4):418-431(inChinese with English abstract)
Shu LS,Zhou XM,Deng P and Yu XQ.2006.Principal geologicalfeatures of Nanling tectonic belt,South China.Geological Review,52(2):251-265(in Chinese with English abstract)
Soderlund U,Patchett PJ,Vervoort JD and Isachen CE.2004.The176Ludecay constant determined by Lu-Hf and U-Pb isotope systematics ofPrecambrian mafic intrusions.Earth and Planetary Science Letters,219(3-4):311-324
Sun SS and McD onough WF.1989.Chemical and isotopic systematics ofoceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the OceanBasins.Geological Society,London,Special Publication,42(1):313-345
Sun T and Zhou XM.2002.Late Mesozoic extension in SoutheasternChina:Petrologic symbols.Journal of Nanjing University(NaturalScience),38(6):737-746(in Chinese with English abstract)
Sun T.2006.A new map showing the distribution of granites in SouthChina and its explanatory notes.Geological Bulletin of China,25(3):332-335(in Chinese with English abstract)
Tang LM,Chen HL,Dong CW,Shen ZY,Cheng XG and Fu LL.2010.Late Mesozoic tectonic extension in SE China:Evidence from thebasic dike swarms in Hainan Island,China.Acta Petrologica Sinica,26(4):1204-1216(in Chinese with English abstract)
Wang DZ.2004.The study of granitic rocks in South China:Lookingback and forward.Geological Journal of China Universities,10(3):306-314(in Chinese with English abstract)
Wang DZ and Zhou JC.2005.New progress in studying the large igneousprovinces.Geological Journal of China Universities,11(1):1-8(in Chinese with English abstract)
Wang FY,Ling MX,Ding X,Hu YH,Zhou JB,Yang XY,Liang HY,Fan WM and Sun WD.2011.Mesozoic large magmatic events andmineralization in SE China:Oblique subduction of the pacific plate.International Geology Review,53(5-6):704-726
Wang Q,Zhao ZH,Jian P,Xiong XL,Bao ZW,Dai TM,Xu JF and MaJL.2005.Geochronology of Cretaceous A-type granitoids or alkalineintrusive rocks in the hinterland,South China:Constraints for lateMesozoic tectonic evolution.Acta Petrologica Sinica,21(3):795-808(in Chinese with English Abstract)
Wang T.2000.Origin of hybrid granitoids and implications forcontinental dynamics.Acta Petrologica Sinica,16(2):161-168(in Chinese with English abstract)
Wang YL,Zhang CJ and Xiu SZ.2001.Th/Hf-Ta/Hf identification oftectonic setting of basalts.Acta Petrologica Sinica,17(3):413-421(in Chinese with English abstract)
Wilson M.2001.Igneous Petrogenesis.London:KluwerAcademic Publishers
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on thepetrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Xie GQ,Hu RZ and Jia DC.2002.Geological and geochemicalcharacteristics and its significance of mafic dikes from NorthwestJiangxi Province.Geochimica,31(4):329-337(in Chinese withEnglish abstract)
Xu XS,Zhou XM and Wang DZ.1999.Crust-mantle interaction andgenesis of granite:A case study of coastal area of southeasternChina.Geological Journal of China Universities,5(3):241-250(in Chinese with English abstract)
Xu XS and Xie X.2005.Late Mesozoic-Cenozoic basaltic rock and crustmantle interaction,SE China.Geological Journal of ChinaUniversities,11(3):318-334(in Chinese with English abstract)
Xu XS.2008.Several problems worthy to be noticed in the research ofgranites and volcanic rocks in SE China.Geological Journal of ChinaUniversities,14(3):283-294(in Chinese with English abstract)
Xu XS and He ZY.2012.Progress in granite studies.Bulletin ofMineralogy,Petrology and Geochemistry,31(3):205-209(inChinese with English abstract)
Yang JB.2012.Petrology,geochemistry,and petrogenesis of Mesozoicgranites of Quanzhou in the southeast coast,Fujian Province.MasterDegree Thesis.Beijing:China University of Geosciences(inChinese with English summary)
Yang JB,Sheng D,Zhao ZD,Ding C,Zhou HF,Cui YY,Jiang T andHu ZC.2013.Petrogenesis and implications of granites andassociated dioritic enclaves in Jiaomei area,Zhangzhou,FujianProvince.Acta Petrologica Sinica,29(11):4004-4010(inChinese with English abstract)
Yang YF,Dong CW,Yan Q,Li NM,Zhu GQ and Song YQ.2010a.Late Mesozoic extension in the coastal area of Zhejiang and Fujianprovinces:An indicator form the basic-intermediate dikes,coastlandof Fujian Province.Journal of Mineralogy and Petrology,30(2):87-94(in Chinese with English abstract)
Yang YF,Yang JJ,Li NM,Yan Q,Zhan X and Dong CW.2010b.SHRIMP U-Pb zircon dating of the basic-Intermediate dikes from thecoastland of Fujian Province.Geological Science and TechnologyInformation,29(5):23-29(in Chinese with English Abstract)
Zhang GS,Wen HJ,Hu RZ,Qiu YZ and Xu C.2007.Genesis anddynamic setting of mafic dikes in southeastern Fujian:Evidence fromSr-Nd isotopic and major and trace element geochemistry.ActaPetrologica Sinica,23(4):794-803(in Chinese with Englishabstract)
Zhao JH.2004.Chronology and geochemistry of mafic rocks from FujianProvince:Implications for the mantle evolution of SE China sinceLate Mesozoic.Ph.D.Dissertation.Beijing:Graduate School ofChinese Academy of Sciences(in Chinese with English summary)
Zhou XM and Li WX.2000.Origin of Late Mesozoic igneous rocks inSoutheastern China:Implications for lithosphere subduction andunderplating of mafic magmas.Tectonophysics,326(3-4):269-287
Zhou XM.2003.My thinking about granite genesis of South China.Geological Journal of China Universities,9(4):556-565(inChinese with English abstract)
Zhou XM,Sun T,Shen WZ,Shu LS and Niu YL.2006.Petrogenesis ofMesozoic granitoids and volcanic rocks in South China:A response totectonic evolution.Episodes,29(1):26-32
陈荣,周金城.2001.福建同安角闪辉长岩的矿物化学、40Ar-39Ar年龄及地质意义.地质论评,47(6):602-607
董传万,张登荣,徐夕生,闫强,竺国强.2006.福建晋江中-基性岩墙群的锆石SHRIMP U-Pb定年和岩石地球化学.岩石学报,22(6):1696-1702
董传万,闫强,张登荣,杜振永,竺国强.2010.浙闽沿海晚中生代伸展构造的岩石学标志:东极岛镁铁质岩墙群.岩石学报,26(4):1195-1203
董传万,周超,顾红艳,马骁雄,吕青.2011.福建湄洲岛镁铁质岩墙群与寄主花岗岩的形成时差、地球化学及成因.吉林大学学报,41(3):735-744
葛小月,李献华,周汉文.2003.琼南晚白垩世基性岩墙群的年代学、元素地球化学和Sr-Nd同位素研究.地球化学,32(1):11-20
胡瑞忠,毕献武,彭建堂,刘燊,钟宏,赵军红,蒋国豪.2007.华南地区中生代以来岩石圈伸展及其与铀成矿关系研究的若干问题.矿床地质,26(2):139-152
华仁民.2005.南岭中生代陆壳重熔型花岗岩类成岩-成矿的时间差及其地质意义.地质评论,51(6):633-639
贾大成,胡瑞忠,谢桂青.2002.湘东北中生代基性岩脉微量元素地球化学特征及岩石成因.地质地球化学,30(3):33-39
李惠民,董传万,徐夕生,周新民.1995.泉州辉长岩中单粒锆石UPb法定年:闽东南基性岩浆岩的起源.科学通报,40(2):158-160
李献华,胡瑞中,饶冰.1997.粤北白垩纪基性岩脉的年代学和地球化学.地球化学,26(2):14-31
毛景文,谢桂青,郭春丽,袁顺达,程彦博,陈毓川.2008.华南地区中生代主要金属矿床时空分布规律和成矿环境.高校地质学报,14(4):510-526
秦社彩,范蔚茗,郭锋,李超文,高晓峰.2010.浙闽晚中生代辉绿岩脉的岩石成因:年代学与地球化学制约.岩石学报,26(11):3295-3306
邱检生,肖娥,胡建,徐夕生,蒋少涌,李真.2008.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NdHf同位素制约.岩石学报,24(11):2468-2484
邱检生,李振,刘亮,赵娇龙.2012.福建漳浦复式花岗岩体的成因:锆石U-Pb年代学、元素地球化学及Nd-Hf同位素制约.地质学报,86(4):561-576
盛丹.2012.厦门-漳州地区白垩纪中基性岩脉群、花岗岩类及其包体的年代学和地球化学.硕士学位论文.北京:中国地质大学
舒良树.2006.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,12(4):418-431
舒良树,周新民,邓平,余心起.2006.南岭构造带的基本地质特征.地质评论,52(2):251-265
孙涛,周新民.2002.中国东南部晚中生代伸展应力体制的岩石学标志.南京大学学报(自然科学版),38(6):737-746
孙涛.2006.新编华南花岗岩分布图及其说明.地质通报,25(3):332-335
唐立梅,陈汉林,董传万,沈忠悦,程晓敢,付璐露.2010.中国东南部晚中生代构造伸展作用———来自海南岛基性岩墙群的证据.岩石学报,26(4):1204-1216
王德滋.2004.华南花岗岩研究的回顾与展望.高校地质学报,10(3):305-314
王德滋,周金城.2005.大火成岩省研究新进展.高校地质学报,11(1):1-8
王强,赵振华,简平,熊小林,包志伟,戴橦谟,许继峰,马金龙.2005.华南腹地白垩纪A型花岗岩类或碱性侵入岩年代学及其对华南晚中生代构造演化的制约.岩石学报,21(3):795-808
王涛.2000.花岗岩混合成因研究及大陆动力学意义.岩石学报,16(2):161-168
汪云亮,张成江,修淑芝.2001.玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别.岩石学报,17(3):413-421
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
谢桂青,胡瑞忠,贾大成.2002.赣西北基性岩脉的地质地球化学特征及其意义.地球化学,31(4):329-337
徐夕生,周新民,王德滋.1999.壳幔作用与花岗岩成因———以中国东南沿海为例.高校地质学报,5(3):241-250
徐夕生,谢昕.2005.中国东南部晚中生代-新生代玄武岩与壳幔作用.高校地质学报,11(3):318-334
徐夕生.2008.华南花岗岩-火山岩成因研究的几个问题.高校地质学报,14(3):283-294
徐夕生,贺振宇.2012.花岗岩研究进展.矿物岩石地球化学通报,31(3):205-209
杨金豹.2012.福建东南沿海泉州地区中生代花岗岩的岩石学、地球化学和岩石成因.硕士学位论文.北京:中国地质大学
杨金豹,盛丹,赵志丹,丁聪,周红芳,崔圆圆,蒋婷,胡兆初.2013.福建漳州角美花岗岩与闪长质包体的岩石成因及意义.岩石学报,29(11):4004-4010
杨永峰,董传万,闫强,李南美,竺国强,宋元青.2010a.浙闽沿海晚中生代伸展构造作用:来自福建沿海中-基性岩墙群的证据.矿物岩石,30(2):87-94
杨永峰,杨俊杰,李南美,闫强,占玄,董传万.2010b.福建沿海中-基性岩墙群锆石SHRIMP U-Pb定年.地质科技情报,29(5):23-29
张贵山,温汉捷,胡瑞忠,裘愉卓,许成.2007.闽东南基性岩脉成因及动力学背景研究:Sr-Nd同位素、元素地球化学.岩石学报,23(4):794-803
赵军红.2004.福建省基性岩的年代学和地球化学:晚中生代以来中国东南部地幔演化.博士学位论文.北京:中国科学院研究生院
周新民.2003.对华南花岗岩研究的若干思考.高校地质学报,9(4):556-565
1福建省地质测量队.1972.1∶20万泉州幅地质图