江西相山酸性火山—侵入杂岩体地球化学特征与岩石成因
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摘要
相山火山盆地主体岩石为一套由熔结凝灰岩、流纹英安岩、碎斑熔岩、流纹英安斑岩、粗斑花岗斑岩及似斑状花岗岩组成的酸性火山-侵入杂岩体,具两个岩浆活动亚旋回。岩石具有富硅、富碱、低钙和低镁的特征,轻重稀土分异显著,稀土配分曲线呈四组分模式,具明显的负铕异常。各岩类之间具有相似的主、微量元素和同位素特征,指示了杂岩体各类岩石之间的同源性。流纹英安岩、碎斑熔岩、粗斑花岗斑岩及似斑状花岗岩的Nd模式年龄T_(2DM)较为接近,分别为1.67Ga、1.66Ga、1.66Ga和1.63Ga,略低于残留锆石~(206)Pb/~(238)U年龄(1787.9Ma)和华夏地块出露的最古老岩石(斜长角闪岩)内的岩浆锆石SHRIMP U-Pb年龄(1766±19Ma),SiO_2与P_2O_5呈明显的负相关关系,结合岩相学特征和Sr-Nd的二元混合模式,推算出杂岩体的物质来源主要为上地壳中元古代基底变质岩部分熔融的结果,有少量幔源的参与(平均含量为22.82%)。每期亚旋回不同岩类之间随着成岩先后顺序,Na_2O和K_2O含量逐渐增高,但SiO_2含量逐渐降低,表现出反序演化特征,可能表明岩浆房内发生过正常的分异作用,反映岩浆房内酸性成分在上偏基性成分在下的分布状况,第一亚旋回的末期或者暂歇期又有酸性岩浆的重新加入。第一亚旋回分异程度较强,以分离斜长石和钾长石为主,第二亚旋回以分离钾长石为主。燕山晚期江西境内的地球动力学背景并不是一致的,有由南向北逐渐演化为板内裂谷的趋势。相山地区在141~132Ma之间表现为陆内造山后的伸展阶段,在125Ma附近逐渐演化为板内裂谷环境。
The Xiangshan volcanic basin comprises volcano-intrusive complexes that are composed of tuff,rhyolite dacite,porphyry rhyolitic dacite,porphyroclastic lava,coarse grained porphyry and porphyritic granite.The paper discussed the origin and evolution of these igneous rocks based on their whole rock major and trace elements,as well as Pb-Sr-Nd isotopes.Different lithologies have similar elemental and isotopic compositoins,indicating that they were derived from the same source region.The rocks are rich in silicon and alkali,low in calcium and magnesium.LREE and HREE differentiate significantly,REE distribution curve presents four component model and obvious negative Eu.Nd model ages(T_(2DM))of rhyodacite,Porphyroclastic Lava,rough spots granite porphyry and porphyritic granite is closer,respectively 1.67 Ga,1.66 Ga,1.66 Ga and 1.63 Ga,slightly lower than the residual zircon ~(207)Pb/~(206)Pb age(1787.9Ma)and the the oldest rocks exposed(amphibolite)of Cathaysian Block within the magmatic zircon SHRIMP U-Pb age of(1766 ± 19Ma).There is a negative correlation between SiO_2 and P_2O_5,combining the facieology and the two element mixed mode petrography of Sr-Nd,calculating that the material source of the complexes has a small amount of mantle source involved,the average content of 22.82%.;each sub cycle between the different rock types with diagenesis sequence,Na_2O and K_2O increased,but SiO_2 content decreased gradually,may indicate that the magma has occurred in the differentiation of normal.acidic component is on the upside,and the partial distribution of basic components at the bottom,at the end of the first sub cycle or timeout period,acidic component join in the magma.The first subcycle variation degree is strong,the separation of plagioclase and potash feldspar,at the second sub cycles,mainly potassium feldspar.At the late Yanshan,Jiangxi in the dynamic background of the earth is different,gradually evolved into intra plate rift trend from south to north.In 141Ma~132Ma the Xiangshan area is post orogenicr,in the vicinity of 125 Ma gradually evolved into an intraplate rift environment.
The Xiangshan volcanic basin comprises volcano-intrusive complexes that are composed of tuff,rhyolite dacite,porphyry rhyolitic dacite,porphyroclastic lava,coarse grained porphyry and porphyritic granite.The paper discussed the origin and evolution of these igneous rocks based on their whole rock major and trace elements,as well as Pb-Sr-Nd isotopes.Different lithologies have similar elemental and isotopic compositoins,indicating that they were derived from the same source region.The rocks are rich in silicon and alkali,low in calcium and magnesium.LREE and HREE differentiate significantly,REE distribution curve presents four component model and obvious negative Eu.Nd model ages(T_(2DM))of rhyodacite,Porphyroclastic Lava,rough spots granite porphyry and porphyritic granite is closer,respectively 1.67 Ga,1.66 Ga,1.66 Ga and 1.63 Ga,slightly lower than the residual zircon ~(207)Pb/~(206)Pb age(1787.9Ma)and the the oldest rocks exposed(amphibolite)of Cathaysian Block within the magmatic zircon SHRIMP U-Pb age of(1766 ± 19Ma).There is a negative correlation between SiO_2 and P_2O_5,combining the facieology and the two element mixed mode petrography of Sr-Nd,calculating that the material source of the complexes has a small amount of mantle source involved,the average content of 22.82%.;each sub cycle between the different rock types with diagenesis sequence,Na_2O and K_2O increased,but SiO_2 content decreased gradually,may indicate that the magma has occurred in the differentiation of normal.acidic component is on the upside,and the partial distribution of basic components at the bottom,at the end of the first sub cycle or timeout period,acidic component join in the magma.The first subcycle variation degree is strong,the separation of plagioclase and potash feldspar,at the second sub cycles,mainly potassium feldspar.At the late Yanshan,Jiangxi in the dynamic background of the earth is different,gradually evolved into intra plate rift trend from south to north.In 141Ma~132Ma the Xiangshan area is post orogenicr,in the vicinity of 125 Ma gradually evolved into an intraplate rift environment.
引文
Bea F,Fershtater G,Corretge L G.1992.The geochemistry of phosphorus in granite rocks and the effect of aluminium.Lithos,29(1/2):43~56.
Chen Jiangfeng,Jahn Bor-ming.1998.Crustal evolution of southeasternChina:Nd and Sr isotopic evidence.Tectonophysics,284:101~133.
Condie K C.2001.Mantle Plume and Their Record in Earth History.London:Cambridge University Press.
Chen Xiaoming,Lu Jianjun,Liu Changshi,Zhao Lianze,Wang Dezi,Li Huimin.1999.Single-grain zircon U-Pb isotopic ages of the volcanic-intrusive complexes in Tonglu and Xiangshan areas.Acta Petrologica Sinica,15(2):272~278(in Chinese with English abstract).
Chen Weifeng,Chen Peirong,Xu Xisheng,Zhang Min.2005.Geochemical characteristics of Cretaceous basaltic rocks in South China and constraints on Pacific plate subduction.Science in China Series D Earth Sciences,48(12):2104~2117.
Doe B R,Zartman R E.1979.Plumbotectonics the Phanerozoic.Barnes H L.Geochemistry of Hydrothermalore Deposits and.Ed.Wilev Interscience.Chap2,22~70.
Dou Xiaoping.2005.REE distribution characteristics of volcanic and epimetamorphic rocks in Xiangshan volcanic basin and discussion on their genesis.Uranium Geology,21(6):338~344(in Chinese with English abstract).
Duan Yun,Zhao Lianze,Fan Honghai,Wang Dezi.2001.REE-Geochemistry of Mesozoic Volcanic-Intrusive Complex and Dark Inclusions inXiangshan District,Jiangxi Pronvince.Geological Journal of China Universities,7(1):92~98(in Chinese with English abstract).
Guo Dongfa,Wu Zhaohui,Cui Jianyong,Ou Guangxi,Fan Guang.2007.Review onur anium geoanalysis and introduction to the concept of network analytical labor ator ies.World Nuclear Geoscience,24(1):50~63(in Chinese with English abstract).
Guo Fusheng,Yang Qingkun,Xie Caifu,Meng Xiangjin,Zhou Wanpeng,Jiang Yongbiao,Zhang Shuming,Wu Zhichun.2015.Zicron geochronology and evolution sequence of the acidic volcano-intrusive complexfrom Xiangshan,Jiangxi Province.Chinese Journal of Geology,50(3):684~707(in Chinese with English abstract).
Fang Xiheng,Hou Wenyao,Wan Guoliang.1982.Petrographic studies of the volcanic complex in the Xiangshan caldera,1:1~10(in Chinese with English abstract).
Fan Honghai,Wang Dezi,Shen Weizhou,Liu Chang shi,Wang Xiang,Ling Hongfei.2005.Formation age of the intermediatebasic dikes and volcanic-Iintrusive complex in Xiangshan,Jiangxi Province.Geolgical Review.51(1):86~91(in Chinese with English abstract).
Fan Honghai,Ling Hongfei,Shen Weizhou,Wang Dezi,Liu Changshi,Jiang Yaohui.2001.Nd-Sr-Pb isotope geochemistry of the volcanicintrusive complex at Xiangshan,Jiangxi province.Acta Petrologica Sinica,17(3):395~402(in Chinese with English abstract).
Faure G.1986.Prineiples of isotope geology.Michigan:University of Michigan,200~249.
Fujimaki H.1986.Partition coefficients of Hf,Zr and REE between zircon,apatite and liquid.Contributions to Mineralogy and Petrology,94(1):42~45.
He Zhenyu,Xu Xisheng.2012.Petrogenesis of the Late Yanshanian mantle-derived intrusions in southeastern China:Response to the geodynamics of paleo-Pacific plate subduction.Chemical Geology,328:208~221.
Hu Ruizhong,Bi Xianwu.2008.Uranium metallogenesis in South China and its relationship to crustal extension during the cretaceous to tertiary.Econ Geol,103(3):583~598.
Hu Ruizhong,Bi Xianwu,Su Wenchao,Peng Jiantang,Li Chaoyang.2004.Meallogenesis and crustal extension during the cretaceous-tertiary in south China.Earth Science Frontiers,11(1):153~160(in Chinese with English abstract).
Jahn B M.1974.Mesozoic thermal events in southeastChina.Nature,248(4):480~483.
Jahn B M,Zhou X H,Li J L.1990.Formation and tectonic evolution of southeastern China and Taiwan:isotopic and geochemical constraints.Tectonophysics,183(1/4):145~160.
Kamona A F,Lévêque J,Friedrich G,Haack U.1999.Lead isotopes of the carbonate-hosted Kabwe,Tsumeb,and Kipushi Pb-Zn-Cu sulphide deposits in relation to Pan African orogensis in the Damaran-Lufilian Fold Belt of Central Africa.Mineralium Deposita,34(3):273~283.
Koppers A A P,Morgan J P,Morgan J W,Staudigel H.2001.Testing the fixed hotspot hypothesis using(40)Ar/(39)Ar age progressions along seamount trails.Earth and Planetary Science Letters,185(3/4):237~252.
Li Xianhua,Wang Yixian,Zhao,Zhenhua,Chen Duofu,Zhang Hong.1998.Shrimp U-Pb zircon geochronology for amphbolite from the Precambrian basement in SW Zhejiang and NW Fujian provinces.Geochimica,27(4):327~334(in Chinese with English abstract).
Li XianHua,Li WuXian,Li ZhengXian.2007.On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range,South China.Chinese Science Bulletin,52(9):981~991.
Li Xianhua,Zhou Hanwen,Liu Ying,Lee Chiyu,Sun Min,Chen Chenhong.2000.Shoshonitic intrusive suite in SE Guangxi:Petrology and geochemistry.Chinese Science Bulletin,45(7):653~659.
Li Xianhua,Chen Zhigang,Liu Dunyi.2003.Jurassic gabbrogranite-syenite suites from southern Jiangxi Province(SEChina):age,origin and tectonic significance.International Geology Review,45:898~921.
Li Zhen.Qiu Jianshen.Yang Xuemei.2013.A review of the geochronology and geochemistry of Late Yanshanian(Cretaceous)plutons along theFujian coastal area of southeastern China:Implications for magma evolution related to slab break-off and rollback in the Cretaceous.Earth-Science Reviews,128~232.
Liegeois J P,Navez J,Hertogen J.1998.Contrasting origin of postcollisional high-alkaline and shoshonitic versus alkaline and peralkaline granitoids.The use of sliding normalization.Lithos,45(1):1~28.
Liu Lei,Xu Xisheng,Xia Yan.2014.Cretaceous Pacific plate movement beneath SE China:Evidence from episodic volcanism and lelated intrusions.Tectonophysics,614:170~184.
Liu Changshi,Zhu Jinchu,Shen Weizhou,Xu Shijin.1990.Classification and source materials of continental crust transformation serises grantoids in South China.Acta Geologica Sinica,1:43~52(in Chinese with English abstract).
Liu Jiayuan.1985.Xiangshan igneous pluton-agranitc hypabyssal intrusive volcanic complex.Geochimica,14(2):142~149(in Chinese with English abstract).
Liu Changshi,Zhu Jinchu,Shen Weizhou,Xu Shijin,Yang Xinyi.1990.Evolution of continental crust and material source(genesis)of granitoids in S.China.Geotectonica et Metallogenia,2(14):395~402(in Chinese with English abstract).
Liu Hanbin,Jin Guishan,Li Junjie,Han Juan,Zhang Jianfeng,Zhang Jia,Zhong Fangwen,Guo Dongqiao.2013.Determination of stable isotope composition in uranium geological samples.World Nuclear Geoscience,30(3):174~179(in Chinese with English abstract).
Ling Hongfei,Xu Shijin,Shen Weizhou,Wang Rucheng,Lin Yuping.1998.Nd,Sr,Pb and O isotopic compositions of Late Proterozoic Gezong-and Donggu-granites in the western margin of Yangtze Plate and comparison with other coeval granitoids.Acta Petrologica Sinica,14(3):269~277(in Chinese with English abstract).
Mahood G,Hildreth W.1983.Large partition coefficients for trace elements in high-silicarhyolites.Geochimica et Cosmochimica Acta,47(1):11~30.
Mo Xuanxue,Zhao Zhidan,Deng Jinfu,Dong Guochen,Zhou Su,Guo Tieying,Zhang Shuangquan,Wang Liangliang.2003.Pesponse of volcanism to the India-Asia collision.Earth Science Frontiers,10(3):135~148(in Chinese with English abstract).
Mao Jinwen,Chen Maohong,Yuan Shuda,Guo Chunli.2011.Geological characteristics of the Qinhang(or Shihang)metallogenic belt in South China and spatial-temporal distribution regularity of mineral deposits.Acta Geologica Sinica,85(5):636~657(in Chinese with English abstract).
Pearce J A.1996.Source and settings of granitic rocks.Episodes,19(4):120~125.
Philpotts J A,Schnetzler C C.1970.Phenocryst-matrix partition coefficients for K,Rb,Sr and Ba,with applications to anorthosite and basalt genesis.Geochimica et Cosmochimica Acta,34(3):307~322.
Su Huimin,Mao Jingwen,Santosh M,Xie Guiqing.2014.Petrogenesis and tectonic significance of Late Jurassic-Eaily Cretaceous volcanic-intrusive complex in the Tianhuashan basin,South China Ore Geology Reviews,56:566~583.
Tao Kuiyuan,Huang Guangzhao,Wang Meixing,Yin Jiaheng,Wang Zhanyu,Xie Jiaying.1985.The characteristics and genetic mechanism of porphyroclastic lavas inSoutheastern China.Bull Nanjing inst geol M R Chinese acad geol sci,6(1):1~21(in Chinese with English abstract).
Wan Tianfeng,Wang Yamei,Liu Junlai.2008.Detachments and magmatic source depth in lithosphere of Eastern China during Yanshanian and Sichuanian stages.Earth Science Frontiers,15(3):1~35(in Chinese with English abstract).
Wang Dezi,Liu Changshi,Shen Weizhou,Chen Fanrong.1993.The contrast between Tonglu I-type and Xiangshan S-type clastoporphyritic lava.Acta Petrologica Sinica,9(1):44~54(in Chinese with English abstract).
Wang Yuejun,Fan Weiming,Guo Feng.2003.Geochemistry of Early Mesozoic potassium-rich dioritic-graniodioritic intrusions inSoutheastern Hunan Province,South China:Petrogenesis and tectonic implication.Geochemical Journal,37(4):427~448.
Wu Jianhua.1999.A discussion on the lithostratigraphical division of continental volcanic terrain.45(Suppl):93~100(in Chinese with English abstract).
Wu Rengui.1999.The features of volcanic formation in Ruyiting profile of Xiangshan.Journal of East China geological institute,22(3):201~208(in Chinese with English abstract).
Xie Jiaying,Tao Kuiyuan,Xie Fangze.1995.A study on tufflava facies feature,model and its genesis.Volcanology mineral resources,16(3):1~6(in Chinese with English abstract).
Xiao Qinghui,Li Yong,Feng Yanfang,Qiu Ruizhao,Zhang Yu.2010.A preliminary study of the relationship between Mesozoic lithosphere evolution in eastern China and the subduction of the Pacific plate.Geology in China,37(4):1093~1102(in Chinese with English abstract).
Yu Dagan,Ye Fawang,Wang Yong.2001.Active succession establishment for volcanic-intrusive complex in middle-late lower cretaceous in guangfeng,Jiangxi and its geological implication.Geotectonic et metallogenia,25(3):271~276(in Chinese with English abstract).
Yu Dagan,Guang Taiyang,Huang Guofu.1996.Metamorphic basement characteristics,palaeo-tectonic patterns and prospect of uranium and gold mineralization in South(East)China.Uranium geology,12(6):321~330(in Chinese with English abstract).
Yang ShuiYuan,Jiang ShaoYong,Jiang YaoHui,Zhao KuiDong,Fan HongHai.2010.Zircon U-Pb geochronology,Hf isotopic composition and geological implications of the rhyodacite and rhyodacitic porphyry in the Xiangshan uranium ore field,Jiangxi Province,China.Science China Earth Sciences,53(10):1411~1426.
Yang Shuiyuan.2013.Petrogenesis and geodynamic setting of magmatic rocks from uranium-bearing volcanic basins,GanHang Belt,Southeast China:[Degree of Doctor of Philosophy].Nanjing:Nanjing University,21~79(in Chinese with English abstract).
Yang S Y,Jiang S Y,Zhao K D,Jiang,Y H,Fan H H.2012.Zircon U-Pb geochronology,geochemistry and Sr-Nd-Hf isotopic compositions of the rhyolite porphyry from the Zhoujiashan deposit in Xiangshan uranium ore field,Jiangxi Province,SE China.Acta Petrologica Sinica,28(12):3915~3928.
Yurimoto H,Duke E F,Papike J J,Shearer C K.1990.Are discontinuous chondrite-normalized REE patterns in pegmatitic granite systems the results of monazite fractionation?.Geochimica et Cosmochimica Acta,54(7):2141~2145.
Zhang Wanliang.2005.Reverse magmatic evolution series of the Xiangshan volcanic intrusive complex.Geology in China,32(4):548~556(in Chinese with English abstract).
Zhang Wanliang,Li Ziying.2007.Single zircon U-Pb age of rhyodacite from Xiangshan area and itsgeological implications.Acta petrologica et mineralogical,26(1):21~26(in Chinese with English abstract).
Zhang Qi.2013.Is the Mesozoic magmatism in easternChina related to the westward subduction of the Pacific plate?.Acta petrologica et mineralogical,32(1):113~118(in Chinese with English abstract).
Zhou X M,Li W X.2000.Origin of Late Mesozoic igneous rocks inSoutheastern China:implications for lithosphere subduction and underplating of mafic magmas.Technophysics,326(3/4):269~287.
Zhou Xinmin,Sun Tao,Shen Weizhou,Shu Lliangshu,Niu Yaoling.2006.Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:A response to tectonic evolution.Episodes,29(1):26~33.
陈小明,陆建军,刘昌实,赵连泽,王德滋,李惠民.1999.桐庐、相山火山-侵入杂岩单颗粒锆石U-Pb年龄.岩石学报,15(2):272~278.
窦小平.2005.相山火山盆地岩石稀土元素分布特征及其成因探讨.铀矿地质,21(6):338~344.
段芸,赵连泽,范洪海,王德滋.2001.江西相山火山-侵入杂岩及其包体稀土元素地球化学.高校地质学报,7(1):92~98.
郭冬发,武朝晖,崔建勇,欧光习,范光.2007.铀矿地质分析测试技术回顾与新形势下网络实验室构建.世界核地质科学,24(1):50~63.
郭福生,杨庆坤,谢财富,孟祥金,周万蓬,姜勇彪,张树明,吴志春.2015.江西相山酸性火山-侵入杂岩精确年代学与演化序列研究.地质科学,50(3):684~707.
孟艳宁,范红海,王凤岗.2015.江西相山矿田邹家山矿床铀钍矿物的年代学研究.地质学报,89(z1):18~21.
方锡珩,侯文尧,万国良.1982.相山破火山口火山杂岩体的岩石学研究.岩矿测试,1∶1~10.
范洪海,王德滋,沈渭洲,刘昌实,汪相,凌洪飞.2005.江西相山火山-侵入杂岩及中基性脉岩形成时代研究.地质论评,51(1):86~91.
范洪海,凌洪飞,沈渭洲,王德滋,刘昌实,姜耀辉.2001.相山火山-侵入杂岩Nd-Sr-Pb同位素地球化学特征.岩石学报,17(3):395~402.
胡瑞忠,毕献武,苏文超,彭建堂,李朝阳.2004.华南白垩-第三纪地壳拉张与铀成矿的关系.地学前缘,11(1):153~160.
刘家远.1985.相山岩体---一个壳源花岗质浅成侵入火山杂岩体.地球化学,14(2):142~149.
刘昌实,朱金初,沈渭洲,徐士进,杨心宜.1990.华南花岗岩物源成因特征与陆壳演化.大地构造与成矿,2(14):395~402.
刘汉彬,金贵善,李军杰,韩娟,张建锋,张佳,钟芳文,郭东侨.2013.铀矿地质样品的稳定同位素组成测试方法.世界核地质科学,30(3):174~179.
李献华,王一先,赵振华,陈多福,张宏.1998.闽浙古元古代斜长角闪岩的离子探针锆石U-Pb年代学.地球化学,27(4):327~334.
刘昌实,朱金初,沈渭洲,徐士进.1990.华南陆壳改造系列花岗岩类型划分和成岩物质来源.地质学报,1:43~52.
凌洪飞,徐士进,沈渭洲,王汝成,林雨萍.1998.格宗、东谷岩体Nd、Sr、Pb、O同位素特征及其与扬子板块边缘其它晋宁期花岗岩对比.岩石学报,14(3):269~277.
莫宣学,赵志丹,邓晋福,董国臣,周肃,郭铁鹰,张双全,王亮亮.2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘,10(3):135~148.
毛景文,陈懋弘,袁顺达,郭春丽.2011.华南地区钦杭成矿带地质特征和矿床时空分布规律.地质学报,85(5):636~657.
郭建,李子颖,黄志章,李秀珍.2015.相山铀矿田邹家山矿床成矿流体氢氧同位素地球化学特征.地质学报,89(z1):99~100.
陶奎元,黄光昭,王美星,尹家衡,王占宇,谢家莹.1985.中国东南部碎斑熔岩基本特征及成因机理的探讨.中国地质科学院南京地质矿产研究所所刊,6(1):1~21.
万天丰,王亚妹,刘俊来.2008.中国东部燕山期和四川期岩石圈构造滑脱与岩浆起源深度.地学前缘,15(3):1~35.
王德滋,刘昌实,沈渭洲,陈繁荣.1993.桐庐I型和相山S型两类碎斑熔岩对比.岩石学报,9(1):44~54.
巫建华.1999.陆相火山岩区岩石地层划分的讨论.地质论评,45(增刊):93~100.
吴仁贵.1999.相山地区如意亭剖面火山建造特征.华东地质学院学报,22(3):201~208.
夏林圻,夏祖春,张诚,Clocchiatti R,Joron J L,Dardel J.1992.相山中生代含铀火山杂岩岩石地球化学.北京:地质出版社,1~35.
谢家莹,陶奎元,谢芳责.1995.试论凝灰熔岩相特征、相模式及其成因.火山地质与矿产,16(3):1~6.
肖庆辉,刘勇,冯艳芳,邱瑞照,张昱.2010.中国东部中生代岩石圈演化与太平洋板块俯冲消减关系的讨论.中国地质,37(4):1093~1102.
肖庆辉,邓晋福,马大铨.2002.花岗岩研究思维与方法.北京:地质出版社,276~294.
余达淦,叶发旺,王勇.2001.江西广丰白垩世中晚期盆地火山-侵入杂岩活动序列确认及其地质意义.大地构造与成矿学,25(3):271~276.
余达淦,管太阳,黄国夫.1996.华南(东)变质基底特征、古构造型式及铀、金矿化远景.铀矿地质,12(6):321~330.
杨水源.2013.华南赣杭构造带含铀火山盆地岩浆岩的成因机制及动力学背景:[博士学位论文].南京:南京大学,21~79.
张万良.2005.相山火山-侵入杂岩的反方向岩浆演化系列研究.中国地质,32(4):548~556.
张万良,李子颖.2007.相山“流纹英安岩”单颗粒锆石U-Pb年龄及地质意义.岩石矿物学杂志,26(1):21~26.
张旗.2013.中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?岩石矿物学杂志,32(1):113~118.
朱炳泉.1998.地球科学中同位素体系理论与应用---兼论中国大陆壳幔演化.北京:科学出版社.
Chen Jiangfeng,Jahn Bor-ming.1998.Crustal evolution of southeasternChina:Nd and Sr isotopic evidence.Tectonophysics,284:101~133.
Condie K C.2001.Mantle Plume and Their Record in Earth History.London:Cambridge University Press.
Chen Xiaoming,Lu Jianjun,Liu Changshi,Zhao Lianze,Wang Dezi,Li Huimin.1999.Single-grain zircon U-Pb isotopic ages of the volcanic-intrusive complexes in Tonglu and Xiangshan areas.Acta Petrologica Sinica,15(2):272~278(in Chinese with English abstract).
Chen Weifeng,Chen Peirong,Xu Xisheng,Zhang Min.2005.Geochemical characteristics of Cretaceous basaltic rocks in South China and constraints on Pacific plate subduction.Science in China Series D Earth Sciences,48(12):2104~2117.
Doe B R,Zartman R E.1979.Plumbotectonics the Phanerozoic.Barnes H L.Geochemistry of Hydrothermalore Deposits and.Ed.Wilev Interscience.Chap2,22~70.
Dou Xiaoping.2005.REE distribution characteristics of volcanic and epimetamorphic rocks in Xiangshan volcanic basin and discussion on their genesis.Uranium Geology,21(6):338~344(in Chinese with English abstract).
Duan Yun,Zhao Lianze,Fan Honghai,Wang Dezi.2001.REE-Geochemistry of Mesozoic Volcanic-Intrusive Complex and Dark Inclusions inXiangshan District,Jiangxi Pronvince.Geological Journal of China Universities,7(1):92~98(in Chinese with English abstract).
Guo Dongfa,Wu Zhaohui,Cui Jianyong,Ou Guangxi,Fan Guang.2007.Review onur anium geoanalysis and introduction to the concept of network analytical labor ator ies.World Nuclear Geoscience,24(1):50~63(in Chinese with English abstract).
Guo Fusheng,Yang Qingkun,Xie Caifu,Meng Xiangjin,Zhou Wanpeng,Jiang Yongbiao,Zhang Shuming,Wu Zhichun.2015.Zicron geochronology and evolution sequence of the acidic volcano-intrusive complexfrom Xiangshan,Jiangxi Province.Chinese Journal of Geology,50(3):684~707(in Chinese with English abstract).
Fang Xiheng,Hou Wenyao,Wan Guoliang.1982.Petrographic studies of the volcanic complex in the Xiangshan caldera,1:1~10(in Chinese with English abstract).
Fan Honghai,Wang Dezi,Shen Weizhou,Liu Chang shi,Wang Xiang,Ling Hongfei.2005.Formation age of the intermediatebasic dikes and volcanic-Iintrusive complex in Xiangshan,Jiangxi Province.Geolgical Review.51(1):86~91(in Chinese with English abstract).
Fan Honghai,Ling Hongfei,Shen Weizhou,Wang Dezi,Liu Changshi,Jiang Yaohui.2001.Nd-Sr-Pb isotope geochemistry of the volcanicintrusive complex at Xiangshan,Jiangxi province.Acta Petrologica Sinica,17(3):395~402(in Chinese with English abstract).
Faure G.1986.Prineiples of isotope geology.Michigan:University of Michigan,200~249.
Fujimaki H.1986.Partition coefficients of Hf,Zr and REE between zircon,apatite and liquid.Contributions to Mineralogy and Petrology,94(1):42~45.
He Zhenyu,Xu Xisheng.2012.Petrogenesis of the Late Yanshanian mantle-derived intrusions in southeastern China:Response to the geodynamics of paleo-Pacific plate subduction.Chemical Geology,328:208~221.
Hu Ruizhong,Bi Xianwu.2008.Uranium metallogenesis in South China and its relationship to crustal extension during the cretaceous to tertiary.Econ Geol,103(3):583~598.
Hu Ruizhong,Bi Xianwu,Su Wenchao,Peng Jiantang,Li Chaoyang.2004.Meallogenesis and crustal extension during the cretaceous-tertiary in south China.Earth Science Frontiers,11(1):153~160(in Chinese with English abstract).
Jahn B M.1974.Mesozoic thermal events in southeastChina.Nature,248(4):480~483.
Jahn B M,Zhou X H,Li J L.1990.Formation and tectonic evolution of southeastern China and Taiwan:isotopic and geochemical constraints.Tectonophysics,183(1/4):145~160.
Kamona A F,Lévêque J,Friedrich G,Haack U.1999.Lead isotopes of the carbonate-hosted Kabwe,Tsumeb,and Kipushi Pb-Zn-Cu sulphide deposits in relation to Pan African orogensis in the Damaran-Lufilian Fold Belt of Central Africa.Mineralium Deposita,34(3):273~283.
Koppers A A P,Morgan J P,Morgan J W,Staudigel H.2001.Testing the fixed hotspot hypothesis using(40)Ar/(39)Ar age progressions along seamount trails.Earth and Planetary Science Letters,185(3/4):237~252.
Li Xianhua,Wang Yixian,Zhao,Zhenhua,Chen Duofu,Zhang Hong.1998.Shrimp U-Pb zircon geochronology for amphbolite from the Precambrian basement in SW Zhejiang and NW Fujian provinces.Geochimica,27(4):327~334(in Chinese with English abstract).
Li XianHua,Li WuXian,Li ZhengXian.2007.On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range,South China.Chinese Science Bulletin,52(9):981~991.
Li Xianhua,Zhou Hanwen,Liu Ying,Lee Chiyu,Sun Min,Chen Chenhong.2000.Shoshonitic intrusive suite in SE Guangxi:Petrology and geochemistry.Chinese Science Bulletin,45(7):653~659.
Li Xianhua,Chen Zhigang,Liu Dunyi.2003.Jurassic gabbrogranite-syenite suites from southern Jiangxi Province(SEChina):age,origin and tectonic significance.International Geology Review,45:898~921.
Li Zhen.Qiu Jianshen.Yang Xuemei.2013.A review of the geochronology and geochemistry of Late Yanshanian(Cretaceous)plutons along theFujian coastal area of southeastern China:Implications for magma evolution related to slab break-off and rollback in the Cretaceous.Earth-Science Reviews,128~232.
Liegeois J P,Navez J,Hertogen J.1998.Contrasting origin of postcollisional high-alkaline and shoshonitic versus alkaline and peralkaline granitoids.The use of sliding normalization.Lithos,45(1):1~28.
Liu Lei,Xu Xisheng,Xia Yan.2014.Cretaceous Pacific plate movement beneath SE China:Evidence from episodic volcanism and lelated intrusions.Tectonophysics,614:170~184.
Liu Changshi,Zhu Jinchu,Shen Weizhou,Xu Shijin.1990.Classification and source materials of continental crust transformation serises grantoids in South China.Acta Geologica Sinica,1:43~52(in Chinese with English abstract).
Liu Jiayuan.1985.Xiangshan igneous pluton-agranitc hypabyssal intrusive volcanic complex.Geochimica,14(2):142~149(in Chinese with English abstract).
Liu Changshi,Zhu Jinchu,Shen Weizhou,Xu Shijin,Yang Xinyi.1990.Evolution of continental crust and material source(genesis)of granitoids in S.China.Geotectonica et Metallogenia,2(14):395~402(in Chinese with English abstract).
Liu Hanbin,Jin Guishan,Li Junjie,Han Juan,Zhang Jianfeng,Zhang Jia,Zhong Fangwen,Guo Dongqiao.2013.Determination of stable isotope composition in uranium geological samples.World Nuclear Geoscience,30(3):174~179(in Chinese with English abstract).
Ling Hongfei,Xu Shijin,Shen Weizhou,Wang Rucheng,Lin Yuping.1998.Nd,Sr,Pb and O isotopic compositions of Late Proterozoic Gezong-and Donggu-granites in the western margin of Yangtze Plate and comparison with other coeval granitoids.Acta Petrologica Sinica,14(3):269~277(in Chinese with English abstract).
Mahood G,Hildreth W.1983.Large partition coefficients for trace elements in high-silicarhyolites.Geochimica et Cosmochimica Acta,47(1):11~30.
Mo Xuanxue,Zhao Zhidan,Deng Jinfu,Dong Guochen,Zhou Su,Guo Tieying,Zhang Shuangquan,Wang Liangliang.2003.Pesponse of volcanism to the India-Asia collision.Earth Science Frontiers,10(3):135~148(in Chinese with English abstract).
Mao Jinwen,Chen Maohong,Yuan Shuda,Guo Chunli.2011.Geological characteristics of the Qinhang(or Shihang)metallogenic belt in South China and spatial-temporal distribution regularity of mineral deposits.Acta Geologica Sinica,85(5):636~657(in Chinese with English abstract).
Pearce J A.1996.Source and settings of granitic rocks.Episodes,19(4):120~125.
Philpotts J A,Schnetzler C C.1970.Phenocryst-matrix partition coefficients for K,Rb,Sr and Ba,with applications to anorthosite and basalt genesis.Geochimica et Cosmochimica Acta,34(3):307~322.
Su Huimin,Mao Jingwen,Santosh M,Xie Guiqing.2014.Petrogenesis and tectonic significance of Late Jurassic-Eaily Cretaceous volcanic-intrusive complex in the Tianhuashan basin,South China Ore Geology Reviews,56:566~583.
Tao Kuiyuan,Huang Guangzhao,Wang Meixing,Yin Jiaheng,Wang Zhanyu,Xie Jiaying.1985.The characteristics and genetic mechanism of porphyroclastic lavas inSoutheastern China.Bull Nanjing inst geol M R Chinese acad geol sci,6(1):1~21(in Chinese with English abstract).
Wan Tianfeng,Wang Yamei,Liu Junlai.2008.Detachments and magmatic source depth in lithosphere of Eastern China during Yanshanian and Sichuanian stages.Earth Science Frontiers,15(3):1~35(in Chinese with English abstract).
Wang Dezi,Liu Changshi,Shen Weizhou,Chen Fanrong.1993.The contrast between Tonglu I-type and Xiangshan S-type clastoporphyritic lava.Acta Petrologica Sinica,9(1):44~54(in Chinese with English abstract).
Wang Yuejun,Fan Weiming,Guo Feng.2003.Geochemistry of Early Mesozoic potassium-rich dioritic-graniodioritic intrusions inSoutheastern Hunan Province,South China:Petrogenesis and tectonic implication.Geochemical Journal,37(4):427~448.
Wu Jianhua.1999.A discussion on the lithostratigraphical division of continental volcanic terrain.45(Suppl):93~100(in Chinese with English abstract).
Wu Rengui.1999.The features of volcanic formation in Ruyiting profile of Xiangshan.Journal of East China geological institute,22(3):201~208(in Chinese with English abstract).
Xie Jiaying,Tao Kuiyuan,Xie Fangze.1995.A study on tufflava facies feature,model and its genesis.Volcanology mineral resources,16(3):1~6(in Chinese with English abstract).
Xiao Qinghui,Li Yong,Feng Yanfang,Qiu Ruizhao,Zhang Yu.2010.A preliminary study of the relationship between Mesozoic lithosphere evolution in eastern China and the subduction of the Pacific plate.Geology in China,37(4):1093~1102(in Chinese with English abstract).
Yu Dagan,Ye Fawang,Wang Yong.2001.Active succession establishment for volcanic-intrusive complex in middle-late lower cretaceous in guangfeng,Jiangxi and its geological implication.Geotectonic et metallogenia,25(3):271~276(in Chinese with English abstract).
Yu Dagan,Guang Taiyang,Huang Guofu.1996.Metamorphic basement characteristics,palaeo-tectonic patterns and prospect of uranium and gold mineralization in South(East)China.Uranium geology,12(6):321~330(in Chinese with English abstract).
Yang ShuiYuan,Jiang ShaoYong,Jiang YaoHui,Zhao KuiDong,Fan HongHai.2010.Zircon U-Pb geochronology,Hf isotopic composition and geological implications of the rhyodacite and rhyodacitic porphyry in the Xiangshan uranium ore field,Jiangxi Province,China.Science China Earth Sciences,53(10):1411~1426.
Yang Shuiyuan.2013.Petrogenesis and geodynamic setting of magmatic rocks from uranium-bearing volcanic basins,GanHang Belt,Southeast China:[Degree of Doctor of Philosophy].Nanjing:Nanjing University,21~79(in Chinese with English abstract).
Yang S Y,Jiang S Y,Zhao K D,Jiang,Y H,Fan H H.2012.Zircon U-Pb geochronology,geochemistry and Sr-Nd-Hf isotopic compositions of the rhyolite porphyry from the Zhoujiashan deposit in Xiangshan uranium ore field,Jiangxi Province,SE China.Acta Petrologica Sinica,28(12):3915~3928.
Yurimoto H,Duke E F,Papike J J,Shearer C K.1990.Are discontinuous chondrite-normalized REE patterns in pegmatitic granite systems the results of monazite fractionation?.Geochimica et Cosmochimica Acta,54(7):2141~2145.
Zhang Wanliang.2005.Reverse magmatic evolution series of the Xiangshan volcanic intrusive complex.Geology in China,32(4):548~556(in Chinese with English abstract).
Zhang Wanliang,Li Ziying.2007.Single zircon U-Pb age of rhyodacite from Xiangshan area and itsgeological implications.Acta petrologica et mineralogical,26(1):21~26(in Chinese with English abstract).
Zhang Qi.2013.Is the Mesozoic magmatism in easternChina related to the westward subduction of the Pacific plate?.Acta petrologica et mineralogical,32(1):113~118(in Chinese with English abstract).
Zhou X M,Li W X.2000.Origin of Late Mesozoic igneous rocks inSoutheastern China:implications for lithosphere subduction and underplating of mafic magmas.Technophysics,326(3/4):269~287.
Zhou Xinmin,Sun Tao,Shen Weizhou,Shu Lliangshu,Niu Yaoling.2006.Petrogenesis of Mesozoic granitoids and volcanic rocks in South China:A response to tectonic evolution.Episodes,29(1):26~33.
陈小明,陆建军,刘昌实,赵连泽,王德滋,李惠民.1999.桐庐、相山火山-侵入杂岩单颗粒锆石U-Pb年龄.岩石学报,15(2):272~278.
窦小平.2005.相山火山盆地岩石稀土元素分布特征及其成因探讨.铀矿地质,21(6):338~344.
段芸,赵连泽,范洪海,王德滋.2001.江西相山火山-侵入杂岩及其包体稀土元素地球化学.高校地质学报,7(1):92~98.
郭冬发,武朝晖,崔建勇,欧光习,范光.2007.铀矿地质分析测试技术回顾与新形势下网络实验室构建.世界核地质科学,24(1):50~63.
郭福生,杨庆坤,谢财富,孟祥金,周万蓬,姜勇彪,张树明,吴志春.2015.江西相山酸性火山-侵入杂岩精确年代学与演化序列研究.地质科学,50(3):684~707.
孟艳宁,范红海,王凤岗.2015.江西相山矿田邹家山矿床铀钍矿物的年代学研究.地质学报,89(z1):18~21.
方锡珩,侯文尧,万国良.1982.相山破火山口火山杂岩体的岩石学研究.岩矿测试,1∶1~10.
范洪海,王德滋,沈渭洲,刘昌实,汪相,凌洪飞.2005.江西相山火山-侵入杂岩及中基性脉岩形成时代研究.地质论评,51(1):86~91.
范洪海,凌洪飞,沈渭洲,王德滋,刘昌实,姜耀辉.2001.相山火山-侵入杂岩Nd-Sr-Pb同位素地球化学特征.岩石学报,17(3):395~402.
胡瑞忠,毕献武,苏文超,彭建堂,李朝阳.2004.华南白垩-第三纪地壳拉张与铀成矿的关系.地学前缘,11(1):153~160.
刘家远.1985.相山岩体---一个壳源花岗质浅成侵入火山杂岩体.地球化学,14(2):142~149.
刘昌实,朱金初,沈渭洲,徐士进,杨心宜.1990.华南花岗岩物源成因特征与陆壳演化.大地构造与成矿,2(14):395~402.
刘汉彬,金贵善,李军杰,韩娟,张建锋,张佳,钟芳文,郭东侨.2013.铀矿地质样品的稳定同位素组成测试方法.世界核地质科学,30(3):174~179.
李献华,王一先,赵振华,陈多福,张宏.1998.闽浙古元古代斜长角闪岩的离子探针锆石U-Pb年代学.地球化学,27(4):327~334.
刘昌实,朱金初,沈渭洲,徐士进.1990.华南陆壳改造系列花岗岩类型划分和成岩物质来源.地质学报,1:43~52.
凌洪飞,徐士进,沈渭洲,王汝成,林雨萍.1998.格宗、东谷岩体Nd、Sr、Pb、O同位素特征及其与扬子板块边缘其它晋宁期花岗岩对比.岩石学报,14(3):269~277.
莫宣学,赵志丹,邓晋福,董国臣,周肃,郭铁鹰,张双全,王亮亮.2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘,10(3):135~148.
毛景文,陈懋弘,袁顺达,郭春丽.2011.华南地区钦杭成矿带地质特征和矿床时空分布规律.地质学报,85(5):636~657.
郭建,李子颖,黄志章,李秀珍.2015.相山铀矿田邹家山矿床成矿流体氢氧同位素地球化学特征.地质学报,89(z1):99~100.
陶奎元,黄光昭,王美星,尹家衡,王占宇,谢家莹.1985.中国东南部碎斑熔岩基本特征及成因机理的探讨.中国地质科学院南京地质矿产研究所所刊,6(1):1~21.
万天丰,王亚妹,刘俊来.2008.中国东部燕山期和四川期岩石圈构造滑脱与岩浆起源深度.地学前缘,15(3):1~35.
王德滋,刘昌实,沈渭洲,陈繁荣.1993.桐庐I型和相山S型两类碎斑熔岩对比.岩石学报,9(1):44~54.
巫建华.1999.陆相火山岩区岩石地层划分的讨论.地质论评,45(增刊):93~100.
吴仁贵.1999.相山地区如意亭剖面火山建造特征.华东地质学院学报,22(3):201~208.
夏林圻,夏祖春,张诚,Clocchiatti R,Joron J L,Dardel J.1992.相山中生代含铀火山杂岩岩石地球化学.北京:地质出版社,1~35.
谢家莹,陶奎元,谢芳责.1995.试论凝灰熔岩相特征、相模式及其成因.火山地质与矿产,16(3):1~6.
肖庆辉,刘勇,冯艳芳,邱瑞照,张昱.2010.中国东部中生代岩石圈演化与太平洋板块俯冲消减关系的讨论.中国地质,37(4):1093~1102.
肖庆辉,邓晋福,马大铨.2002.花岗岩研究思维与方法.北京:地质出版社,276~294.
余达淦,叶发旺,王勇.2001.江西广丰白垩世中晚期盆地火山-侵入杂岩活动序列确认及其地质意义.大地构造与成矿学,25(3):271~276.
余达淦,管太阳,黄国夫.1996.华南(东)变质基底特征、古构造型式及铀、金矿化远景.铀矿地质,12(6):321~330.
杨水源.2013.华南赣杭构造带含铀火山盆地岩浆岩的成因机制及动力学背景:[博士学位论文].南京:南京大学,21~79.
张万良.2005.相山火山-侵入杂岩的反方向岩浆演化系列研究.中国地质,32(4):548~556.
张万良,李子颖.2007.相山“流纹英安岩”单颗粒锆石U-Pb年龄及地质意义.岩石矿物学杂志,26(1):21~26.
张旗.2013.中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?岩石矿物学杂志,32(1):113~118.
朱炳泉.1998.地球科学中同位素体系理论与应用---兼论中国大陆壳幔演化.北京:科学出版社.