辽东岫岩地区晚三叠世侵入岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及地质意义
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摘要
辽东半岛一直是研究华北克拉通减薄的热点地区,前人对于晚三叠世时期辽东半岛的构造环境一直有不同的认识。本文选择辽东岫岩地区出露的后边沟岭黑云母二长花岗岩和大黑坑石英二长闪长岩进行了LA-ICP-MS锆石U-Pb年代学、岩石地球化学的研究,并对上述两个岩体的岩浆来源及形成环境进行了讨论,得出以下认识:辽东岫岩地区后边沟岭黑云母二长花岗岩和大黑坑石英二长闪长岩均形成于晚三叠世(220.9±1.2 Ma和220.3±1 Ma);地球化学研究表明:后边沟岭黑云母二长花岗岩具高硅、富碱的特征,属A型花岗岩;大黑坑石英二长闪长岩具高镁的特征;后边沟岭黑云母二长花岗岩和大黑坑石英二长闪长岩具有相似的稀土元素和微量元素特征,二者均显示轻稀土分馏明显,重稀土分馏不明显的特征,均富集大离子亲石元素Rb、K,亏损Ba、Sr,富集高场强元素Th、La、Ce、Nd、Hf、Tb,而亏损P、Nb、Ta、Y等元素;二者具有相同的岩浆来源且均具有壳幔混源的特征;在220.9±1.2～220.3±1.0 Ma这一时期,辽东岫岩地区整体可能处于地壳伸展减薄的构造背景,后边沟岭黑云母二长花岗岩和大黑坑石英二长闪长岩均形成于这一构造背景中,上述两个岩体的形成可能与大陆深俯冲和扬子—华北之间发生陆陆碰撞造山作用后所引起的华北克拉通减薄有关。
Objectives: Liaodong peninsula is always a hot spot area for study of North China Craton( NCC) thinning.Previous researcher still have a disagreenment on tectonic environment in Liaodong peninsula.Metheods: We select biotite monzogranite outcropped in Houbiangouling and quartz monzodiorite outcropped in Daheikeng,Xiuyan area,eastern Liaoning province,to be studied by using LA-ICP-MS zircon U-Pb chronology and Petrogeochemistry.Results : In addition,the origin and formation environment of the above two plutons are discussed and work out the following results: the formation age of Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite is Late Triassic( 220.9 ±1.2 Ma and 220.3 ±1 Ma); the geochemical characteristic of Houbiangouling biotite monzogranite has high content of Si O2,riched in alkali; the Daheikeng quartz monzodiorite has high content of Mg, the obvious fractional distillation of LREE, but HREE is not obvious; the Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite have similar characteristics in rare earth elements and trace elements,both of them show characteristics of light rare earth obvious fractionation,while heavy rare earth fractionation was not obvious,and are enriched in large ion lithophile elements Rb,K,loss Ba,Sr; and enriched in high field intensity elements Th,La,Ce,Nd,Hf,Tb,while loss P,Nb,Ta,Y.Conclusions: Both of them have the same magmatic source and the characteristics of crust—mantle magama mixture; the probable tectonic background is crustal extension and thinning in Xiuyan area,eastern Liaoning province during 220.9 ± 1. 2 Ma ～ 220. 3 ± 1. 0 Ma; the Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite formed in the crustal extension and thinning tectonic background. The formation of the Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite are relate to North China Craton thinning caused by continental collision orogeny between Yangtze Craton and North China Craton.
Objectives: Liaodong peninsula is always a hot spot area for study of North China Craton( NCC) thinning.Previous researcher still have a disagreenment on tectonic environment in Liaodong peninsula.Metheods: We select biotite monzogranite outcropped in Houbiangouling and quartz monzodiorite outcropped in Daheikeng,Xiuyan area,eastern Liaoning province,to be studied by using LA-ICP-MS zircon U-Pb chronology and Petrogeochemistry.Results : In addition,the origin and formation environment of the above two plutons are discussed and work out the following results: the formation age of Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite is Late Triassic( 220.9 ±1.2 Ma and 220.3 ±1 Ma); the geochemical characteristic of Houbiangouling biotite monzogranite has high content of Si O2,riched in alkali; the Daheikeng quartz monzodiorite has high content of Mg, the obvious fractional distillation of LREE, but HREE is not obvious; the Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite have similar characteristics in rare earth elements and trace elements,both of them show characteristics of light rare earth obvious fractionation,while heavy rare earth fractionation was not obvious,and are enriched in large ion lithophile elements Rb,K,loss Ba,Sr; and enriched in high field intensity elements Th,La,Ce,Nd,Hf,Tb,while loss P,Nb,Ta,Y.Conclusions: Both of them have the same magmatic source and the characteristics of crust—mantle magama mixture; the probable tectonic background is crustal extension and thinning in Xiuyan area,eastern Liaoning province during 220.9 ± 1. 2 Ma ～ 220. 3 ± 1. 0 Ma; the Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite formed in the crustal extension and thinning tectonic background. The formation of the Houbiangouling biotite monzogranite and Daheikeng quartz monzodiorite are relate to North China Craton thinning caused by continental collision orogeny between Yangtze Craton and North China Craton.
引文
崔维龙,刘正宏,杜洋,王师捷,万乐.2016.辽东地区大兴岩体LA-ICP-MS锆石U-Pb定年、地球化学特征及地质意义.地球科学与环境学报,38(5):623～637.
邓晋福,冯艳芳,狄永军,刘翠,肖庆辉,苏尚国,赵国春,孟斐,马帅,姚图.2015a.岩浆弧火成岩构造组合与洋陆转换.地质论评,61(3):473～484.
邓晋福,刘翠,冯艳芳,肖庆辉,苏尚国,赵国春,段培新,戴蒙.2015b.关于火成岩常用图解的正确使用:讨论与建议.地质论评,61(4):717～734.
段晓侠,刘建明,王永彬,周伶俐,李永贵,李斌,张壮,张作伦. 2012. 辽宁青城子铅锌多金属矿田晚三叠世岩浆岩年代学、地球化学及地质意义. 岩石学报, 28(2): 595～606.
葛小月,李献华,陈志刚,李伍平.2002.中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因—对中国东部地壳厚度的制约.科学通报,47(6):474～480.
韩宝福,加加美宽雄,李惠民.2004.河北光头山碱性花岗岩的时代、Sr—Nd同位素特征及其对华北古生代壳幔相互作用的意义.岩石学报,20:1375～1388.
贾小辉,王晓地,杨文强,牛志军.2017.钾玄质系列岩石的研究现状.地质论评,63(6):1587～1601.
贾小辉,王强,唐功建.2009.A型花岗岩的研究进展及意义.大地构造与成矿学,33(3):465～480.
李光来,华仁民,胡东泉,黄小娥,张文兰,王旭东.2010.赣南地区石雷石英闪长岩的成因:岩石化学、副矿物微量元素、锆石U-Pb年代学与Sr—Nd—Hf同位素制约.岩石学报,26(3):903～918.
李三忠,郝德峰,赵国春,孙敏,韩宗珠,郭晓玉.2004.丹东花岗岩的地球化学特征及成因.岩石学报, 20(6):1417～1423.
黎心远,赵元艺,刘春花.2018.黑龙江三矿沟—庄乎河地区岩浆岩年代学、地球化学研究及其俯冲构造与成矿意义.地质学报,92(2):244～262.
刘杰勋,郭巍,朱凯.2016.辽东岫岩地区早白垩世侵入岩的年代学、地球化学及地质意义.岩石学报,32(9):2889～2900.
刘阁,朱志新,佘建忠,邓洪涛,赵同阳,王庆军,孙耀峰.2016.新疆西准噶尔朱鲁木特A型花岗岩年代学、地球化学及岩石成因.地质论评,62(2):331～342.
康磊,校培喜,高晓峰,奚仁刚,杨再朝.2016.茫崖山二长花岗岩、石英闪长岩的年代学、地球化学及岩石成因:对阿尔金南缘早古生代构造—岩浆岩化的启示.岩石学报,32(6):1731～1748.
邱士东,辜平阳,庞新愉,董增产,查显峰,查方勇,陈锐明,庄玉军.2015.青海冷湖北片麻状石英闪长岩的MC-LA-ICP-MS锆石U-Pb年龄、地球化学特征及地质意义.地质论评,61(4):948～959.
秦亚,梁一鸿,胡兆初,冯坚,李敏.2013.吉南老岭地区早白垩世铝质A型花岗岩的厘定及其构造意义.地球科学,38(4) : 677～688.
宋运红,杨凤超,闫国磊,魏明辉,石绍山.2016. 辽东地区古元古代花岗岩SHRIMP U-Pb年龄、Hf同位素组成及构造意义.地质学报,90(10):2620～2636.
吴福元,徐义刚,高山,郑建平.2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报,24(6):1145～1174.
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.
吴福元,杨进辉,柳小明.2005.辽东半岛中生代花岗质岩浆作用的年代学格架.高校地质学报,11(3):305～317.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589～1604.
吴福元,葛文春,孙德有.2002.埃达克岩的概念、识别标志及其地质意义.见:肖庆辉,邓晋福,马大铨等著.花岗岩研究思维与方法.北京:地质出版社: 172～191.
杨佳林,顾玉超,杨凤超,李东涛,鞠楠,贾宏翔.2018. 辽东半岛大金山花岗岩体SHRIMP U-Pb年龄、元素地球化学和Hf同位素特征及地质意义.地质论评,64(6):1541～1556
杨凤超,宋运红,郝立波,柴鹏.2015.辽东三家子地区晚侏罗世花岗岩SHRIMP U-Pb年龄、Hf同位素特征及地质意义.地质学报,2015,89(10):1773～1782
杨进辉,吴福元.2009.华北东部晚三叠纪岩浆作用.中国科学D辑:地球科学,39(7):910～921.
杨进辉,吴福元,罗清华,钟孙霖,张艳斌,Wilde S A. 2004. 辽宁丹东地区侏罗纪花岗岩的变形时代40Ar/39Ar年代学制约.岩石学报,20(5):1205～1214.
张朋,陈冬,寇林林,赵岩,杨宏智,沙德铭,王希今.2015. 辽东卧龙泉岩体锆石U-Pb年代学、地球化学、Sr—Nd—Pb同位素特征及其地质意义.地质学报,89(10):1762～1772.
张旗,冉白皋,李承东.2012.A型花岗岩的实质是什么?岩石矿物学杂志,31(4):621～626.
张旗,王焰,熊小林,李承东.2008.埃达克岩和花岗岩:挑战与机遇.北京:中国大地出版社,3～18.
朱金初,张佩华,谢才富,张辉,杨策.2006.南岭西段花山—姑婆山A型花岗质杂岩带:岩石学、地球化学和岩石成因.地质学报,80(4):529～542.
赵振华,王中刚,邹天人,增田彰正.1996.新疆乌伦古富碱侵入岩成因探讨.地球化学,25(3):205～220.
Barth M G,McDonough W F and Rudnick R L.2000.Tracking the budget of Nb and Ta in the continental crust.Chemical Geology,165(3～4):197～213.
Cui Weilong,Liu Zhenghong,Du Yang,Wang Shijie,Wan Le. 2016&. LA-ICP-MS zircon U-Pb dating,geochemical characteristics and geological significance of Daxing pluton in Liaodong Area. Journal of Earth Sciences and Environment, 38(5):623～637.
Creaser R A, Price R C and Wormald R J.1991.A-typr granites revisited: Assessment of a residual-source model. Geology,19:163～166.
Collins W J, Beams S D,White A J R and Chappell B W.1982. Nature and origin of A-type granites with particular reference to Southeastern Australia. Contr. Miner. Petrol., 10: 189～200.
Deng Jinfu,Feng Yanfang, Di Yongjun, Liu Cui, Xiao Qinghui, Su Shangguo, Zhao Guochun, Meng Fei, Ma Shuai, Yaotu. 2015a&. Magmatic arc and ocean—continent transition: Discussion. Geological Review, 61(3):473～484.
Deng Jinfu, Liu Cui,Feng Yanfang,Xiao Qinghui,Su Shangguo,Zhao Guochun,Duan Peixin,Dai Meng.2015b&.On the correct application in the common igneous petrological diagrams: Discussion and suggestion. Geological Review,61(4):717～734.
Duan Xiaoxia, Liu Jianmin, Wang Yongbin, Zhou Lingli, Li Yonggui, Li Bin, Zhang Zhuang, Zhang Zuolun. 2012&. Geochronology, geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield, Liaoning. Acta Petrologica Sinica, 28(2): 595～606.
Frost C D, Frost B R, Chamberlain K R and Edwards B. 1999. Petrogenesis of the 1.43 Ga Sherman batholith,SE Wyoming,USA:A reduced,rapakivi-type anorogenic granite. J. Petrol., 40: 1771～1802.
Frost B R,Barnes C G,Collins W J,Arcuuius R J,Ellis D J and Frost C D. 2001.A geochemical classification for granitic rocks.Journal of Petrology,42(11):2033～2048.
Furukawa Y and Tatsumi Y.1999.Melting of a subducting slab and production of high-Mg and esite magmas:Unusual magmatism in SW Japan. Geophys. Res. Lett., 26:2271～2274.
Gao S, Ridnick R L, Xu W L, et al. 2004. Recycling lower continental crust in the North China Craton. Nature, 432: 1145～1174.
Ge Xiaoyue,Li Xianhua,Chen Zhigang,Li Wuping.2002#.Geochemistry and petrogenesis of Jurassic high Sr/low Y granitoids in eastern China:Constrains on crustal thickness.Chinese Science Bulletin,47:474～480.
Han Baofu, Kagami H and Li Huimin.2004&.Age and Nd-Sr isotopic geochemistry of the Guangtoushan alkaline granite,Hebei province,China: implications for early Mesozoic crust-mantle interaction in North China Block.Acta Petrologica Sinica,20(6):1375～1388.
Harris N B W, Marzouki F M H and Ali S.1986.The Jabel Sayid Comlex,Arabian Shield:Geochemical constraints on the origin of peralkaline and related granites. J. Geol. Soc. London, 143: 287～295.
Hofmann A W.1988.Chemical differentiation of the earth:the relationship between mantle continental crust,and oceanic crust.Earth and Planetary Science Letters,90:297～314.
Jia Xiaohui,Wang Qiang, Tang Gongjian. 2009&. A-type granites:Research progress and implications. Geotectonica et Metallogenia, 33(3):465～480.
Jia Xiaohui, Wang Xiaodi,Yang Wenqiang,Niu Zhijun.2017&.An overview of studies on shoshonitic rocks, Geological Review, 63(6):1587～1601.
Jung S and Pfnder J A.2007.Source composition and melting temperatures of orogenic graitoids:Comstrains from CaO/Na2O,Al2O3/TiO2 and accessory mineral saturation thermometry. European Journal of Mineralogy,19(6):859～870.
Kang Lei, Xiao Peixi,Gao Xiaofeng,Xi Rengang,Yang Zaichao.2016&.Chronology,geochemistry and petrogenesis of monzonitic granite and quartz diorite in Mangai area: Its inspiration to Early Paleozoic tectonic—magmatic evolution of the southern Altyn Tagh. Acta Petrologica Sinica,32(6):1731～1748.
Kamei A,Owada M,Nagao T, et al. 2004.High-Mg diorites derived from sanukitic HMA magmas, Kyushu Island, southwest Japan arc: Evidence from clinopyroxene and whole rock compositions. Lithos,75:359～371.
Li Sanzhong,Hao Defeng,Zhao Guochun,Sun Ming,Han Zongzhu,Guo Xiaoyu.2004&.Geochemical fentures and orgin of Dandong granite.Acta Petrologica Sinica, 20(6):1417～1423.
Litvinovsky B A, Jahn B M, Zanvilevich A N, Saunders A,Poulain S,Kuzmin D V,Reichow M K and Titov A V. 2002. Petrogenesis of syenite-granite suites from the Bryansky Complex (Transbaikalia,Russia):Implications for the origin of A-type granitoid magmas. Chem. Geol., 189:105～133.
Li Xinyuan,Zhao Yuanyi,Liu Chunhua.2018&. Geochronology and geochemical characteristics of igneous rocks in the Sankuanggou-Zhuanghuhe area in Heilongjiang and its implications for subduction structure and metallogeng. Acta Geologica Sinica, 92(2):244～262.
Liu Jiexun,GuoWei,Zhu Kai.2016&.Geochronology,geochemistry and geological significance of the Early Cretaceous intrusive rocks from Xiuyan area,eastern Liaoning Province. Acta Petrologica Sinica, 32(9):2889～2900.
Liu Ge,Zhu Zhixin,She Zhizhong,Deng Hongtao,Zhao Tongyang,Wang Qingjun,Sun Yaofeng.2016&.Geochronology,Geochemistry and Petrogenesis of the Zhulumute A type granites in West Junggar, Xinjinag. Geological Review,62(2):331～342.
Liu Y S, Hu Z C,Zong K Q,et al.2010&. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Chinese Science Bullein, 55(15):1535～1546.
Li Guanglai, Hua Renmin, Hu Dongquan, Huang Xiao’e, Zhang Wenlan, Wang Xudong. 2010&.Petrogenesis of Shilei quartz diorite in southern Jiangxi: Constraints from petrochemistry,trace elements of accessory minerals,zircon U-Pb dating,and Sr-Nd-Hf is otopes.Acta Petrologica Sinica,26(3):903～918.
Li Sanzhong, Hao Defeng, Zhao,Guochun, Sun Ming, Han Zongzhu, Guo Xiaoyu.2004&.Geochemical fentures and origin of Dandong granite. Acta Petrologica Sinica, 20(6):1417～1423.
Litvinovsky B A,Steele I M and Wickham S M. 2000. Silicic magma formation in overthickened crust: Melting of charnockite and leucogranite at 15, 20 and 25 kbar. J. Petrol.,41(5):717～737.
Loiselle M C and Wones D R.1979. Characteristics and origin of anorogenic granites. Geol. Soc. Am. Bull. (Abstracts with Programs), 11:468.
Maniar P D,Piccoli P M.1989.Tectonic discrimination of granitoids. GSA Bull.,101: 635～643.
Menzies M A, Fan W M and Zhang M. 1993.Palaeozoic and Cenozoic lithoprobes and the loss of 120 km of Archaean lithosphere,Sino-Korean Craton,China.In:Prichard H M, Alabaster T, Harris N B W and Neary C R. eds. Magmatic Processes and Plate Tectonics. Geological Society, London, Special Publication, 76:71～81.
Pearce J A, Harris N B W and Tindle A G.1984.Trace element discrimination diagrams for the tectonic interpretatiaon of granitic rocks. J. Petrol., 25: 956～983.
Qiu Shidong, Gu Pingyang, Pang Xinyu, Dong Zengchan, Zha Xianfeng, Zha Fangyong, Chen Ruiming, Zhuang Yujun.2015&. Zircon MC-LA-ICP-MS U-Pb dating, geochemistry and geological significance of gneissic quartz diorite in north Lenghu, Qinghai. Geological Review, 61(4):948～959.
Qin Ya,Liang Yiming,Hu Zhaochu,Feng Jian,Li Min. 2013&. Confirmatiaon of aluminous A-type granite emplacement and its tectonic significance during Early Cretaceous in the Laoling Area,South of Jilin Province. Earth Science, 38(4):677～688.
Song Yunhong, Yang Fengchao, Yan Guolei,Wei Minghui,Shi Shaoshan.2016&. SHRIMP U-Pb ages and Hf isotopic compositions of Paleoproterozoic granites from the eastern part of Liaoning Province and their tectonic significance. Acta Geologica Sinica, 90(10):2620～2636.
Rapp R P, Watson E B. 1995. Dehydration melting of metabasalt at 8～32 kbar;implications for continental growth and crust-mantle recycling. J. Petrol., 36:891～931.
Rudinick R L, Barth M, Horn I, et al.2000.Rutile-bearing refractory eclogites:Missing link between continents and depleted mantle.Science,287(5451):278～281.
Rushmer T. 1991. Partial melting of two ampbbolites. Contrib. Mineral. Petrol., 107:41 ～49.
Rickwood P C.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22( 4) : 247～263.
Taylor S R and Mclennan S M.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell,91～92.
Tvan de Flierdt T, Hoernes S,et al. 2003. Lower crustal melting and the role of open-system processes in the genesis of synorogenic diorite-granite-leucogranite associations;const raints from Sr-Nd-O isotopes from the Bandombaai complex,Namibia. Lithos, 67:205 ～226.
Wu Fuyuan,Xu Yigang,Gao Shan,Zheng Jianping.2008&. Lithospheric thinning and destruction of the North China Craton. Acta Petrologica Sinica, 24(6):1145～1174
Wu Fuyuan,Li Xianhua ,Yang Jinhui, Zheng Yongfei. 2007&.Discussions on the petrogenesis of granites. Acta Petrologica Sinica, 23(6): 1217～1238.
Wu Fuyuan,Yang Jinhui,Liu Xiaoming.2005&.Geochronological framework of the Mesozoic granitic Magmatism in the Liaodong peninsula,Northeast China. Geological Journal of China Universities,11(3): 305～317.
Wu Yuanbao,Zheng Yongfei.2004&. Zircon genetic mineralogy and its constraints on U-Pb age interpretation. Chinese Science Bulletin, 49(16):1589～1604.
Wu F Y,Sun D Y,Li X H, Jahn B M and Wilde S A.2002.A-type granites in Northeastern China:Age and geochemical constraints on their petrogenesis.Chem. Geol., 187: 143～173.
Whalen J B, Currie K L and Chappell B W. 1987.A-type granites: Geochemical characteristics,discrimination and petrogenesis. Contrib. Mineral. Petrol., 95: 529～542.
Xu Y G. 2001.Thermo-tectonic destruction of the Archean lithospheric keel beneath eastern China:evidence,thinning and, mechanism. Phys. Chem. Earth, 26: 747～757.
Yang Fengchao, Song Yunhong, Hao Libo, Chai Peng. 2015.Liaodong area three shijiazi late Jurassic SHRIMP U-Pb age and Hf iostopic characteristics of granite from Sanjiazi area in Liaodong and geological significance. Acta Geologica Sinica, 89(10):1773～1782.
Yang Jinhui,Wu Fuyuan.2009&.Triassic magmatism and its relation to decrationization in the eastern North China Craton. Sci. China Ser. D——Earth Sci., 39(7):910～921.
Yang J H, Wu F Y, Wilde S A, et al. 2007a. Petrogenesis of Late Triassic granitoids and their enclaves with implications for post-collisional lithospheric thinning of the Liaodong Penisula,North China Craton. Chem. Geol., 242(1～2):155～175.
Yang J H, Sun J F, Chen F K, et al. 2007b. Sources and petrogenesis of Late Triassic dolenite dikes in the Liaodong Peninsula: implications for post-collisional lithosphere thinning of Eastern North China Craton. J. Petrol., 48(10):1973～1997.
Yang J H, Wu F Y, Chuang S L, Wilde S A and Chu M F. 2006.A hybrid origin for the Qianshan A type granite ,northeast China:Gechemical and Sr-Nd-Hf isotopic evidence.Lithos,89: 89～106.
Yang Jinhui,Wu Fuyuan,Lo Ching-hua, Chung Sun-lin,Zhang Yanbin.2004&.Deformatiaon age of Jurassic granites in the Dandong area,eastern China: 40Ar/39Ar geochronological constrains. Acta Petrologica Sinica, 20(5):1205～1214.
Yogodzinski G M,Kay R W,Volynets O N, et al.1995. Magnesian andesite in the western Aleutian Komandorsky region:Implications for slab melting and processes in the mantle wedge. Geol. Soc, Am. Bull.,107:505～519.
Zhang Peng, Chen Dong, Kou Linlin, Zhao Yan, Yang Hongzhi,Sha Deming,Wang Xijin. 2015&. Geochronology, geochemistry and Sr-Nd-Pb isotopes of the Wolongquan intrusion in Liaodong and its geological significance. Acta Geologica Sinica, 89(10):1762～1772.
Zhang Qi, Wang Yan, Xiong Xiaolin, Li Chengdong.2008&. Adakite and Granites: Challenges and Opportunities. Beijing: China Land Press, 3～18.
Zhang Qi, Ran Baigao,Li Chengdong.2012&.A-type granite:what is the essence? Acta Petrologica et Mineralogica, 31(4):621～626.
Zhu Jinchu, Zhang Peihua, Xie Caifu, Zhanghui,Yang Ce.2006&.The Huashan-Guposhan A-type granitoid belt in the western part of the Nanling Mountains: Petrology,geochemistry and genetic interpretations. Acta Geologica Sinica, 80(4):529～542.
Zhao Zhenhua,Wang Zhonggang, Zou Tianren, Akimasa Masuda. 1996#.Discussion about the origin of rich alkali intrusive rocks in Wulungu Xinjiang. Geochemistry, 25(3):205～220.
邓晋福,冯艳芳,狄永军,刘翠,肖庆辉,苏尚国,赵国春,孟斐,马帅,姚图.2015a.岩浆弧火成岩构造组合与洋陆转换.地质论评,61(3):473～484.
邓晋福,刘翠,冯艳芳,肖庆辉,苏尚国,赵国春,段培新,戴蒙.2015b.关于火成岩常用图解的正确使用:讨论与建议.地质论评,61(4):717～734.
段晓侠,刘建明,王永彬,周伶俐,李永贵,李斌,张壮,张作伦. 2012. 辽宁青城子铅锌多金属矿田晚三叠世岩浆岩年代学、地球化学及地质意义. 岩石学报, 28(2): 595～606.
葛小月,李献华,陈志刚,李伍平.2002.中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因—对中国东部地壳厚度的制约.科学通报,47(6):474～480.
韩宝福,加加美宽雄,李惠民.2004.河北光头山碱性花岗岩的时代、Sr—Nd同位素特征及其对华北古生代壳幔相互作用的意义.岩石学报,20:1375～1388.
贾小辉,王晓地,杨文强,牛志军.2017.钾玄质系列岩石的研究现状.地质论评,63(6):1587～1601.
贾小辉,王强,唐功建.2009.A型花岗岩的研究进展及意义.大地构造与成矿学,33(3):465～480.
李光来,华仁民,胡东泉,黄小娥,张文兰,王旭东.2010.赣南地区石雷石英闪长岩的成因:岩石化学、副矿物微量元素、锆石U-Pb年代学与Sr—Nd—Hf同位素制约.岩石学报,26(3):903～918.
李三忠,郝德峰,赵国春,孙敏,韩宗珠,郭晓玉.2004.丹东花岗岩的地球化学特征及成因.岩石学报, 20(6):1417～1423.
黎心远,赵元艺,刘春花.2018.黑龙江三矿沟—庄乎河地区岩浆岩年代学、地球化学研究及其俯冲构造与成矿意义.地质学报,92(2):244～262.
刘杰勋,郭巍,朱凯.2016.辽东岫岩地区早白垩世侵入岩的年代学、地球化学及地质意义.岩石学报,32(9):2889～2900.
刘阁,朱志新,佘建忠,邓洪涛,赵同阳,王庆军,孙耀峰.2016.新疆西准噶尔朱鲁木特A型花岗岩年代学、地球化学及岩石成因.地质论评,62(2):331～342.
康磊,校培喜,高晓峰,奚仁刚,杨再朝.2016.茫崖山二长花岗岩、石英闪长岩的年代学、地球化学及岩石成因:对阿尔金南缘早古生代构造—岩浆岩化的启示.岩石学报,32(6):1731～1748.
邱士东,辜平阳,庞新愉,董增产,查显峰,查方勇,陈锐明,庄玉军.2015.青海冷湖北片麻状石英闪长岩的MC-LA-ICP-MS锆石U-Pb年龄、地球化学特征及地质意义.地质论评,61(4):948～959.
秦亚,梁一鸿,胡兆初,冯坚,李敏.2013.吉南老岭地区早白垩世铝质A型花岗岩的厘定及其构造意义.地球科学,38(4) : 677～688.
宋运红,杨凤超,闫国磊,魏明辉,石绍山.2016. 辽东地区古元古代花岗岩SHRIMP U-Pb年龄、Hf同位素组成及构造意义.地质学报,90(10):2620～2636.
吴福元,徐义刚,高山,郑建平.2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报,24(6):1145～1174.
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.
吴福元,杨进辉,柳小明.2005.辽东半岛中生代花岗质岩浆作用的年代学格架.高校地质学报,11(3):305～317.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589～1604.
吴福元,葛文春,孙德有.2002.埃达克岩的概念、识别标志及其地质意义.见:肖庆辉,邓晋福,马大铨等著.花岗岩研究思维与方法.北京:地质出版社: 172～191.
杨佳林,顾玉超,杨凤超,李东涛,鞠楠,贾宏翔.2018. 辽东半岛大金山花岗岩体SHRIMP U-Pb年龄、元素地球化学和Hf同位素特征及地质意义.地质论评,64(6):1541～1556
杨凤超,宋运红,郝立波,柴鹏.2015.辽东三家子地区晚侏罗世花岗岩SHRIMP U-Pb年龄、Hf同位素特征及地质意义.地质学报,2015,89(10):1773～1782
杨进辉,吴福元.2009.华北东部晚三叠纪岩浆作用.中国科学D辑:地球科学,39(7):910～921.
杨进辉,吴福元,罗清华,钟孙霖,张艳斌,Wilde S A. 2004. 辽宁丹东地区侏罗纪花岗岩的变形时代40Ar/39Ar年代学制约.岩石学报,20(5):1205～1214.
张朋,陈冬,寇林林,赵岩,杨宏智,沙德铭,王希今.2015. 辽东卧龙泉岩体锆石U-Pb年代学、地球化学、Sr—Nd—Pb同位素特征及其地质意义.地质学报,89(10):1762～1772.
张旗,冉白皋,李承东.2012.A型花岗岩的实质是什么?岩石矿物学杂志,31(4):621～626.
张旗,王焰,熊小林,李承东.2008.埃达克岩和花岗岩:挑战与机遇.北京:中国大地出版社,3～18.
朱金初,张佩华,谢才富,张辉,杨策.2006.南岭西段花山—姑婆山A型花岗质杂岩带:岩石学、地球化学和岩石成因.地质学报,80(4):529～542.
赵振华,王中刚,邹天人,增田彰正.1996.新疆乌伦古富碱侵入岩成因探讨.地球化学,25(3):205～220.
Barth M G,McDonough W F and Rudnick R L.2000.Tracking the budget of Nb and Ta in the continental crust.Chemical Geology,165(3～4):197～213.
Cui Weilong,Liu Zhenghong,Du Yang,Wang Shijie,Wan Le. 2016&. LA-ICP-MS zircon U-Pb dating,geochemical characteristics and geological significance of Daxing pluton in Liaodong Area. Journal of Earth Sciences and Environment, 38(5):623～637.
Creaser R A, Price R C and Wormald R J.1991.A-typr granites revisited: Assessment of a residual-source model. Geology,19:163～166.
Collins W J, Beams S D,White A J R and Chappell B W.1982. Nature and origin of A-type granites with particular reference to Southeastern Australia. Contr. Miner. Petrol., 10: 189～200.
Deng Jinfu,Feng Yanfang, Di Yongjun, Liu Cui, Xiao Qinghui, Su Shangguo, Zhao Guochun, Meng Fei, Ma Shuai, Yaotu. 2015a&. Magmatic arc and ocean—continent transition: Discussion. Geological Review, 61(3):473～484.
Deng Jinfu, Liu Cui,Feng Yanfang,Xiao Qinghui,Su Shangguo,Zhao Guochun,Duan Peixin,Dai Meng.2015b&.On the correct application in the common igneous petrological diagrams: Discussion and suggestion. Geological Review,61(4):717～734.
Duan Xiaoxia, Liu Jianmin, Wang Yongbin, Zhou Lingli, Li Yonggui, Li Bin, Zhang Zhuang, Zhang Zuolun. 2012&. Geochronology, geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield, Liaoning. Acta Petrologica Sinica, 28(2): 595～606.
Frost C D, Frost B R, Chamberlain K R and Edwards B. 1999. Petrogenesis of the 1.43 Ga Sherman batholith,SE Wyoming,USA:A reduced,rapakivi-type anorogenic granite. J. Petrol., 40: 1771～1802.
Frost B R,Barnes C G,Collins W J,Arcuuius R J,Ellis D J and Frost C D. 2001.A geochemical classification for granitic rocks.Journal of Petrology,42(11):2033～2048.
Furukawa Y and Tatsumi Y.1999.Melting of a subducting slab and production of high-Mg and esite magmas:Unusual magmatism in SW Japan. Geophys. Res. Lett., 26:2271～2274.
Gao S, Ridnick R L, Xu W L, et al. 2004. Recycling lower continental crust in the North China Craton. Nature, 432: 1145～1174.
Ge Xiaoyue,Li Xianhua,Chen Zhigang,Li Wuping.2002#.Geochemistry and petrogenesis of Jurassic high Sr/low Y granitoids in eastern China:Constrains on crustal thickness.Chinese Science Bulletin,47:474～480.
Han Baofu, Kagami H and Li Huimin.2004&.Age and Nd-Sr isotopic geochemistry of the Guangtoushan alkaline granite,Hebei province,China: implications for early Mesozoic crust-mantle interaction in North China Block.Acta Petrologica Sinica,20(6):1375～1388.
Harris N B W, Marzouki F M H and Ali S.1986.The Jabel Sayid Comlex,Arabian Shield:Geochemical constraints on the origin of peralkaline and related granites. J. Geol. Soc. London, 143: 287～295.
Hofmann A W.1988.Chemical differentiation of the earth:the relationship between mantle continental crust,and oceanic crust.Earth and Planetary Science Letters,90:297～314.
Jia Xiaohui,Wang Qiang, Tang Gongjian. 2009&. A-type granites:Research progress and implications. Geotectonica et Metallogenia, 33(3):465～480.
Jia Xiaohui, Wang Xiaodi,Yang Wenqiang,Niu Zhijun.2017&.An overview of studies on shoshonitic rocks, Geological Review, 63(6):1587～1601.
Jung S and Pfnder J A.2007.Source composition and melting temperatures of orogenic graitoids:Comstrains from CaO/Na2O,Al2O3/TiO2 and accessory mineral saturation thermometry. European Journal of Mineralogy,19(6):859～870.
Kang Lei, Xiao Peixi,Gao Xiaofeng,Xi Rengang,Yang Zaichao.2016&.Chronology,geochemistry and petrogenesis of monzonitic granite and quartz diorite in Mangai area: Its inspiration to Early Paleozoic tectonic—magmatic evolution of the southern Altyn Tagh. Acta Petrologica Sinica,32(6):1731～1748.
Kamei A,Owada M,Nagao T, et al. 2004.High-Mg diorites derived from sanukitic HMA magmas, Kyushu Island, southwest Japan arc: Evidence from clinopyroxene and whole rock compositions. Lithos,75:359～371.
Li Sanzhong,Hao Defeng,Zhao Guochun,Sun Ming,Han Zongzhu,Guo Xiaoyu.2004&.Geochemical fentures and orgin of Dandong granite.Acta Petrologica Sinica, 20(6):1417～1423.
Litvinovsky B A, Jahn B M, Zanvilevich A N, Saunders A,Poulain S,Kuzmin D V,Reichow M K and Titov A V. 2002. Petrogenesis of syenite-granite suites from the Bryansky Complex (Transbaikalia,Russia):Implications for the origin of A-type granitoid magmas. Chem. Geol., 189:105～133.
Li Xinyuan,Zhao Yuanyi,Liu Chunhua.2018&. Geochronology and geochemical characteristics of igneous rocks in the Sankuanggou-Zhuanghuhe area in Heilongjiang and its implications for subduction structure and metallogeng. Acta Geologica Sinica, 92(2):244～262.
Liu Jiexun,GuoWei,Zhu Kai.2016&.Geochronology,geochemistry and geological significance of the Early Cretaceous intrusive rocks from Xiuyan area,eastern Liaoning Province. Acta Petrologica Sinica, 32(9):2889～2900.
Liu Ge,Zhu Zhixin,She Zhizhong,Deng Hongtao,Zhao Tongyang,Wang Qingjun,Sun Yaofeng.2016&.Geochronology,Geochemistry and Petrogenesis of the Zhulumute A type granites in West Junggar, Xinjinag. Geological Review,62(2):331～342.
Liu Y S, Hu Z C,Zong K Q,et al.2010&. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS. Chinese Science Bullein, 55(15):1535～1546.
Li Guanglai, Hua Renmin, Hu Dongquan, Huang Xiao’e, Zhang Wenlan, Wang Xudong. 2010&.Petrogenesis of Shilei quartz diorite in southern Jiangxi: Constraints from petrochemistry,trace elements of accessory minerals,zircon U-Pb dating,and Sr-Nd-Hf is otopes.Acta Petrologica Sinica,26(3):903～918.
Li Sanzhong, Hao Defeng, Zhao,Guochun, Sun Ming, Han Zongzhu, Guo Xiaoyu.2004&.Geochemical fentures and origin of Dandong granite. Acta Petrologica Sinica, 20(6):1417～1423.
Litvinovsky B A,Steele I M and Wickham S M. 2000. Silicic magma formation in overthickened crust: Melting of charnockite and leucogranite at 15, 20 and 25 kbar. J. Petrol.,41(5):717～737.
Loiselle M C and Wones D R.1979. Characteristics and origin of anorogenic granites. Geol. Soc. Am. Bull. (Abstracts with Programs), 11:468.
Maniar P D,Piccoli P M.1989.Tectonic discrimination of granitoids. GSA Bull.,101: 635～643.
Menzies M A, Fan W M and Zhang M. 1993.Palaeozoic and Cenozoic lithoprobes and the loss of 120 km of Archaean lithosphere,Sino-Korean Craton,China.In:Prichard H M, Alabaster T, Harris N B W and Neary C R. eds. Magmatic Processes and Plate Tectonics. Geological Society, London, Special Publication, 76:71～81.
Pearce J A, Harris N B W and Tindle A G.1984.Trace element discrimination diagrams for the tectonic interpretatiaon of granitic rocks. J. Petrol., 25: 956～983.
Qiu Shidong, Gu Pingyang, Pang Xinyu, Dong Zengchan, Zha Xianfeng, Zha Fangyong, Chen Ruiming, Zhuang Yujun.2015&. Zircon MC-LA-ICP-MS U-Pb dating, geochemistry and geological significance of gneissic quartz diorite in north Lenghu, Qinghai. Geological Review, 61(4):948～959.
Qin Ya,Liang Yiming,Hu Zhaochu,Feng Jian,Li Min. 2013&. Confirmatiaon of aluminous A-type granite emplacement and its tectonic significance during Early Cretaceous in the Laoling Area,South of Jilin Province. Earth Science, 38(4):677～688.
Song Yunhong, Yang Fengchao, Yan Guolei,Wei Minghui,Shi Shaoshan.2016&. SHRIMP U-Pb ages and Hf isotopic compositions of Paleoproterozoic granites from the eastern part of Liaoning Province and their tectonic significance. Acta Geologica Sinica, 90(10):2620～2636.
Rapp R P, Watson E B. 1995. Dehydration melting of metabasalt at 8～32 kbar;implications for continental growth and crust-mantle recycling. J. Petrol., 36:891～931.
Rudinick R L, Barth M, Horn I, et al.2000.Rutile-bearing refractory eclogites:Missing link between continents and depleted mantle.Science,287(5451):278～281.
Rushmer T. 1991. Partial melting of two ampbbolites. Contrib. Mineral. Petrol., 107:41 ～49.
Rickwood P C.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22( 4) : 247～263.
Taylor S R and Mclennan S M.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell,91～92.
Tvan de Flierdt T, Hoernes S,et al. 2003. Lower crustal melting and the role of open-system processes in the genesis of synorogenic diorite-granite-leucogranite associations;const raints from Sr-Nd-O isotopes from the Bandombaai complex,Namibia. Lithos, 67:205 ～226.
Wu Fuyuan,Xu Yigang,Gao Shan,Zheng Jianping.2008&. Lithospheric thinning and destruction of the North China Craton. Acta Petrologica Sinica, 24(6):1145～1174
Wu Fuyuan,Li Xianhua ,Yang Jinhui, Zheng Yongfei. 2007&.Discussions on the petrogenesis of granites. Acta Petrologica Sinica, 23(6): 1217～1238.
Wu Fuyuan,Yang Jinhui,Liu Xiaoming.2005&.Geochronological framework of the Mesozoic granitic Magmatism in the Liaodong peninsula,Northeast China. Geological Journal of China Universities,11(3): 305～317.
Wu Yuanbao,Zheng Yongfei.2004&. Zircon genetic mineralogy and its constraints on U-Pb age interpretation. Chinese Science Bulletin, 49(16):1589～1604.
Wu F Y,Sun D Y,Li X H, Jahn B M and Wilde S A.2002.A-type granites in Northeastern China:Age and geochemical constraints on their petrogenesis.Chem. Geol., 187: 143～173.
Whalen J B, Currie K L and Chappell B W. 1987.A-type granites: Geochemical characteristics,discrimination and petrogenesis. Contrib. Mineral. Petrol., 95: 529～542.
Xu Y G. 2001.Thermo-tectonic destruction of the Archean lithospheric keel beneath eastern China:evidence,thinning and, mechanism. Phys. Chem. Earth, 26: 747～757.
Yang Fengchao, Song Yunhong, Hao Libo, Chai Peng. 2015.Liaodong area three shijiazi late Jurassic SHRIMP U-Pb age and Hf iostopic characteristics of granite from Sanjiazi area in Liaodong and geological significance. Acta Geologica Sinica, 89(10):1773～1782.
Yang Jinhui,Wu Fuyuan.2009&.Triassic magmatism and its relation to decrationization in the eastern North China Craton. Sci. China Ser. D——Earth Sci., 39(7):910～921.
Yang J H, Wu F Y, Wilde S A, et al. 2007a. Petrogenesis of Late Triassic granitoids and their enclaves with implications for post-collisional lithospheric thinning of the Liaodong Penisula,North China Craton. Chem. Geol., 242(1～2):155～175.
Yang J H, Sun J F, Chen F K, et al. 2007b. Sources and petrogenesis of Late Triassic dolenite dikes in the Liaodong Peninsula: implications for post-collisional lithosphere thinning of Eastern North China Craton. J. Petrol., 48(10):1973～1997.
Yang J H, Wu F Y, Chuang S L, Wilde S A and Chu M F. 2006.A hybrid origin for the Qianshan A type granite ,northeast China:Gechemical and Sr-Nd-Hf isotopic evidence.Lithos,89: 89～106.
Yang Jinhui,Wu Fuyuan,Lo Ching-hua, Chung Sun-lin,Zhang Yanbin.2004&.Deformatiaon age of Jurassic granites in the Dandong area,eastern China: 40Ar/39Ar geochronological constrains. Acta Petrologica Sinica, 20(5):1205～1214.
Yogodzinski G M,Kay R W,Volynets O N, et al.1995. Magnesian andesite in the western Aleutian Komandorsky region:Implications for slab melting and processes in the mantle wedge. Geol. Soc, Am. Bull.,107:505～519.
Zhang Peng, Chen Dong, Kou Linlin, Zhao Yan, Yang Hongzhi,Sha Deming,Wang Xijin. 2015&. Geochronology, geochemistry and Sr-Nd-Pb isotopes of the Wolongquan intrusion in Liaodong and its geological significance. Acta Geologica Sinica, 89(10):1762～1772.
Zhang Qi, Wang Yan, Xiong Xiaolin, Li Chengdong.2008&. Adakite and Granites: Challenges and Opportunities. Beijing: China Land Press, 3～18.
Zhang Qi, Ran Baigao,Li Chengdong.2012&.A-type granite:what is the essence? Acta Petrologica et Mineralogica, 31(4):621～626.
Zhu Jinchu, Zhang Peihua, Xie Caifu, Zhanghui,Yang Ce.2006&.The Huashan-Guposhan A-type granitoid belt in the western part of the Nanling Mountains: Petrology,geochemistry and genetic interpretations. Acta Geologica Sinica, 80(4):529～542.
Zhao Zhenhua,Wang Zhonggang, Zou Tianren, Akimasa Masuda. 1996#.Discussion about the origin of rich alkali intrusive rocks in Wulungu Xinjiang. Geochemistry, 25(3):205～220.