辽东岫岩北部王家堡子一带富铝片麻岩的变质作用及其地质意义
|
摘要
高级变质富铝片麻岩出露于辽东岫岩北部王家堡子一带南辽河岩群变质岩石中,通过详细的岩相学和变质作用研究,确定其变质峰期典型矿物组合为Sil+Grt+Crd+Bt+Pl+Kfs+Qz;峰期后存在典型的减压反应Grt+Sil+Qz→Crd。早期进变质阶段以出现十字石、蓝晶石为特征,晚期退变质阶段以石榴石变斑晶和黑云母转变为绿泥石为特征。传统地质温压计估算的富铝片麻岩峰期变质条件为:T=640℃～690℃,P=5. 5～7. 0 kbar;峰期后减压阶段变质条件为:T=560℃～660℃,P=4. 7～4. 9kbar;晚期退变质条件为:T=520℃～560℃,P=2. 9～3. 0 kbar。矿物组合特征、矿物相转变结构及其温压条件变化反映其具有近等温减压的顺时针P--T轨迹演化特征,不同于前人所获得的逆时针P--T轨迹。研究结果认为南、北辽河岩群在古元古代可能经历了相同的变质作用演化过程。
The study on petrography and metamorphism of aluminum-rich gneiss occurred in South Liaohe Group in Wangjiapuzi of northern Xiuyan area,East Liaoning has been carried out. The peak mineral assemblage consists of garnet + sillimanite + cordierite + biotite + plagioclase + k-feldspar + quartz,and there is a typical decompression reaction of garnet + sillimanite + quartz→cordierite after peak stage. Early prograde metamorphic stage is characterized by the occurrence of staurolite and kyanite,whereas the late retrograde metamorphic stage is characterized by the transformation of garnet and biotite into chlorite. Traditional P--T estimation suggests that the metamorphic conditions for peak stage are 640℃ ～ 690℃ and 5. 5 ～ 7. 0 kbar of aluminum-rich gneiss,560℃ ～ 660℃and 4. 7 ～ 4. 9 kbar for post-peak near-isothermal decompression stage,and 520℃ ～ 560℃ and 2. 9 ～ 3. 0 kbar for late retrograde metamorphic stage. The characteristics of mineral assemblage,transition structure of mineral phase and P--T conditions of aluminum-rich gneiss indicate a clockwise P-T path with near isothermal decompression,which is different from the counterclockwise P--T path obtained by predecessors. The results show that South Liaohe Group and North Liaohe Group probably underwent the same metamorphic evolution process in Paleoproterozoic.
The study on petrography and metamorphism of aluminum-rich gneiss occurred in South Liaohe Group in Wangjiapuzi of northern Xiuyan area,East Liaoning has been carried out. The peak mineral assemblage consists of garnet + sillimanite + cordierite + biotite + plagioclase + k-feldspar + quartz,and there is a typical decompression reaction of garnet + sillimanite + quartz→cordierite after peak stage. Early prograde metamorphic stage is characterized by the occurrence of staurolite and kyanite,whereas the late retrograde metamorphic stage is characterized by the transformation of garnet and biotite into chlorite. Traditional P--T estimation suggests that the metamorphic conditions for peak stage are 640℃ ～ 690℃ and 5. 5 ～ 7. 0 kbar of aluminum-rich gneiss,560℃ ～ 660℃and 4. 7 ～ 4. 9 kbar for post-peak near-isothermal decompression stage,and 520℃ ～ 560℃ and 2. 9 ～ 3. 0 kbar for late retrograde metamorphic stage. The characteristics of mineral assemblage,transition structure of mineral phase and P--T conditions of aluminum-rich gneiss indicate a clockwise P-T path with near isothermal decompression,which is different from the counterclockwise P--T path obtained by predecessors. The results show that South Liaohe Group and North Liaohe Group probably underwent the same metamorphic evolution process in Paleoproterozoic.
引文
[1]Li S Z,Zhao G C,Sun M,et al.Deformation history of the Paleoproterozoic Liaohe assemblage in the eastern block of the North China Craton[J].Journal of Asian Earth Sciences,2005,24(5):659-674．
[2]Li S Z,Zhao G C,Santosh M,et al.Paleoproterozoic structural evolution of the southern segment of the JiaoLiao--Ji belt,North China Craton[J].Precambrian Research,2012,200-203(4):59-73．
[3]辽宁省地质矿产局．辽宁省区域地质志[M]．北京:地质出版社，1989:48-54,614-639.Bureau of Geology and Mineral Resources of Liaoning Province.Regional geology of Liaoning Province[M].Beijing:Geological Publishing House,1989:48-54,614-639．
[4]郭洪方，王忠江，仲米山，等．辽河群的变形作用和变质作用[J]．西北地质，2016,49(1):68-81.GUO Hong-fang,WANG Zhong-jiang,ZHONG Mi-shan,et al.Deformation and metamorphism of Liaohe Group[J].Northwestern Geology,2016,49(1):68-81．
[5]田忠华，刘福来，许王，等．构造变形在变质岩专题填图中的作用及其意义:以辽南辽河群试点填图为例[J]．地质通报，2017,36(11):1942-1952.TIAN Zhong-hua,LIU Fu-lai,XU Wang,et al.The role and significance of structural deformation in metamorphicrock mapping:a case study of the Liaohe Group mapping in central segment of Jiao-Liao-Ji orogenic belt[J].Geological Bulletin of China,2017,36(11):1942-1952．
[6]Luo Y,Sun M,Zhao G C,et al.A comparison of U--Pb and Hf isotopic compositions of detrital zircons from the North and South Liaohe Groups:constraints on the evolution of the Jiao--Liao--Ji belt North China Craton[J].Precambrian Research,2008,163(3/4):279-306．
[7]Zhao G,Cawood P,Wilde S,et al.Amalgamation of the North China Craton:key issues and discussion[J].Precambrian Research,2012,222-223(12):55-76．
[8]刘福来，刘平华，王舫，等．胶-辽-吉古元古代造山/活动带巨量变沉积岩系的研究进展[J]．岩石学报，2015,31(10):2816-2846.LIU Fu-lai,LIU Ping-hua,WANG Fang,et al.Progresses and overviews of voluminous meta-sedimentary series within the Paleoproterozoic Jiao--Liao--Ji orogenic/mobile belt,North China Craton[J].Acta Petrologica Sinica,2015,31(10):2816-2846．
[9]李壮，陈斌，刘经纬，等．辽东半岛南辽河群锆石U-Pb年代学及其地质意义[J]．岩石学报，2015,31(6):1589-1605.LI Zhuang,CHEN Bin,LIU Jing-wei,et al.U--Pb geochronology of the Nanliaohe Group in the Liaodong peninsula and its geological significance[J].Acta Petrologica Sinica,2015,31(6):1589-1605．
[10]高铂森，董永胜，李富强，等．辽东黄花甸地区南辽河群里尔峪组成因研究[J]．岩石学报，2017,33(9):2725-2742.GAO Bo-sen,DONG Yong-sheng,LI Fu-qiang,et al.Petrogenesis of the Lieryu Formation of the South Liaohe Group in the Huanghuadian area,Liaodong Peninsula[J].Acta Petrologica Sinica,2017,33(9):2725-2742．
[11]王鹏森，董永胜，李富强，等．辽东黄花甸地区古元古代花岗质岩浆及其地质意义[J]．岩石学报，2017,33(9):2708-2724.WANG Peng-sen,DONG Yong-sheng,LI Fu-qiang,et al.Geological significance in Huanghuadian area eastern Liaoning Province[J].Acta Petrologica Sinica,2017,33(9):2708-2724．
[12]王舫，刘建辉，刘超辉．辽南三家子地区南辽河群里尔峪组变沉积岩中碎屑锆石U-Pb年代学研究[J]．岩石学报，2017,33(9):2785-2791.WANG Fang,LIU Jian-hui,LIU Chao-hui,et al.Detrital zircon U--Pb geochronology of metasedimentary rocks from the Li'eryu Formation of the South Liaohe Group in Sanjiazi area,the South Liaoning Province[J].Acta Petrologica Sinica,2017,33(9):2785-2791．
[13]Yin A,Nie S.A Phanerozoic palinspastic reconstruction of China and its neighboring regions[C]//Yin A,Harrison T M.The tectonic evolution of Asia.New York:Cambridge University Press,1996:285-442．
[14]王惠初，任云伟，陆松年，等．辽吉古元古代造山带的地层单元划分构造属性[J]．地球学报，2015,36(5):1-16.WANG Hui-chu,REN Yun-wei,LU Song-nian,et al.Stratigraphic units and tectonic setting of the Paleoproterozoic Liao--Ji orogen[J].Acta Geoscientica Sinica,2015,36(5):1-16．
[15]吴福元，李秋立，杨正赫，等．朝鲜北部狼林地块构造归属与地壳形成时代[J]．岩石学报，2016,32(10):2933-2947.WU Fu-yuan,LI Qiu-li,YANG Zheng-he,et al.Crustal growth and evolution of the Rangnim Massif,northern Korean Peninsula[J].Acta Petrologica Sinica,2016,32(10):2933-2947．
[16]许王，刘福来，刘超辉．胶-辽-吉造山带北辽河变基性岩的成因、地球化学属性及其构造意义[J]．岩石学报，2017,33(9):2743-2757.XU Wang,LIU Fu-lai,LIU Chao-hui.Petrogenesis and geochemical characteristics of the North Liaohemetabasic rocks,Jiao-Liao-Ji orogenic belt and their tectonic significance[J].Acta Petrologica Sinica,2017,33(9):2743-2757．
[17]贺高品，叶惠文．辽东-吉南地区早元古代两种类型变质作用及其构造意义[J]．岩石学报，1998,14(2):152-162.HE Gao-pin,YE Hui-wen.Two types of Early Proterozoic metamorphism and its tectonic significance in eastern Liaoning and southern Jilin areas[J].Acta Petrologica Sinica,1998,14(2):152-162．
[18]李三忠，韩宗珠，刘永江，等．辽河群区域变质特征及其大陆动力学意义[J]．地质论评，2001,47(1):9-18.LI San-zhong,HAN Zong-zhu,LIU Yong-jiang,et al.Continental dynamics and regional metamorphism of the Liaohe Group[J].Geology Review,2001,47(1):9-18．
[19]Zhao G C,Wilde S A,Cawood P A,et al.Archean blocks and their boundaries in the North China Craton:lithological,geochemical,structural and P--T path constraints and tectonic evolution[J].Precambrian Research,2001,107(1/2):45-73．
[20]Zhao G C,Sun M,Wilde S A,et al.Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited[J].Precambrian Research,2005,136(2):177-202．
[21]卢良兆，徐学纯，刘福来．中国北方早前寒武纪孔兹岩系[M]．长春:长春出版社，1996:195-234.LU Liang-zhao,XU Xue-chun,LIU Fu-lai.Early Precambrian khondalite series in North China[M].Changchun:Changchun Publishing House,1996:195-234．
[22]Aydin F,Karsli O,Sadiklar M B.Mineralogy and chemistry of biotites from eastern pontide granitoid rocks,NE-Turkey:some petrological implications for granitoid magmas[J].Chemie der Erde-Geochemistry,2003,63 63(2):163-182．
[23]张翠光，魏春景．中-低压泥质岩在KFMASH体系中的相平衡关系[J]．岩石学报，2004,20(3):725-736.ZHANG Cui-guang,WEI Chun-jing.Phase equilibria for metapelites in the system K2O-FeO-Mg-Al2O3-Si O2-H2O(KFMASH)[J].Acta Petrologica Sinica,2004,20(3):725-736．
[24]Thompson A B.Mineral reactions in pelitic rocks II.calculation of some P-T-X(Fe-Mg)phase.American relations[J].Journal of Science,1976,276(4):425-454．
[25]Holdaway M J,Lee S M.Fe--Mg cordierite stability in high-grade pelitic rocks based on experimental,theoretical natural observations[J].Contributions to Mineralogy and Petrology,1977,63(2):175-198．
[26]Ferry J M,Spear F S.Experimental calibration of the partitioning of Fe and Mg between biotite and garnet[J].Contributions to Mineralogy and Petrology,1978,66(2):113-117．
[27]Hodges K V,Spear F S.Geothermometry,geobarometry and the Al2Si O5triple point at Mt.Moosilauke,New Hampshire[J].American Mineralogist,1982,67(11):1118-1134．
[28]Perchuk L L.Precambrian granulites of the Aldan shield,eastern Siberia,USSR[J].Journal of Metamorphic Geology,1985,3(3):265-310．
[29]Hodges K V,Crowley P D.Error estimation and empirical geothermobarometry for politic systems[J].American Mineralogist,1985,72(3),671-680．
[30]Koziol A M,Newton R C.Redetermination of the anorthite breakdown reaction and improvement of the plagioclase-garnet-Al2Si O5-quartz geobarometer[J].America Mineral,1988,73(1):10-30
[31]Koziol A M,Newton R C.Grossular activity-composition relationships in ternary garnets determined by reversed displaced-equilibrium experiments[J].Contributions to Mineralogy and Petrology,1989,103(4):423-433．
[32]Bhattacharya A,Mazumdar A C,Sen S K.Fe--Mg mixing in cordierite;constraints from natural data and implications for cordierite-garnet geothermometry in granulites[J].American Mineralogist,1988,73(3):338-344．
[33]Wu C M,Zhang J,Ren L D.Empirical garnet-biotiteplagioclase-quartz(GBPQ)geobarometry in medium to high-grade metapelites[J].Journal of Petrology,2004,45(9):1907-1921．
[34]Hyndman D W.Petrology of igneous and metamorphic rocks[M].New York:McGraw-Hill,1985:234-236．
[35]张秋生，杨振升．辽东半岛早期地壳与矿床[M]．北京:地质出版，1988:218-450.ZHANG Qiu-sheng,YANG Zhen-sheng.Early crustal and deposit in Liaodong Peninsula[M].Beijing:Geological Publishing House,1988:218-450．
[36]姜春潮．辽吉东部前寒武纪地质[M]．沈阳:辽宁科学技术出版社，1987:184-255.JIANG Chun-chao.Precambrian geology in eastern Liaoning and Jilin provinces[M].Shenyang:Liaoning Science and Technology Press,1987:184-255．
[37]陈荣度，李显东，张福生，等．对辽东古元古代地质若干问题的讨论[J]．中国地质，2003,30(2):207-213.CHEN Rong-du,LI Xian-dong,ZHANG Fu-sheng,et al.Several problems about the Paleoproterozoic geology of eastern Liaodong[J].Geology in China,2003,30(2):207-213．
[38]白瑾．华北陆台北缘前寒武纪地质及铅锌成矿作用[M]．北京:地质出版社，1993:212-225.BAI Jin.Precambrian geology and lead-zinc mineralization in the northern margin of North China platform[M].Beijing:Geological Publishing House,1993:212-225．
[39]贺高品，叶慧文．辽东-吉南地区早元古代变质地体的组成及主要特征[J]．长春科技大学学报，1998:121-126,134.HE Gao-pin,YE Hui-wen.The composition of the Early Proterozoie metamorphic terrains in eastern Liaoningwestern Jilin area and its main characteristics[J].Journal of Changchun University of Science and Technology,1998,28(2):121-126,134．
[40]Binns R A.Ferromagnesian minerals in high-grade metamorphic rocks[J].Geological Society of Australia Bulletin,1969,30(2):323-332．
[41]陈斌，李壮，王家林，等．辽东半岛~2.2 Ga岩浆事件及其地质意义[J]．吉林大学学报(地球科学版)，2016,46(2):303-320.CHEN Bin,LI Zhuang,WANG Jia-lin,et al.Liaodong penisula~2.2 Ga magmatic event and its geological significance[J].Journal of Jilin University(Earth Science Edition),2016,46(2):303-320．
[42]刘平华，蔡佳，邹雷．辽东半岛北部三家子石榴斜长角闪岩变质演化PTt轨迹及其地质意义:来自相衡模拟与锆石U-Pb定年的约束[J]．岩石学报，2017,33(9):2649-2674.LIU Ping-hua,CAI Jia,ZOU Lei.Metamorphic P--T--t path and its geological implication of the Sanjiazi garnet amphibolites from the northern Liaodong penisula,Jiao--Liao-Ji belt:constraints on phase equilibria and zircon U--Pb dating[J].Acta Petrologica Sinica,2017,33(9):2649-2674．
[43]李修亮．吉林通化地区集安群变质演化与成因研究:硕士学位论文[D]．北京:中国地质大学，2016.LI Xiu-liang.Metamorphic evolution and genesis of the Ji'an group in the Tonghua region Jilin Province:master's degree thesis[D].Beijing:China University of Geoscience,2016．
[44]蔡佳，刘福来，刘平华．胶-辽-吉带吉林南部地区集安群泥质麻粒岩变质作用与年代学研究[C]//2017中国地球科学联合学术年会论文集，2017.CAI Jia,LIU Fu-lai,LIU Ping-hua.Metamorphism and chronology of argillaceous granulite of Ji'an Group in southern Jilin,Jiao--Liao--Jilin belt[C]//Papers Collection of the 2017 China Geosciences Joint Academic Annual Meeting,2017．
[45]Lu X P,Wu F Y,Guo J H,et al.Zircon U--Pb geochronological constraints on the paleoproterozoic crustal evolution of the eastern block in the North China Craton[J].Precambrian Research,2006,146(3/4):138-164.
[2]Li S Z,Zhao G C,Santosh M,et al.Paleoproterozoic structural evolution of the southern segment of the JiaoLiao--Ji belt,North China Craton[J].Precambrian Research,2012,200-203(4):59-73．
[3]辽宁省地质矿产局．辽宁省区域地质志[M]．北京:地质出版社，1989:48-54,614-639.Bureau of Geology and Mineral Resources of Liaoning Province.Regional geology of Liaoning Province[M].Beijing:Geological Publishing House,1989:48-54,614-639．
[4]郭洪方，王忠江，仲米山，等．辽河群的变形作用和变质作用[J]．西北地质，2016,49(1):68-81.GUO Hong-fang,WANG Zhong-jiang,ZHONG Mi-shan,et al.Deformation and metamorphism of Liaohe Group[J].Northwestern Geology,2016,49(1):68-81．
[5]田忠华，刘福来，许王，等．构造变形在变质岩专题填图中的作用及其意义:以辽南辽河群试点填图为例[J]．地质通报，2017,36(11):1942-1952.TIAN Zhong-hua,LIU Fu-lai,XU Wang,et al.The role and significance of structural deformation in metamorphicrock mapping:a case study of the Liaohe Group mapping in central segment of Jiao-Liao-Ji orogenic belt[J].Geological Bulletin of China,2017,36(11):1942-1952．
[6]Luo Y,Sun M,Zhao G C,et al.A comparison of U--Pb and Hf isotopic compositions of detrital zircons from the North and South Liaohe Groups:constraints on the evolution of the Jiao--Liao--Ji belt North China Craton[J].Precambrian Research,2008,163(3/4):279-306．
[7]Zhao G,Cawood P,Wilde S,et al.Amalgamation of the North China Craton:key issues and discussion[J].Precambrian Research,2012,222-223(12):55-76．
[8]刘福来，刘平华，王舫，等．胶-辽-吉古元古代造山/活动带巨量变沉积岩系的研究进展[J]．岩石学报，2015,31(10):2816-2846.LIU Fu-lai,LIU Ping-hua,WANG Fang,et al.Progresses and overviews of voluminous meta-sedimentary series within the Paleoproterozoic Jiao--Liao--Ji orogenic/mobile belt,North China Craton[J].Acta Petrologica Sinica,2015,31(10):2816-2846．
[9]李壮，陈斌，刘经纬，等．辽东半岛南辽河群锆石U-Pb年代学及其地质意义[J]．岩石学报，2015,31(6):1589-1605.LI Zhuang,CHEN Bin,LIU Jing-wei,et al.U--Pb geochronology of the Nanliaohe Group in the Liaodong peninsula and its geological significance[J].Acta Petrologica Sinica,2015,31(6):1589-1605．
[10]高铂森，董永胜，李富强，等．辽东黄花甸地区南辽河群里尔峪组成因研究[J]．岩石学报，2017,33(9):2725-2742.GAO Bo-sen,DONG Yong-sheng,LI Fu-qiang,et al.Petrogenesis of the Lieryu Formation of the South Liaohe Group in the Huanghuadian area,Liaodong Peninsula[J].Acta Petrologica Sinica,2017,33(9):2725-2742．
[11]王鹏森，董永胜，李富强，等．辽东黄花甸地区古元古代花岗质岩浆及其地质意义[J]．岩石学报，2017,33(9):2708-2724.WANG Peng-sen,DONG Yong-sheng,LI Fu-qiang,et al.Geological significance in Huanghuadian area eastern Liaoning Province[J].Acta Petrologica Sinica,2017,33(9):2708-2724．
[12]王舫，刘建辉，刘超辉．辽南三家子地区南辽河群里尔峪组变沉积岩中碎屑锆石U-Pb年代学研究[J]．岩石学报，2017,33(9):2785-2791.WANG Fang,LIU Jian-hui,LIU Chao-hui,et al.Detrital zircon U--Pb geochronology of metasedimentary rocks from the Li'eryu Formation of the South Liaohe Group in Sanjiazi area,the South Liaoning Province[J].Acta Petrologica Sinica,2017,33(9):2785-2791．
[13]Yin A,Nie S.A Phanerozoic palinspastic reconstruction of China and its neighboring regions[C]//Yin A,Harrison T M.The tectonic evolution of Asia.New York:Cambridge University Press,1996:285-442．
[14]王惠初，任云伟，陆松年，等．辽吉古元古代造山带的地层单元划分构造属性[J]．地球学报，2015,36(5):1-16.WANG Hui-chu,REN Yun-wei,LU Song-nian,et al.Stratigraphic units and tectonic setting of the Paleoproterozoic Liao--Ji orogen[J].Acta Geoscientica Sinica,2015,36(5):1-16．
[15]吴福元，李秋立，杨正赫，等．朝鲜北部狼林地块构造归属与地壳形成时代[J]．岩石学报，2016,32(10):2933-2947.WU Fu-yuan,LI Qiu-li,YANG Zheng-he,et al.Crustal growth and evolution of the Rangnim Massif,northern Korean Peninsula[J].Acta Petrologica Sinica,2016,32(10):2933-2947．
[16]许王，刘福来，刘超辉．胶-辽-吉造山带北辽河变基性岩的成因、地球化学属性及其构造意义[J]．岩石学报，2017,33(9):2743-2757.XU Wang,LIU Fu-lai,LIU Chao-hui.Petrogenesis and geochemical characteristics of the North Liaohemetabasic rocks,Jiao-Liao-Ji orogenic belt and their tectonic significance[J].Acta Petrologica Sinica,2017,33(9):2743-2757．
[17]贺高品，叶惠文．辽东-吉南地区早元古代两种类型变质作用及其构造意义[J]．岩石学报，1998,14(2):152-162.HE Gao-pin,YE Hui-wen.Two types of Early Proterozoic metamorphism and its tectonic significance in eastern Liaoning and southern Jilin areas[J].Acta Petrologica Sinica,1998,14(2):152-162．
[18]李三忠，韩宗珠，刘永江，等．辽河群区域变质特征及其大陆动力学意义[J]．地质论评，2001,47(1):9-18.LI San-zhong,HAN Zong-zhu,LIU Yong-jiang,et al.Continental dynamics and regional metamorphism of the Liaohe Group[J].Geology Review,2001,47(1):9-18．
[19]Zhao G C,Wilde S A,Cawood P A,et al.Archean blocks and their boundaries in the North China Craton:lithological,geochemical,structural and P--T path constraints and tectonic evolution[J].Precambrian Research,2001,107(1/2):45-73．
[20]Zhao G C,Sun M,Wilde S A,et al.Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited[J].Precambrian Research,2005,136(2):177-202．
[21]卢良兆，徐学纯，刘福来．中国北方早前寒武纪孔兹岩系[M]．长春:长春出版社，1996:195-234.LU Liang-zhao,XU Xue-chun,LIU Fu-lai.Early Precambrian khondalite series in North China[M].Changchun:Changchun Publishing House,1996:195-234．
[22]Aydin F,Karsli O,Sadiklar M B.Mineralogy and chemistry of biotites from eastern pontide granitoid rocks,NE-Turkey:some petrological implications for granitoid magmas[J].Chemie der Erde-Geochemistry,2003,63 63(2):163-182．
[23]张翠光，魏春景．中-低压泥质岩在KFMASH体系中的相平衡关系[J]．岩石学报，2004,20(3):725-736.ZHANG Cui-guang,WEI Chun-jing.Phase equilibria for metapelites in the system K2O-FeO-Mg-Al2O3-Si O2-H2O(KFMASH)[J].Acta Petrologica Sinica,2004,20(3):725-736．
[24]Thompson A B.Mineral reactions in pelitic rocks II.calculation of some P-T-X(Fe-Mg)phase.American relations[J].Journal of Science,1976,276(4):425-454．
[25]Holdaway M J,Lee S M.Fe--Mg cordierite stability in high-grade pelitic rocks based on experimental,theoretical natural observations[J].Contributions to Mineralogy and Petrology,1977,63(2):175-198．
[26]Ferry J M,Spear F S.Experimental calibration of the partitioning of Fe and Mg between biotite and garnet[J].Contributions to Mineralogy and Petrology,1978,66(2):113-117．
[27]Hodges K V,Spear F S.Geothermometry,geobarometry and the Al2Si O5triple point at Mt.Moosilauke,New Hampshire[J].American Mineralogist,1982,67(11):1118-1134．
[28]Perchuk L L.Precambrian granulites of the Aldan shield,eastern Siberia,USSR[J].Journal of Metamorphic Geology,1985,3(3):265-310．
[29]Hodges K V,Crowley P D.Error estimation and empirical geothermobarometry for politic systems[J].American Mineralogist,1985,72(3),671-680．
[30]Koziol A M,Newton R C.Redetermination of the anorthite breakdown reaction and improvement of the plagioclase-garnet-Al2Si O5-quartz geobarometer[J].America Mineral,1988,73(1):10-30
[31]Koziol A M,Newton R C.Grossular activity-composition relationships in ternary garnets determined by reversed displaced-equilibrium experiments[J].Contributions to Mineralogy and Petrology,1989,103(4):423-433．
[32]Bhattacharya A,Mazumdar A C,Sen S K.Fe--Mg mixing in cordierite;constraints from natural data and implications for cordierite-garnet geothermometry in granulites[J].American Mineralogist,1988,73(3):338-344．
[33]Wu C M,Zhang J,Ren L D.Empirical garnet-biotiteplagioclase-quartz(GBPQ)geobarometry in medium to high-grade metapelites[J].Journal of Petrology,2004,45(9):1907-1921．
[34]Hyndman D W.Petrology of igneous and metamorphic rocks[M].New York:McGraw-Hill,1985:234-236．
[35]张秋生，杨振升．辽东半岛早期地壳与矿床[M]．北京:地质出版，1988:218-450.ZHANG Qiu-sheng,YANG Zhen-sheng.Early crustal and deposit in Liaodong Peninsula[M].Beijing:Geological Publishing House,1988:218-450．
[36]姜春潮．辽吉东部前寒武纪地质[M]．沈阳:辽宁科学技术出版社，1987:184-255.JIANG Chun-chao.Precambrian geology in eastern Liaoning and Jilin provinces[M].Shenyang:Liaoning Science and Technology Press,1987:184-255．
[37]陈荣度，李显东，张福生，等．对辽东古元古代地质若干问题的讨论[J]．中国地质，2003,30(2):207-213.CHEN Rong-du,LI Xian-dong,ZHANG Fu-sheng,et al.Several problems about the Paleoproterozoic geology of eastern Liaodong[J].Geology in China,2003,30(2):207-213．
[38]白瑾．华北陆台北缘前寒武纪地质及铅锌成矿作用[M]．北京:地质出版社，1993:212-225.BAI Jin.Precambrian geology and lead-zinc mineralization in the northern margin of North China platform[M].Beijing:Geological Publishing House,1993:212-225．
[39]贺高品，叶慧文．辽东-吉南地区早元古代变质地体的组成及主要特征[J]．长春科技大学学报，1998:121-126,134.HE Gao-pin,YE Hui-wen.The composition of the Early Proterozoie metamorphic terrains in eastern Liaoningwestern Jilin area and its main characteristics[J].Journal of Changchun University of Science and Technology,1998,28(2):121-126,134．
[40]Binns R A.Ferromagnesian minerals in high-grade metamorphic rocks[J].Geological Society of Australia Bulletin,1969,30(2):323-332．
[41]陈斌，李壮，王家林，等．辽东半岛~2.2 Ga岩浆事件及其地质意义[J]．吉林大学学报(地球科学版)，2016,46(2):303-320.CHEN Bin,LI Zhuang,WANG Jia-lin,et al.Liaodong penisula~2.2 Ga magmatic event and its geological significance[J].Journal of Jilin University(Earth Science Edition),2016,46(2):303-320．
[42]刘平华，蔡佳，邹雷．辽东半岛北部三家子石榴斜长角闪岩变质演化PTt轨迹及其地质意义:来自相衡模拟与锆石U-Pb定年的约束[J]．岩石学报，2017,33(9):2649-2674.LIU Ping-hua,CAI Jia,ZOU Lei.Metamorphic P--T--t path and its geological implication of the Sanjiazi garnet amphibolites from the northern Liaodong penisula,Jiao--Liao-Ji belt:constraints on phase equilibria and zircon U--Pb dating[J].Acta Petrologica Sinica,2017,33(9):2649-2674．
[43]李修亮．吉林通化地区集安群变质演化与成因研究:硕士学位论文[D]．北京:中国地质大学，2016.LI Xiu-liang.Metamorphic evolution and genesis of the Ji'an group in the Tonghua region Jilin Province:master's degree thesis[D].Beijing:China University of Geoscience,2016．
[44]蔡佳，刘福来，刘平华．胶-辽-吉带吉林南部地区集安群泥质麻粒岩变质作用与年代学研究[C]//2017中国地球科学联合学术年会论文集，2017.CAI Jia,LIU Fu-lai,LIU Ping-hua.Metamorphism and chronology of argillaceous granulite of Ji'an Group in southern Jilin,Jiao--Liao--Jilin belt[C]//Papers Collection of the 2017 China Geosciences Joint Academic Annual Meeting,2017．
[45]Lu X P,Wu F Y,Guo J H,et al.Zircon U--Pb geochronological constraints on the paleoproterozoic crustal evolution of the eastern block in the North China Craton[J].Precambrian Research,2006,146(3/4):138-164.