北淮阳变质单元中“浅变质”带——佛子岭群主期变质条件和碎屑锆石年代学探究
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摘要
佛子岭群为北淮阳变质单元的重要组成部分,其位于大别碰撞造山带最北缘,处于扬子和华北板块的结合部位,构造位置极为关键。长期以来,佛子岭群一直被视为扬子板块北缘沉积产物,并以加积楔形式产出。然而,随着年代学和构造地质学的研究的深入,对其构造归属和形成动力学机制产生了差异性认识,究其原因主要是对佛子岭群变质属性缺乏准确的判定所致。为此,本研究对佛子岭群展开了详细的野外观测和区域变质岩石学研究,以及岩相学、热力学和年代学分析。研究表明佛子岭群构成较为复杂,主体由细粒的云母石英片岩、石英云母片岩和石榴云母片岩构成。主期变质PT条件评价显示,其温压范围为610～620℃和0. 9～1. 0GPa,普遍经历了中-高压角闪岩相变质,并非为"浅"变质产物,并卷入了较深层次的俯冲-折返过程。锆石U-Pb年代学研究表明,佛子岭群年龄跨度较大,范围为3101±48Ma～413±9Ma,可分为5组年龄,年龄峰值分别为2537Ma、1567Ma、940Ma、749Ma和440Ma,显示了华北和扬子板块混合物源特征,最年轻的年龄峰值暗示其形成于早古生代晚期。
The Foziling Group( FZG) is an important component of the Beihuaiyang metamorphic unit in the northernmost margin of the Dabie collisional orogenic belt,and is located in the crucial position between the Yangtze and North China plates. For a long time,the FZG has been regarded as the sedimentary product of the northern margin of the Yangtze Plate as an accretionary wedge. However,the disputes on the tectonic attribute and dynamic formation mechanism of the FZG are incessancy due to the different viewpoints from studies of its geochronology and structural geology. The reason for this situation lies on the lack of the accurate appraise for the metamorphic attribution of the FZG. In this study,detailed fieldworks and regional metamorphic investigations on the FZG,together with abundant analysis of its metamorphic petrology,thermodynamic characteristics and geochronological dating have been carried out.The result indicates that the FZG is mainly lithologically composed of fine-grained mica-quartz schists,quartz-mica schists and garnetmica schists. The estimates of the main metamorphic P-T conditions of the FZG show that it has metamorphosed in a middle-high pressure amphibolite facies with a P-T range of 610 ～ 620℃ and 0. 9 ～ 1. 0 GPa,respectively,and it should not be the‘lower'-grade metamorphic unit. which demonstrates that the FZG might be involved into the process of subduction and exhumation in the deeper level. On the basis of zircon U-Pb dating,a large age range of 3101 ± 48 Ma ～ 413 ± 9 Ma has been gained for the FZG,which can be divided into 5 groups with the peak age values of 2537 Ma,1567 Ma,940 Ma,749 Ma and 440 Ma,respectively. These peak ages imply that the FZG has a mixture source from North China and Yangtze plates,and the youngest peak age suggests that the FZG has been formed in late Early Paleozoic.
The Foziling Group( FZG) is an important component of the Beihuaiyang metamorphic unit in the northernmost margin of the Dabie collisional orogenic belt,and is located in the crucial position between the Yangtze and North China plates. For a long time,the FZG has been regarded as the sedimentary product of the northern margin of the Yangtze Plate as an accretionary wedge. However,the disputes on the tectonic attribute and dynamic formation mechanism of the FZG are incessancy due to the different viewpoints from studies of its geochronology and structural geology. The reason for this situation lies on the lack of the accurate appraise for the metamorphic attribution of the FZG. In this study,detailed fieldworks and regional metamorphic investigations on the FZG,together with abundant analysis of its metamorphic petrology,thermodynamic characteristics and geochronological dating have been carried out.The result indicates that the FZG is mainly lithologically composed of fine-grained mica-quartz schists,quartz-mica schists and garnetmica schists. The estimates of the main metamorphic P-T conditions of the FZG show that it has metamorphosed in a middle-high pressure amphibolite facies with a P-T range of 610 ～ 620℃ and 0. 9 ～ 1. 0 GPa,respectively,and it should not be the‘lower'-grade metamorphic unit. which demonstrates that the FZG might be involved into the process of subduction and exhumation in the deeper level. On the basis of zircon U-Pb dating,a large age range of 3101 ± 48 Ma ～ 413 ± 9 Ma has been gained for the FZG,which can be divided into 5 groups with the peak age values of 2537 Ma,1567 Ma,940 Ma,749 Ma and 440 Ma,respectively. These peak ages imply that the FZG has a mixture source from North China and Yangtze plates,and the youngest peak age suggests that the FZG has been formed in late Early Paleozoic.
引文
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Okay AI,Xu ST andeng9r AMC.1989.Coesite from the Dabie Shan eclogites,central China.European Journal of Mineralogy,1(4):595-598
Okay AI,eng9r AMC and Satir M.1993.Tectonics of an ultra-highpressure metamorphic terrane:The Dabie Shan/Tongbai Shan orogen,China.Tectonics,12(6):1320-1334
Qiu YM,Gao S,McN aughton NJ,Groves DI and Ling WL.2000.First evidence of>3.2Ga continental crust in the Yangtze craton of South China and its implications for Archean crustal evolution and Phanerozoic tectonics.Geology,28(1):11-14
Ratschbacher L,Franz L,Enkelmann E,Jonckheere R,P9rschke A,Hacker BR,Dong SW and Zhang YQ.2006.The Sino-KoreanYangtze suture,the Huwan detachment,and the Paleozoic-Tertiary exhumation of(ultra)high-pressure rocks along the Tongbai-XinxianDabie Mountains.In:Hacker BR,McC lelland WC,Liou JG(eds.).Ultrahigh-pressure Metamorphism:Deep Continental Subduction.Geological Society of America,403:45-75
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Wang YS,Sheng Y,Xiang BW and Zhang CY.2012.Metamorphic pressure of the Luzhenguan Group in the North Huaiyang low-grade metamorphic belt and its indication for evolution of the Dabie Mountains.Geological Review,58(5):865-872(in Chinese with English abstract)
Wu CM,Zhang J and Ren LD.2004.Empirical garnet-biotiteplagioclase-quartz(GBPQ)geobarometry in medium-to high-grade metapelites.Journal of Petrology,45(9):1907-1921
Wu CM and Zhao GC.2006.Recalibration of the garnet-muscovite(GM)geothermometer and the garnet-muscovite-plagioclase-quartz(GMPQ)geobarometer for metapelitic assemblages.Journal of Petrology,47(4):2357-2368
Wu CM and Chen HX.2015a.Revised Ti-in-biotite geothermometer for ilmenite-or rutile-bearing crustal metapelites.Science Bulletin,60(1):116-121
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Chen FK,Guo JH,Jiang LL,Siebel W,Cong BL and Satir M.2003.Provenance of the Beihuaiyang lower-grade metamorphic zone of the Dabie ultrahigh-pressure collisional orogen,China:Evidence from zircon ages.Journal of Asian Earth Sciences,22(4):343-352
Chen WT,Sun WH,Wang W,Zhao JH and Zhou MF.2014.“Grenvillian”intra-plate mafic magmatism in the southwestern Yangtze Block,SW China.Precambrian Research,242:138-153
Chen YZ and Sao BL.1995.Metamorphic petrology and metamorphism of the Foziling Group in northern Huaiyang and its age.Regional Geology of China,3:280-188(in Chinese with English abstract)
Cong BL.1996.Ultrahigh-Pressure Metamorphic Rocks in the Dabieshan-Sulu Region of China.Beijing:Science Press,1-224
Faure M,Lin W,Shu L,Sun Y and Schrer U.1999.Tectonics of the Dabieshan(eastern China)and possible exhumation mechanism of ultra-high-pressure rocks.Terra Nova,11(6):251-258
Faure M,Lin W,Schrer U,Shu LS,Sun Y and Arnaud N.2003.Continental subduction and exhumation of UHP rocks:Structural and geochronological insights from the Dabieshan(East China).Lithos,70(3-4):213-241
Gao S,Ling WL,Qiu YM,Lian Z,Hartmann G and Simon K.1999.Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton:Evidence for cratonic evolution and redistribution of REEduring crustal anatexis.Geochimica et Cosmochimica Acta,63(13-14):2071-2088
Gao S,Qiu YM,Ling WL,McN aughton NJ and Groves DI.2001.Single zircon U-Pb dating of the Kongling high-grade metamorphic terrain:Evidence for>3.2Ga old continental crust in the Yangtze craton.Science in China(Series D),44(4):326-335
Gao S,Yang J,Zhou L,Li M,Hu ZC,Guo JL,Yuan HL,Gong HJ,Xiao GQ and Wei JQ.2011.Age and growth of the Archean Kongling terrain,South China,with emphasis on 3.3Ga granitoid gneisses.American Journal of Science,311(2):153-182
Holdaway MJ.2000.Application of new experimental and garnet Margules data to the garnet-biotite geothermometer.American Mineralogist,85(7-8):881-892
Ji WB,Lin W,Faure M,Shi YH and Wang QC.2017.The Early Cretaceous orogen-scale Dabieshan metamorphic core complex:Implications for extensional collapse of the Triassic HP-UHP orogenic belt in east-central China.International Journal of Earth Sciences,106(4):1311-1340
Li SG,Wang SS,Chen YZ,Liu DL,Qiu J,Zhou HX and Zhang ZM.1994.Excess argon in phengite from eclogite:Evidence from dating of eclogite minerals by Sm-Nd,Rb-Sr and40Ar-39Ar methods.Chemical Geology,112(3-4):343-350
Li SG,Huang F,Nie YH,Han WL,Long G,Li MH,Zhang SQ,and Zhang ZH.2001.Geochemical and geochronological constraints on the suture location between the North and South China Blocks in the Dabie orogen,central China.Physics and Chemistry of the Earth,Part A:Solid Earth and Geodesy,26(9-10):656-672
Li XH,Li ZX and Li WX.2014.Detrital zircon U-Pb age and Hf isotope constrains on the generation and reworking of Precambrian continental crust in the Cathaysia Block,South China:A synthesis.Gondwana Research,25(3):1202-1215
Lin W,Wang QC,Faure M and Arnaud N.2005.Tectonic evolution of the Dabieshan orogen:In the view from polyphase deformation of the Beihuaiyang metamorphic zone.Science in China(Series D),48(7):886-899
Lin W,Ji WB,Faure M,Wu L,Li QL,Shi YH,Scharer U,Wang Fand Wang QC.2015.Early Cretaceous extensional reworking of the Triassic HP-UHP metamorphic orogen in Eastern China.Tectonophysics,662:256-270
Liu YC,Li SG,Xu ST,Jahn BM,Zheng YF,Zhang ZQ,Jiang LL,Chen GB and Wu WP.2005.Geochemistry and geochronology ofeclogites from the northern Dabie Mountains,central China.Journal of Asian Earth Sciences,25(3):431-443
Niu BG,Fu YL,Liu ZG,Ren JS and Chen W.1994.Main tectonothermal events and40Ar/39Ar dating of the Tongbai-Dabie MTS.Acta Geoscientia Sinica,(1-2):20-34(in Chinese with English abstract)
Okay AI,Xu ST andeng9r AMC.1989.Coesite from the Dabie Shan eclogites,central China.European Journal of Mineralogy,1(4):595-598
Okay AI,eng9r AMC and Satir M.1993.Tectonics of an ultra-highpressure metamorphic terrane:The Dabie Shan/Tongbai Shan orogen,China.Tectonics,12(6):1320-1334
Qiu YM,Gao S,McN aughton NJ,Groves DI and Ling WL.2000.First evidence of>3.2Ga continental crust in the Yangtze craton of South China and its implications for Archean crustal evolution and Phanerozoic tectonics.Geology,28(1):11-14
Ratschbacher L,Franz L,Enkelmann E,Jonckheere R,P9rschke A,Hacker BR,Dong SW and Zhang YQ.2006.The Sino-KoreanYangtze suture,the Huwan detachment,and the Paleozoic-Tertiary exhumation of(ultra)high-pressure rocks along the Tongbai-XinxianDabie Mountains.In:Hacker BR,McC lelland WC,Liou JG(eds.).Ultrahigh-pressure Metamorphism:Deep Continental Subduction.Geological Society of America,403:45-75
Shi YH,Cao S,Wang J,Nie F and Kang T.2014.Analysis of petrology,geochronology for Beihuaiyang metamorphic unit,and discussion about the suture of Dabie Orogen.Chinese Journal of Geology,49(2):378-393(in Chinese with English abstract)
Wang X,Jing L,Liou JG,Pan G,Liang W,Xia M and Maruyama S.1990.Field occurrences and petrology of eclogites from the Dabie Mountains,Anhui,central China.Lithos,25(1-3):119-131
Wang XM,Liou JG and Mao HK.1989.Coesite-bearing eclogite from the Dabie Mountains in central China.Geology,17(12):1085-1088
Wang YS,Sheng Y,Xiang BW and Zhang CY.2012.Metamorphic pressure of the Luzhenguan Group in the North Huaiyang low-grade metamorphic belt and its indication for evolution of the Dabie Mountains.Geological Review,58(5):865-872(in Chinese with English abstract)
Wu CM,Zhang J and Ren LD.2004.Empirical garnet-biotiteplagioclase-quartz(GBPQ)geobarometry in medium-to high-grade metapelites.Journal of Petrology,45(9):1907-1921
Wu CM and Zhao GC.2006.Recalibration of the garnet-muscovite(GM)geothermometer and the garnet-muscovite-plagioclase-quartz(GMPQ)geobarometer for metapelitic assemblages.Journal of Petrology,47(4):2357-2368
Wu CM and Chen HX.2015a.Revised Ti-in-biotite geothermometer for ilmenite-or rutile-bearing crustal metapelites.Science Bulletin,60(1):116-121
Wu CM and Chen HX.2015b.Calibration of a Ti-in-muscovite geothermometer for ilmenite-and Al2SiO5-bearing metapelites.Lithos,212-215:122-127
Wu YB,Zheng YF,Tang J,Cong B,Zhao ZF and Liu XM.2007.Zircon U-Pb dating of water-rock interaction during Neoproterozoic rift magmatism in South China.Chemical Geology,246(1-2):65-86
Wu YB,Gao S,Zhang HF,Zheng JP,Liu XC,Wang H,Gong GJ,Zhou L and Yuan HL.2012.Geochemistry and zircon U-Pb geochronology of Paleoproterozoic arc related granitoid in the northwestern Yangtze Block and its geological implications.Precambrian Research,200-203:26-37
Xu ST,Su W,Liu YC,Jiang LL,Ji SY,Okay AI and爦eng9r AMC.1992.Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting.Science,256(5053):80-82
Yang ZJ.1964.Geological time problems of Foziling Group.Geological Review,22(5):327-336(in Chinese)
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