引文
[1]安徽省地质矿产局.安徽省区域地质志.北京:地质出版社,1987ABGMR(Anhui Bureau of Geology and Mineral Resources).Regional Geology of Anhui Province(in Chinese).Beijing:Geological Publishing House,1987.
[2]万天丰.中国大地构造学纲要.北京:地质出版社,2004.Wan T F.An Outline in Tectonics of China(in Chinese).Beijing:Geological Publishing House,2004.
[3]杜建国,张鹏.大别造山带北部的中生代火山岩.现代地质,1999,13(1):57-65.Du J G,Zhang P.Mesozoic volcanic rocks in northern part ofDabie orogenic belt.Geoscience(in Chinese),1999,13(1):57-65.
[4]刘文灿,王果胜.北淮阳地区中生代逆冲推覆构造.现代地质,1999,13(2):143-149.Liu W C,Wang G S.Mesozoic thrust and nappe tectonics innorthern Huaiyang region.Geoscience(in Chinese),1999,13(2):143-149.
[5]李丕龙,李学田,宋明水等.合肥盆地石油地质与地球物理特征研究及进展.北京:地质出版社,2003.Li P L,Li X T,Song M S,et al.Petroleum Geology andGeophysical Prospecting and Advance in Heifei Basin(inChinese).Beijing:Geological Publishing House,2003.
[6]柳忠泉.北淮阳构造带可燃天然气的发现与合肥盆地油气远景分析.地质学报,2009,83(4):478-482.Liu Z Q.Discovery of the combustible gas in the Beihuaiyangtectonic belt and analysis of oil-gas potential in the HefeiBasin.Acta Geologica Sinica(in Chinese),2009,83(4):478-482.
[7]詹婷婷.安徽发现特大钼矿.当代矿工,2010,(6):21.Zhan T T.Discovery of large molybdenum orefield in Anhuiprovince.Modern Miner(in Chinese),2010,(6):21.
[8]Grimmer J C,Jonckheere R,Enkelmann E,et al.Cretaceous-Cenozoic history of the southern Tan-Lu faultzone:apatite fission-track and structural constraints from theDabie Shan(eastern China).Tectonophysics,2002,359(3-4):225-253.
[9]陈建平.合肥盆地中新生代构造演化与油气地质特征.北京:地质出版社,2005.Chen J P.Tectonic Evolution and Oil-Gas Exploration duringthe Mesozoic and Cenozoic in the Hefei Basin(in Chinese).Beijing:Geological Publish House,2005.
[10]Jahn B M,Chen B.Dabieshan UHP metamorphic terrane:Sr-Nd-Pb isotopic constraint to pre-metamorphic subductionpolarity.International Geology Review,2007,49(1):14-29.
[11]侯广顺,韩吟文,曲军锋.秦岭—大别造山带地壳化学结构研究.地球化学,2003,32(3):230-238.Hou G S,Han Y W,Qu J F.Research of continental crustchemical texture of Qinling-Dabie orogenic belt.Geochimica(in Chinese),2003,32(3):230-238.
[12]张本仁,张宏飞,高山.大别造山带现今地壳结构-岩石组成研究.矿物岩石地球化学通报,2004,23(3):187-193.Zhang B R,Zhang H F,Gao S.Rock-constitution of variousstructural layers of the present crust in the Dabie orogenicbelt,Central China.Bulletin of Mineralogy,Petrology andGeochemistry(in Chinese),2004,23(3):187-193.
[13]Zhang L,Zhong Z,Zhang H,et al.The formation of foliated(garnet-bearing)granites in the Tongbai-Dabie orogenic belt:Partial melting of subducted continental crust during exhumation.Journal of Metamorphic Geology,2009,27(9):789-803.
[14]林伟,王清晨,Faure M等.从北淮阳构造带的多期变形透视大别山构造演化.中国科学(D辑),2005,35(2):127-139.Lin W,Wang Q C,Faure M,et al.Tectonic evolution of theDabieshan orogen:In the view from polyphase deformation ofthe Beihuaiyang metamorphic zone.Science in China(SeriesD)(in Chinese),2005,48(7):886-899.
[15]董树文,孙先如,张勇等.大别山碰撞造山带基本结构.科学通报,1993,38(6):542-545.Dong S W,Sun X R,Zhang Y,et al.Basic structure of Dabiecollisional orogen.Chinese Science Bulletin(in Chinese),1993,38(6):542-545.
[16]肖骑彬,赵国泽,詹艳等.大别山超高压变质带深部电性结构及其动力学意义初步研究.地球物理学报,2007,50(3):812-822.Xiao Q B,Zhao G Z,Zhan Y,et al.A preliminary study onelectrical structure and dynamics of the ultrahigh pressuremetamorphic belt beneath the Dabie Mountains.Chinese J.Geophys.(in Chinese),2007,50(3):812-822.
[17]王椿镛,郑金涵,胡鸿翔等.大别造山带的地壳结构研究.中国科学(D辑),1997,27(3):221-226.Wang C Y,Zheng J H,Hu H X,et al.Study on cruststructure of Dabie orogen.Science in China(Series D)(inChinese),1997,27(3):221-226.
[18]董树文,吴宣志,高锐等.大别造山带地壳速度结构与动力学.地球物理学报,1998,41(3):349-361.Dong S W,Wu X Z,Gao R,et al.On the crust velocitylevels and dynamics of the Dabieshan orogenic belt.ChineseJ.Geophys.(Acta Geophysica Sinica)(in Chinese),1998,41(3):349-361.
[19]刘福田,徐佩芬,刘劲松等.大陆深俯冲带的地壳速度结构-东大别造山带深地震宽角反射/折射研究.地球物理学报,2003,46(3):366-372.Liu F T,Xu P F,Liu J S,et al.The crustal velocitystructure of the continental deep subduction belt:study onthe eastern Dabie orogen by seismic wide-angle reflection/refraction.Chinese J.Geophys.(in Chinese),2003,46(3):366-372.
[20]赵志新,徐纪人.苏鲁大别及其周围地区深部P波速度结构特征的初步分析.岩石学报,2005.21(2):525-532.Zhao Z X,Xu J R.Characteristic outline of P wave velocitystructure in the depth beneath the Sulu-Dabie region.ActaPetrologica Sinica(in Chinese),2005,21(2):525-532.
[21]徐佩芬,刘福田,王清晨等.大别—苏鲁碰撞造山带的地震层析成像研究-岩石圈三维速度结构.地球物理学报,2000,43(3):377-385.Xu P F,Liu F T,Wang Q C,et al.Seismic tomographybeneath the Dabie-Sulu collision orogen-3Dvelocity structuresof lithosphere.Chinese J.Geophys.(in Chinese),2000,43(3):377-385.
[22]赵志新,徐纪人,许志琴.上地幔三维S波速度结构与大别苏鲁超高压变质带俯冲折返机制探讨.岩石学报,2004,20(1):157-164.Zhao Z X,Xu J R,Xu Z Q.3-D S wave velocity structure inthe upper mantle and the mechanism investigation for theultrahigh-pressure metamorphosed belt in the Dabie-Suluregion.Acta Petrologica Sinica(in Chinese),2004,20(1):157-164.
[23]刘启元,Rainer K,陈九辉等.大别造山带壳幔界面的断错结构和壳内低速体.中国科学(D辑),2005,35(4):304-313.Liu Q Y,Rainer K,Chen J H,et al.The break-slipstructure and low-speed body in crust at the boundary ofcrust-mantle in Dabie orogen.Science in China(Series D)(in Chinese),2005,35(4):304-313.
[24]高锐,董树文,贺日政等.莫霍面地震反射图像揭露出扬子陆块深俯冲过程.地学前缘,2004,11(3):43-49.Gao R,Dong S W,He R Z,et al.Subduction process of theYangtze continental block from Moho reflection image,SouthChina.Earth Science Frontiers(in Chinese),2004,11(3):43-49.
[25]董树文,高锐,李秋生等.大别山造山带前陆深地震反射剖面.地质学报,2005,79(5):595-601.Dong S W,Gao R,Li Q S,et al.A deep seismic reflectionprofile across a foreland of the Dabie Orogen.GeologicaSinica(in Chinese),2005,79(5):595-601.
[26]Yuan X C,Klemperer S L,Teng W B,et al.Crustalstructure and exhumation of the Dabie Shan ultrahighpressure orogen,eastern China,from seismic reflectionprofiling.Geology,2003,31(5):435-438.
[27]徐树桐,袁学诚,吴维平等.大别山黄石—六安反射地震剖面新的地质解释.地质通报,2008,27(1):19-26.Xu S T,Yuan X C,Wu W P,et al.New geologicalinterpretation of the seismic reflection profile from Huangshito Liu’an across the Dabie Mountains,China.GeologicalBulletin of China(in Chinese),2008,27(1):19-26.
[28]江来利,吴维平,储东如.大别造山带东段扬子陆块和华北陆块间缝合带的位置.地球科学(中国地质大学学报),2005,30(3):264-274.Jiang L L,Wu W P,Chu D R.Location of the suture zonebetween Yangtze and North China blocks in Eastern DabieOrogen.Earth Science(Journal of China University ofGeosciences)(in Chinese),2005,30(3):264-274.
[29]李曙光,杨蔚.大别造山带深部地缝合线与地表地缝合线的解耦及大陆碰撞岩石圈楔入模型:中生代幔源岩浆岩Sr-Nd-Pb同位素证据.科学通报,2002,47(24):1898-1905.Li S G,Yang W.Suture decoupling of deep part and surfacialpart in Dabie orogen and the wedge model of continentcollision lithosphere:evidence of Sr-Nd-Pb from Mesozoicmagma of mantle.Chinese Science Bulletin(in Chinese),2002,47(24):1898-1905.
[30]索书田,钟增球,周汉文等.大别—苏鲁超高压和高压变质带构造演化.地学前缘,2004,11(3):71-82.Suo S T,Zhong Z Q,Zhou H W,et al.Tectonic evolution ofDabie-Sulu UHP and HP metamorphic belts,East-CentralChina.Earth Science Frontiers(China University ofGeosciences,Beijing)(in Chinese),2004,11(3):71-82.
[31]大别山超高压变质作用与碰撞造山动力学编写组.大别山超高压变质作用与碰撞造山动力学.北京:科学出版社,2005.Editing Board of Ultrahigh-pressure Metamorphism andCollisional Dynamics of the Dabie Mountains(EBUMCDDM).Ultrahigh-pressure Metamorphism and Collisional Dynamics ofthe Dabie Mountains(in Chinese).Beijing:Science Press,2005.
[32]Li R W,Wan Y S,Cheng Z Y,et al.Provenance of Jurassicsediments in the Hefei Basin,east-central China and thecontribution of high-pressure and ultrahigh-pressure metamorphicrocks from the Dabie Shan.Eartha nd Planetary Science Letters,2005,231(3-4):279-294.
[33]张交东,郝天珧,樊德华等.合肥盆地中生界的地层时代判识及意义.地质学报,2009,83(5):599-608.Zhang J D,Hao T Y,Fan D H,et al.Identification ofgeological time of Mesozoic strata in Hefei basin and itssignificance.Acta Geologica Sinica(in Chinese),2009,83(5):599-608.
[34]安徽省地质矿产局.安徽地层志(白垩系分册,侏罗系分册).合肥:安徽科学技术出版社,1988:66-126(白垩系分册),17-37(侏罗系分册).ABGMR(Anhui Bureau of Geology and Mineral Resources).Stratigraphic Memoirs of Anhui(cretaceous Volume andJurassic Volume).Hefei:Anhui Science and TechnologyPress,1988.66-126(cretaceous Vo1ume),17-37(JurassicVolume).
[35]张交东,刘德良,徐春华等.北淮阳构造带的电性结构.地学前缘,2003,(4):544.Zhang J D,Liu D L,Xu C H,et al.Electrical structure ofthe Beihuaiyang metamorphic zone.Earth Science Frontiers(in Chinese),2003,(4):544.
[36]滕吉文,白武明,张中杰等.中国大陆动力学研究导向和思考.地球物理学进展,2009,24(6):1913-1936.Teng J W,Bai W M,Zhang Z J,et al.Developmentdirection and ponders of the continental dynamics in China.Progress in Geophysics(in Chinese),2009,24(6):1913-1936.
[37]李云平,吴时国,韩文功等.合肥盆地和郯庐断裂带南段深部地球物理特征研究.地球物理学报,2006,49(1):115-122.Li Y P,Wu S G,Han W G,et al.A study on geophysicalfeatures of deep structures of the Hefei Basin and the southernTan-Lu fault zone.Chinese J.Geophys.(in Chinese),2006,49(1):115-122.
[38]郝天珧,黄松,徐亚等.关于黄海深部构造的地球物理认识.地球物理学报,2010,53(6):1315-1326.Hao T Y,Huang S,Xu Y,et al.Geophysicalunderstandings on deep structure in Yellow Sea.Chinese J.Geophys.(in Chinese),2010,53(6):1315-1326.
[39]戴圣潜,邓晋福,吴宗絮等.大别造山带燕山期造山作用的岩浆岩石学证据.中国地质,2003,30(2):159-164.Dai S Q,Deng J F,Wu Z X,et al.Evidence of magmaticpetrology for the Yanshanian orogeny in the Dabie orogen.Geology in China(in Chinese),2003,30(2):159-164.
[40]赵子福,郑永飞.俯冲大陆岩石圈重熔:大别—苏鲁造山带中生代岩浆岩成因.中国科学(D辑),2009,39(7):888-909.Zhao Z F,Zheng Y F.Remeshing of subducted continentallithosphere:Petrogenesis of Mesozoic magmatie rocks in theDabie-Sulu orogenic belt.Science in China(Series D)(inChinese),2009,52(9):1295-1318.
[41]冀文斌,林伟,石永红等.大别山早白垩世变质核杂岩的结构与演化.地质科学,2011,46(1):161-180.Ji We B,Lin W,Shi Y H,et al.Structure and evolution ofthe Early Cretaceous Dabieshan metamorphic core complex.Geologica Sinica(in Chinese),2011,46(1):161-180.
[42]介霖,朱儒勋,陈瑞庚等.中国石油地质志(卷八)苏浙皖闽油气区.北京:石油工业出版社,1992.341-409.Jie L,Zhu R X,Chen R G,et al.Petroleum Geology ofChina(8):Jiangsu,Zhejiang and Anhui Provinces(inChinese).Beijing:Petroleum Industry Press,1992.341-409.
[43]沈修志,薛爱民,刘德良等.华北南部盆地构造与天然气关系.合肥:中国科学技术大学出版社,1995.Shen X Z,Xue A M,Liu D L,et al.The RelationshipBetween Tectonics and Natural Gas in the Southern NorthChina Basin(in Chinese).Hefei:Publishing House of ChinaUniversity of Science and Technology,1995.
[44]张交东,王登稳,刘德良等.合肥盆地安参1超深井钻遇的基底时代问题讨论.地质论评,2008,54(4):433-438.Zhang J D,Wang D W,Liu D L,et al.A discussion on thebasement time in the deep drill Ancan-1,Hefei basin,southern margin of the North China Plate.Geological Review(in Chinese),2008,54(4):433-438.
[45]张交东,刘德良,黄开权等.合肥盆地盆缘刘老碑组烃源岩特征探讨.石油实验地质,2004,26(5):474-478.Zhang J D,Liu D L,Huang K Q,et al.Discussion on thehydrocarbon source rock characters of the Liulaobei formationon the fringes of the Hefei basin.Petroleum Geology&Expeximent(in Chinese),2004,26(5):474-478.
[46]赵新福,李建威,马昌前等.北淮阳古碑花岗闪长岩侵位时代及地球化学特征:对大别山中生代构造体制转换的启示.岩石学报,2007,23(6):1392-1402.Zhao X F,Li J W,Ma C Q,et al.Geochronology andgeochemistry of the Gubei granodiorite,North Huaiyang:Implications for Mesozoic tectonic transition of the Dabieorogen.Acta Petrologica Sinica(in Chinese),2007,23(6):1392-1402.
[47]刘晓春,江博明,李三忠等.桐柏高压变质地体:对桐柏—大别—苏鲁高压/超高压变质带构造框架和俯冲/折返机制的制约.岩石学报,2011,27(4):1151-1162.Liu X C,Jahn B M,Li S Z,et al.The Tongbai HPmetamorphic terrane:constraints on the architecture andsubduction/exhumation of the Tongbai-Dabie-Sulu HP-UHPmetamorphic belt.Acta Petrologica Sinica(in Chinese),2011,27(4):1151-1162.
[48]董树文,张岳桥,龙长兴等.中国侏罗纪构造变革与燕山运动新诠释.地质学报,2007,81(11):1449-1461.Dong S W,Zhang Y Q,Long C X,et al.Jurassic tectonicrevolution in China and new interpretation of the Yanshanmovement.Acta Geologica Sinica(in Chinese),2007,81(11):1449-1461
[49]张岳桥,董树文,赵越等.华北侏罗纪大地构造:综评与新认识.地质学报,2007,81(11):1462-1480.Zhang Y Q,Dong S W,Zhao Y,et al.Jurassic tectonics ofnorth China:a synthetic view.Acta Geologica Sinica(inChinese),2007,81(11):1462-1480.
[50]Ren J Y,Tamaki K,Li S T,et al.Late Mesozoic andCenozoic rifting and its dynamic setting in eastern China andadjacent areas.Tectonophysics,2002,344(3-4):175-205.
[51]Wang Y S,Xiang B W,Zhu G,et al.Structural andgeochronological evidence for Early Cretaceous orogen-parallel extension of the ductile lithosphere in the northernDabie orogenic belt,east China.Journal of StructuralGeology,2011,33(3):362-380.
[52]Zhang J S,Wei C J,Lou Y X,et al.Phase equilibria ofhornblende-bearing eclogite in the Western Dabie Mountain,Central China.Acta Geologica Sinica,2009,83(1):57-69.
[53]滕吉文,闫雅芬,王光杰等.大别造山带与郯庐断裂带壳-幔结构和陆内“俯冲”的耦合效应.地球物理学报,2006,49(2):449-457.Teng J W,Yan Y F,Wang G J,et al.Structure of Earth′scrust and upper mantle,inland subduction and its couplingeffects on the Dabie orogenic belt and the Tancheng-Lujiangfault belt.Chinese J.Geophys.(in Chinese),2006,49(2):449-457.
[54]许志琴,梁凤华,杨经绥等.再论“大陆深俯冲和折返动力学”:来自中国大陆科学群钻及苏鲁超高压变质带的制约.岩石学报,2009,25(7):1561-1574.Xu Z Q,Liang F H,Yang J S,et al.Continental deepsubduction and exhumation dynamics:constraints from holesof the Chinese Continental Scientific Drilling and the SuluHP-UHP metamorphic terrane.Acta Petrologica Sinica(inChinese),2009,25(7):1561-1574.
[55]Malaspina N,Hermann J,Scambelluri M,et al.Multistagemetasomatism in ultrahigh-pressure mafic rocks from thenorth Dabie complex(China).Lithos,2006,90(1-2):19-42.
[56]郑永飞.超高压变质与大陆碰撞研究进展:以大别—苏鲁造山带为例.科学通报,2008,53(18):2129-2152.Zheng Y F.A perspective view on ultrahigh-pressuremetamorphism and continental collision in the Dabie-Suluorogenic belt.Chinese Science Bulletin(in Chinese),2008,53(20):3081-3104.
[57]杨经绥,许志琴,张建新等.中国主要高压-超高压变质带的大地构造背景及俯冲/折返机制的探讨.岩石学报,2009,25(7):1529-1560.Yang J S,Xu Z Q,Zhang J X,et al.Tectonic setting of mainhigh-and ultra-pressure metamorphic belts in China andadjacent region and discussion on their subduction andexhumation mechanism.Acta Petrologica Sinica(in Chinese),2009,25(7):1529-1560.
[58]Chen F K,Guo J H,Jiang L L,et al.Provenance of theBeihuaiyang lower-grade metamorphic zone of the Dabieultrahigh-pressure collisional orogen,China:Evidence fromzircon ages.Journal of Asian Earth Sciences,2003,22(4):343-352.
[59]杨文采.东大别超高压变质带的深部构造.中国科学(D),2003,33(2):183-192.Yang W C.Deep structure of eastern Dabie ultrahighpressure metamorphic belt.Science in China(Series D)(inChinese),2003,33(2):183-192.
[60]翟洪涛,张毅,孙宝延.合肥地区地震活动性及地震地质构造背景分析.华南地震,2006,26(3):68-77.Zhai H T,Zhang Y,Sun B Y.Analysis of seismic activityand seismogeological structure background in Hefei area.South China Journal of Seismology(in Chinese),2006,26(3):68-77.
[61]王国强,徐威,吴道祥等.安徽省环境地质特征与地质灾害.岩石力学与工程学报,2004,23(1):164-169.Wang G Q,Xu W,Wu D X,et al.Characteristics ofenvironmental geology and geological disasters of AnhuiProvince.Journal of Rock Mechanics and Engineering(inChinese),2004,23(1):164-169.