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地质通报  2010 

大别山低级变质岩的构造背景

, PP. 795-810

Keywords: 大别山,弧前盆地,增生楔,洋壳

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Abstract:

大别山南北两侧的浅变质岩是碰撞造山以前洋壳俯冲造山阶段的重要组成部分。木兰山片岩或张八岭群是俯冲的洋壳;苏家河群、信阳群和佛子岭群是由洋壳俯冲形成的海沟沉积,并因俯冲过程中的前进变形而形成增生楔;杨山煤系和梅山群是石炭纪弧前盆地沉积,并因俯冲过程中的前进变形而被增生楔逆掩。宿松群是扬子大陆被动边缘沉积,不是俯冲造山带的成员。因洋壳俯冲形成的弧和弧后盆地可能已被新生界沉积物掩盖。高压―超高压变质带是碰撞造山后期从深部折返的外来体。高压―超高压变质带正好处于洋壳和增生楔之间,破坏了早期洋壳俯冲造山带的完整性,使得洋壳俯冲造山阶段的特征被破坏,因而不易辨别。俯冲造山阶段应为奥陶纪到泥盆纪,碰撞造山阶段应从二叠纪开始。

References

[1]  Ma C,Ehlers C,Xu C,The roots of the Dabieshan ultrahigh (pressu re metamorphic terrane:constrains from geochemistry and Nd-Sr isotope systems,Precambrian Research,2000.
[2]  Zhang H,Gao S,Zhong Z,Geochemical and Sr-Nd-Pb isotopic compositions of Cretaceous granotoids:constrains on tectonic framework and crustal structure of the Dabieshan ultrahigh-pressure metamorphic belt,China,Geochemical Geology,2002.
[3]  徐树桐,陈冠宝,刘贻灿,大别山造山带地质图:《大别山超高压变质作用与碰撞造山动力学》附件,北京:科学出版社,2005.
[4]  Li S,Sun W,Zhang G,Chronology of ultrahigh pressure in the Dabie Mountains and Sulu terrane:I.Sm-Nd isotope system,Science in China(Series D),1996.
[5]  Li S,Chen Y,Mill J,Geochemical and geochronological constrains on the tectonic outline of the Dabie Mountains,central China:A continent-micro-continent-collision model,Continental Dynamics,1998(Special Issue).
[6]  Li S,Jagoutz E,Chen Y,Sm-Nd and Rb-Sr isotope chronology of ultrahigh pressure metamorphic rocks and their country rocks at Shuanghe m the Dabie Mountains,central China,Geochemica and Cosmochimica Acta,2000.
[7]  Chavagnac V,Jahn B,Coesite-bearing eclogites from the Bixiling complex,Dabie Mountains,China:Sm-Nd ages,geochemical characteristics and tectomc implications,Chemical Geology,1996.
[8]  Chen D,Deloule E,Chen H,Multi-isotopic system geochronology of low temperature eclogite from Huangzhen,south ern Dabie terrane,Science in China (Series D:Earth Sciences),2004.
[9]  Hacker B R,Ratschbacher L,Webb L,U-Pb zircon ages constrain the architecture of the ultrahigh pressure Qinling-Dabie orogen,China,Earth and Planetary Science Letters,1998.
[10]  简平,刘敦一,杨巍燃,大别山西部河南罗山熊店加里东期榴辉岩锆石特征及SHRIMP分析结果,地质学报,2000(3).
[11]  Liu Y,Li S,Xu S,Zircon SHRIMP U-Pb dating for gneisses in northem Dabie high T/P zone,central China:Implications for de coupling within subducted continental crust,Lithos,2008.
[12]  刘贻灿,李曙光,俯冲陆壳内部的拆离和超高压岩石的多板片差异折返:以大别-苏鲁造山带为例,科学通报,2007(18).
[13]  Chen H,King R A,Nakamura Z,Tansitional time of oceanic to continental subduction in the Dabie orogen:constrains for U-Pb,Lu-Hf,Sm-Nd and Ar-Ar multichronometric dating,Lithos,2009.
[14]  Underwood M B,Moore G F,Trenches and trench-slope basins,Blackwell Sceince,1995.
[15]  安徽省地质矿产局,安徽省区域地质志,北京:地质出版社,1987.
[16]  河南省地质矿产局,河南省区域地质志,北京:地质出版社,1989.
[17]  Hsü K J,Relic back-arc basins:Principles of recognition and possible new examples from China,New York:springer-verlag,1988.
[18]  安徽省地质矿产局,安徽省岩石地层,武汉:中国地质大学出版社,1997.
[19]  高联达,刘志刚,河南信阳群南湾组微体化石的发现及其地质意义,地质论评,1988(5).
[20]  叶伯丹,许俊文,李志昌,桐柏-大别山地区苏家河群动物化石的发现及其意义,中国地质,1991.
[21]  刘志刚,牛宝贵,任纪舜,信阳群的解体及其大地构造意义,地质论评,1992(4).
[22]  刘志刚,富云莲,牛宝贵,大别山北坡苏家河群及原信阳群龟山组变基性杂岩测年及其地质意义,科学通报,1993(13).
[23]  金福全,张廷秀,王家文,河南同始花园墙组时代的新认识,地层学杂志,1994(4).
[24]  刘印环,杜凤军,刘振宏,河南省"商城群"中晚奥陶世化石的发现及其意义,中国区域地质,1995(2).
[25]  刘文灿,王果胜,马文璞,大别山北麓梅山群的含义、区域对比及时代归属,中国区域地质,1996(3).
[26]  王晓燕,崔文元,刘树忠,豫南地区含柯石英榴辉岩的发现,岩石学报,1993(2).
[27]  Xu S,Okay A I,Ji S,Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting,Science,1992.
[28]  Xu S,Lin Y,Chen G,New findings of microdiamonds in eclogite from Dabie-Sulu region in China,Chinese Science Bulletin,2003.
[29]  马文璞,刘文灿,王果胜,梅山群的再定位,现代地质,1997(1).
[30]  Suo S,Zhong,Sequence of ductile shear zone in UHP metamorphic province within Dabie massif,China,Journal of China University of Geosciences,1998(3).
[31]  Hacker B R,Rutschbacher L,Webb L,Exhumation of ultra-high-pressure continental crust in east central China:late Triassic -early Jurassic tectonic unroofing,Journal of Geophysical Research,2000(B6).
[32]  汤加富,大别山及邻区地质构造特征与形成演化,北京:地质出版社,2003.
[33]  Wang Q,Shi Y,Guo J,Exhumation of the Dabie UHP terrane,China,International Geology Review,2008.
[34]  Xu Z,Etude tectonique et de la Chaine Paleozoic et Triassique des Qinlings (Chine),Univ.Sci.Tech.Languedoc,Montpenier,1987.
[35]  Okay A I,Xu S,Sengor A M C,Coesite from the Dabie Shan eclogite,central China,European Journal of Mineralogy,1989.
[36]  Wang X,Liou J G,Mao H,Coesite-bearing eclogites from the Dabie Mountains in central China,Geology,1989.
[37]  Wang X,Liou J G,Regional ultrahigh pressure coesite-bearing eclogite terrane in central China:evidence from country rocks,gneiss marble,and metapelite,Geology,1991.
[38]  Zhang R Y,Liou J G,Wang X,Discovery of coesite from eclogite in Henan,central China and its geological significance,Acta Petrolei Sinica,1993(2).
[39]  Xu S,Liu Y,Chen G,Microdiamonds,their classification and tectonic implicatiom for the host eclogites from Dabie and Su-Lu regions in central eastern China,Mineralogical Magazine,2005(4).
[40]  刘贻灿,李曙光,徐树桐,北大别片麻岩的超高压变质证据--来自锆石提供的信息,岩石学报,2006(7).
[41]  Zhang R,Shu J F,Mao H K,Magnetite hmellae in olivine and clinohumite from Dabie UHP ultramafic rocks,central China,American Mineralogist,1999.
[42]  Li X P,Zheng Y-F,Wu Y-B,Low-T eclogite in the Dabie Terrane of China:petrological and isotopic constraints on fluid activity and radiometric dating,Contributions to Mineralogy & Petrology,2004.
[43]  Castelli D,Rolfo F,Compagnoni R,Metamorphic veins with kyanite,zoisite and quartz in the Zhu-Jia-Chong eclogite,Dabie Shan,China,Island Arc,1998.
[44]  Schmidt M W,Poli S,The stability of lawsanite and zoisite at high pressure:experiments in CASH to 92 kbar and implicatiom for the presence of hydrous phases in subducted lithosphere,Earth and Planetary Science Letters,1994(1/4).
[45]  Schmidt M W,Lawsonite:upper pressure stability and formation of high density hydrous phases,American Mineralogist,1995.
[46]  Ma W,The Carboniferous at the northern foot of the Dabie Mountains and its tectonic implications,Acta Geologica Sinica,1991(3).
[47]  湖北省地质矿产局,湖北省区域地质志,北京:地质出版社,1990.
[48]  商庆芳,薛松鹤,曹祯,河南西峡信阳群龟山组化石碎屑的发现及其意义,河南地质,1992(1).
[49]  河南省地质矿产厅,河南省岩石地层,武汉:中国地质大学出版社,1997.
[50]  Marsaglia K M,Interarc and backarc basins,Blackwell Sceince,1995.
[51]  徐树桐,袁学诚,吴维平,刘贻灿,大别山黄石-六安反射地震剖面新的地质解释,地质通报,2008(1).
[52]  安徽省地质矿产局区域地质调查队,安徽省地层志(前寒武系分册),合肥:安徽科学技术出版社,1985.
[53]  徐树桐,刘贻灿,江来利,大别山的构造格局和演化,北京:科学出版社,1994.
[54]  Faure M,Lin W,Shu L,Tectonics of the Dabieshan (eastern China) and possible exhumation mechanism of ultra high-pressure rocks,Terra Nova,1999(6).
[55]  Turner F J,Verhoogen J,Igneous and Metamorphic Petrology (second edition),New York:mcgraw-hill Book Company,inc,1960.
[56]  Carmichael I S E,Turner F J,Verhoogen J,Igneous Petrology,New York:mcgraw-hill Book Company,inc,1974.
[57]  Jahn B,Liu X,Yui Z-F,High pressure/ultrahigh pressure eclogites from the Hong\'an Block,East-central China:Geochemical characterization,isotope disequilibrium and geochronological controversy,Contributions to Mineralogy & Petrology,2005.
[58]  Liu X,Jahn B-M,Liu D-Y,SHRIMP U-P zircon dating of a metagabbro and eclogites from western Dabieshan (Hong\'an Block),China,Tectonophysics,2004.
[59]  Li S-G,Huang F,Nie Y-H,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,2001(9/10).
[60]  徐树桐,刘贻灿,江来利,大别山造山带的构造几何学和运动学,合肥:中国科学技术大学出版社,2002.
[61]  游振东,韩郁菁,杨巍然,东秦岭大别高压超高压变质带,武汉:中国地质大学出版社,1998.
[62]  Hydman W D,Petrology of Igneous and Metamorphic Rocks,New York:mcgraw-hill Book Company,inc,1972.
[63]  Ernst W G,Zhou G,Liou J G,High-pressure and surper-high-pressure metamorphic terranes in the Qinling-Dabie Mountain belt,central China:early-to middle-Phanerozoic accretion of the western Paleo-Pacific rim,Pac Sci Assoc Info Bull,1991.
[64]  Zhou G,Liu Y J,Edie E A,High pressure/low temperature metamorphism in northern Hubei Province,central China,Journal of Metamorphic Geology,1993.
[65]  Eide E A,Liou J G,High-pressure blue schists and eclogites in Hong\'an:a framework for addressing the evolution of high-and ultrahigh-pressure rocks in central China,Lithos,2000.
[66]  Nakajima T,Maruyama S,Uchiumi S,Evidence for late Proterozoic subduction from 700-Myr-old blueschists in China,Nature,1990(2681).
[67]  Ingersoll R V,Busby C J,Tectonics of sedimentary basius,Blackwell Sceince,1995.
[68]  Liou J G,Wang X,Coleman R G,Blueschist in major suture zones of China,Tectonics,1989(3).
[69]  全国地层委员会,中国区域年代地层(地质年代)表,地层学杂志,2005(增刊).
[70]  汤加富,钱存照,高天山,大别山榴辉岩带浅变质火山-碎屑岩层组合的发现及其地质意义,安徽地质,1995(2).
[71]  Moores E M,Twiss R J,Tectonics,Freeman and Company,1995.
[72]  Xu S,Wu W,Xiao W,Moissanite in serpentinite from the Dabie Mountains in China,Mineralogical Magazine,2008(4).
[73]  荆延仁,汤家富,高天山,安徽宿松天蓝石的矿物学研究,科学通报,1995(23).
[74]  刘雅琴,胡克,中国中部高铝质超高压变质岩,岩石学报,1999(4).
[75]  Hsü K J,Thin-skinned plate-tectonic model for collision-type orogenesis,Science in China,1981(1).
[76]  徐树桐,吴维平,刘贻灿,大别山的变质碰撞混杂岩,地质力学学报,2008(1).
[77]  Liu X,Wei C,Li S,Thermobaric structure of a traverse across western Dabieshan:implications for collision tectonics between the Sino-Korean and Yangtze Cratous,Journal of Metamorphic Geology,2004.

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