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桐柏—大别山高压超高压变质带
hemicatandgeodynamiealnotesandanextensivebibliography．In：SmithDC，ed．Eelogita—faciesRock．Amsterdam：Elseviver，l989．1～2O66ChopinC，H~nryC，MichaniA—Geologyandpetrologyofthecoesite~bearlr*terrain，DataMaltaMassif．WesternApls．EarJMth~al，1991．3#263~2917张泽明t辨振东．大别山地区含柯石英榴辉岩变质作用的轨迹及其地球动力学意义．地球科学——中国地质大学学报，1992，17(2)；1{l～1498董申保．中国蓝闪石片岩带的一般特征及其分布．地质学报,[link widoczny dla zalogowanych]，I989．3：273~2849张树业等．华中高压变质带的岩石组合特征及成因．见：刘国募等编．秦岭～大巴山地质论文臬f一)．北京：北京科学技术出版社．1990．221~228l0李曙光等．中国华北、华南陆块碰撞时代的钐一铷同位索年龄证据．中国科学B辑,[link widoczny dla zalogowanych]，1989，3312~31811徐树桐等．大别山高压变质带及其中的金刚石．见：郭令智等编．现代地质文集(上)．南京；南京大学出版社，1992．157～165】2Kr6nerA,[link widoczny dla zalogowanych]，ZhangGW．GranulitesiatheTongbaiaJ'e~t，QinlJngbelt,[link widoczny dla zalogowanych]，China：Geochen~stzy，petrology，slngtezir—congeochronology，andimplicationsforthetectonicevolutionofEasternAsia．Tectonics，l992．12(1)l245～255High—PressureandVeryHigh-PressureMetamorphicBeltofTongbai—DabieArea．CentralChinaZhangZemingYouZhendongHanYujing(chinaUni,x,r,sa,[link widoczny dla zalogowanych],ofGeosczences．w430074)AbstractHigh-pressureandveryhigh-pressuremetamorphicrocksinTongbai--Dab~RreRmaybecMssi-fledintothreebeltsfromsouthtonorth：theepidote—blueschistfacies，high—pressureeclogitefacie~andveryhish—presaureeclogitefacieelts．Thel丑tterwasformedbySLIbductionofoeealliccrustnorth—wardbeneaththeNorthChinaplateortheDabiemicro—plateduringtheCaledonianorogeny．Thefor-mertWOWereformedbysubduction—collisionbetweentheNorthChinaplateandYangtzeplateinTri—assictime·Atleasttwotimesofhigh—pre~uremetamorphismoccurredintheTbngbai—D~bieorogen·Keywordsmetamorphicbelt，eclogite，epidote—blueschist，Tongbai--Dabie，CentralChina．