Abercrombie brussel 青藏高原南缘新生代磨拉石的沉积

青藏高原南缘新生代磨拉石的沉积特征
uzzle：Mechanismofinvertedmetamorphismconstrainedby theSiwalksedimentaryrecord[J]．Currentscience，1997,oakley sale 四川若尔盖阿西金矿岩石学及岩石地球化学，71(11)：862—873．[1O]NajmaYMR，PringleMS，TohnsonMRW，eta1．LaserAr。7∞Ardat ingofsingledetritMmus-covitegrainsfromearlyforeland—basinsedimentarydepo sitsinIndia：ImplicationsforearlyHimalayasevolution[J]．Geology，1997，25：535--538．[11]BossartP，OtfigerR．RocksoftheMurreeForma-tion：IndicationsofadescendingforelandbasinoflatePa leocenetomiddleEoceneage?[J]．EclogaeGeolHelo,Abercrombie Paris，1989，82：133—165．[12]GansserA．Geology0ftheHimalayas[M]．London：IntersciencePubl，1964．289．[13]CriteUiS，GarzantiE．ProvenanceofthelowerTer-tiaryMurreeredbeds(Hazara-Kashmirsyntaxis，Pakistan)andinitialrisingoftheHima layas[J]．SedimentaryGeology，1994，89：265--284．[14]MngnierJL，LeturmyP，M嘣．JeG．11leSiwaliksofwesternNep alI．GeometryandKinematics[J]．Journal0fAsJanEarthSciences，1999,Günstige Ed Hardy，17：629—642．[15]SalvatoreCriteUi，RaymondVI．Sandstonepetrologyandpr ovenanceoftheSiwalikGroup(NorthwesternPakistanandW astm-n-southeaste~TtNepa1)口]．J0fSedimentRes，1994，A64：815--823．[16]Qa~]umM，LawrenceRD，NiemAR．Discoveryofthepalaeo-Indusdeltafancomplex[J]．JournaloftheGeologicalSociety，1997，54：753--756．[17]CurrayJR，MooreDG．GrowthoftheBengalDeep-SeaFanandDenudationintheHimalayas口]．GeologicalSocietyofAmericaBulletin,Abercrombie brussel，1971，82：563—572．[18]AlamM．GeologyandDepositionalHistoryofCeno-zoicSedimentsoftheBengalBasinofBangladesh[J]．Palaeography，Palaeolimetology，Palaeogeolo-gy，1989,Ed Hardy outlet，69：125—139．[19]KazuoA，AsahikoT．Two-phaseupliftofHigherHimalayasince17Ma[J]．Geology，1992，20：391—394．‘