摘要
TheDolomitesregionisaspectacularlyexposedportionoftheSouthernAlps,anorthernItalianchainderivedfromthecomparativelygentledeformationoftheTethyanpassivecontinentalmarginofAdria.TheregionhadanactivePermo-Jurassictectono-magmaticevolu-tion,leadingfromPermianmagmatism,throughaMid-dieTriassicepisodeoffastsubsidenceandvolcanism,totheJurassicoceanicbreak-up.AlthoughthesedimentarysuccessionrangesinagefromMiddlePermiantoCreta-ceous,thegeologicallandscapeislargelydominatedbythemajesticTriassiccarbonates,makingtheareaaclas-sicalonefortheearlyMesozoicstratigraphy.Particu-larlynoteworthyaretheAnisiantoCarniancarbonateplatforms,recordinganevolutionfromregionalmuddybankstoisolatedhigh-reliefbuilduos.Thehllineofthevariousbasinsandthedevelopmentofalastgenerationofregionalperitidalplatformfollowed.ThecarbonateplatformsoftheDolomitesbearwitnesstoaremarkablesetofchangesinthecarbonateproductionandtosignif-icantpalaeoclimaticfluctuations,fromaridtomoistcon-difionsandviceversa;agreatrangeofmarginandslopedepositionalstylesisthereforerecorded.Alpinetectonicshorteningstronglyaffectedthearea,withafirstEocenedeformation,followedbylaterNeogeneoverthrustingandstrike-slipmovements.
出版日期
2003年03月13日（中国Betway体育网页登陆平台首次上网日期，不代表论文的发表时间）
