%0 Journal Article
%T 西南日本秋吉带石炭系高山(Ko-yama)灰岩群的石炭纪(Visean–Moscovian)牙形石序列
%A Keisuke ISHIDA
%A Sigeyuki SUZUKI
%A Noriyuki INADA
%A Shinji YAMASHITA
%J 地球学报
%D 2012
%R 10.3975/cagsb.2012.s1.14
%X TheCarboniferousconodontfaunalsuccessionofthelowerpartofKo-yamaLimestoneGroupwasstudied.TheconfirmedupperVisean–lowerMoscovianlithostratigraphyofthegroupischaracterizedbytheclasticcarbonateswithcommonassociationofthebasalticpyroclasticsandsomeintercalationofspicularchertbeds.ThefaunalsuccessionofGnathodussemiglaber(upperVisean),Gnathoduspraebilineatus–Lochrieamultinodosa(upperVisean),Lochrieaziegleri–Gnathodusgirtyigirtyis.l.(lowerSerpukhovian),Neoganthodussymmetricus–Idiognathodusprimulus(middle–upperBashkirian),andIdiognathoidesconvexus–Gondolellaclarki(lowerMoscovian)faunas,appearsinconcordancewiththelithostratigraphicorder.ThefaunasarecorrelativewiththosefromtheconodontzonesoftheHina,Atetsu,AkiyoshiandOmilimestonegroupsintheAkiyoshiBelt.TheVisean/SerpukhovianboundaryofthesectionwasrecognizedbytheFADofLochrieaziegleri.
%K conodont
%K Ko-yamaLimestone
%K Carboniferous
%K AkiyoshiBelt
%K SWJapan
%U http://www.cagsbulletin.com/dqxbcn/ch/reader/view_abstract.aspx?file_no=2012s114&flag=1