%0 Journal Article
%T 西南日本秋吉带石炭系高山(Ko-yama)灰岩群的褶皱构造
%A Noriyuki INADA
%A Shigeyuki SUZUKI
%A Keisuke ISHIDA
%A Shinji YAMASHITA
%J 地球学报
%D 2012
%R 10.3975/cagsb.2012.s1.13
%X ThestudyareaislocatedinKawakami-cho,OkayamaPrefecture,whichisoccupiedbyLowerCarboniferoustoMiddlePermianKo-yamaLimestoneGroup(Yokoyamaetal.,1979),PermianYoshiiGroup(Sanoetal.,1987)andTriassicNariwaGroup(Tera-oka,1959).TheNariwaGroupunconformablycoversthePaleozoicsuccessions(Otoh,1985).Thesesucces-sionsbelongtotheAkiyoshiBelt.TheKo-yamaLimestoneGroupiscomposedmainlyofmassivelimestone,withbasicvolcanicrocks,acidictuffandchert.Thegroupwasdatedbyforaminiferandfusu-linidasLowerCarboniferoustoMiddlePermian(Yo-koyamaetal.,1979).
%K foldedstructure
%K Ko-yamaLimestone
%K Carboniferous
%K AkiyoshiBelt
%U http://www.cagsbulletin.com/dqxbcn/ch/reader/view_abstract.aspx?file_no=2012s113&flag=1