%0 Journal Article
%T 泰国东南部Rayong省Klaeng地区的中?晚泥盆世放射虫
%A Yoshihito KAMATA
%A Miyako KATO
%A Katsumi UENO
%A Akira MIYAHIGASHI
%A Thasinee CHAROENTITIRAT
%A Apsorn SARDSUD
%J 地球学报
%D 2012
%R 10.3975/cagsb.2012.s1.17
%X TectonicsubdivisionofmainlandThailandhasbeendiscussedbymeansofPaleozoicandMesozoicstratigraphy,micropaleontologyrepresentedbyfo-raminiferalandradiolarianbiostratigraphyandpaleo-biogeography,tectonicsettingsofgranitoids,andul-tramaficrocksthataredistinctiveofsuturelines.Re-cently,Ueno(2002)andUenoandCharoentitilat(2011)proposedanewtectonicschemeofmainlandThailandanddivideditintothreegeotectonicunits:theSibu-masuBlock,SukhothaiZone,andIndochinaBlockfromwesttoeast,whichareseparatedbytheMaeYuanFault,theChiangRaiTectonicLine,andtheNan–UttaraditSuture,respectively.InNorthernThai-land,moreover,thepeculiarInthanonZoneisrecog-nizedintheeasternpartoftheSibumasuBlock,wherePaleo-Tethyanoceanicrocksarewidelydistributedastectonicslices.ThesegeotectonicsubdivisionsinNorthernThailandarerelativelyclear.However,thetectonicsubdivisionsofCentralandSoutheastThai-landhavenotbeenwelldocumentedandarestillcon-troversialbecausethereisshortofinformationaboutbasementrocksinthoseareas.Inthiscircumstance,wehaveexaminedPaleozoictoMesozoicstratigraphy,lithology,andradiolarianagesofsiliceousrocksdis-tributedinSoutheastThailandtoclarifythegeotec-tonicbelongingsofthisareaandthesouthernexten-sionsofgeotectonicunitsconsistingofNorthernThailand.Inthecourseofthisresearch,wecouldob-tainMiddletoLateDevonianradiolariansfromwell-beddedsiliceousrocksdistributedinsouthwestofKlaeng,RayongProvince.Inthisstudy,wereportlithologyandageoftheradiolaria-bearingrocksanddiscusstheirstratigraphyandgeologicalcorrelationnearbytheKlaengregion.
%K Radiolarian
%K Klaeng
%K SoutheastThailand
%K Devonian
%U http://www.cagsbulletin.com/dqxbcn/ch/reader/view_abstract.aspx?file_no=2012s117&flag=1