%0 Journal Article
%T CambriantracefossilsandwormlikeimpressionsfromtheTalGroup,Gopi-Chand-KaMahalsection,Mussooriesyncline,LesserHimalaya
%A Birendra P. SINGH
%J µØÇòѧ±¨
%D 2009
%R 10.3975/cagsb.2009.s1.30
%X CambriantracefossilsandwormlikeimpressionsaredescribedhereinfromthethreestratigraphicunitsofTalGroupofrocksexposedalongthetrackfromMaldeotatoDhaulagiriinGopi-Chand-KaMahalsec-tion,Mussooriesyncline.Theupper10mthicksand-stonesuccession(ArenaceousMember)ofDeo-Ka-TibbaFormation(lowerTalGroup)containshighden-sityandlowdiversitySkolithospiperock.TheSko-lithospiperockinsandstonesuccessionofArenaceousMember(Deo-Ka-TibbaFormation)indicatesshallowmarineconditionundersandshiftingenvironmentofdeposition.Higherinthesuccession,incalcareousMember(Deo-Ka-TibbaFormation),Cruzianaichno-faciesoccursinassociationwithMonomorphichnus,PlanolitesandPaleophycus.
%K EarlyCambrian
%K TalGroup
%K LesserHimalaya
%K PaleoolenusZone
%K DrepanuroidesZone
%U http://www.cagsbulletin.com/dqxbcn/ch/reader/view_abstract.aspx?file_no=2009S130&flag=1