During the last five years conodont faunas of 6 Carboniferous-Permian sections of the Eastern and Central Iran have been investigated.Recently fusulinids from these sections(Anarak,Zaladu,Halvan,Tangale -Mokhtar,Kaviz...During the last five years conodont faunas of 6 Carboniferous-Permian sections of the Eastern and Central Iran have been investigated.Recently fusulinids from these sections(Anarak,Zaladu,Halvan,Tangale -Mokhtar,Kaviz and Bage-Vang) were studied by E.Ja.Leven.The provincial Permian scale in the Tethys (Leven,1980) is based on fusulinids.The occurrence of fusulinids and conodonts in the same samples展开更多
The distribution of Lower Silurian conodonts from the sections on the Kozhym River was studied first by S.V. Melnikov.After additional studies of the Upper Ordovician-Lower Silurian strata,Oulodus? aff.nathani, Wallis...The distribution of Lower Silurian conodonts from the sections on the Kozhym River was studied first by S.V. Melnikov.After additional studies of the Upper Ordovician-Lower Silurian strata,Oulodus? aff.nathani, Walliserodus cf.curvatus,Panderodus sp.and Ozarkodina sp.were identified by P.M(a|¨)nnik in the Subpolar Urals.Studies of conodonts from the展开更多
文摘During the last five years conodont faunas of 6 Carboniferous-Permian sections of the Eastern and Central Iran have been investigated.Recently fusulinids from these sections(Anarak,Zaladu,Halvan,Tangale -Mokhtar,Kaviz and Bage-Vang) were studied by E.Ja.Leven.The provincial Permian scale in the Tethys (Leven,1980) is based on fusulinids.The occurrence of fusulinids and conodonts in the same samples
文摘The distribution of Lower Silurian conodonts from the sections on the Kozhym River was studied first by S.V. Melnikov.After additional studies of the Upper Ordovician-Lower Silurian strata,Oulodus? aff.nathani, Walliserodus cf.curvatus,Panderodus sp.and Ozarkodina sp.were identified by P.M(a|¨)nnik in the Subpolar Urals.Studies of conodonts from the
