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Information Journal Paper

Title

STRATIGRAPHY AND PALEONTOLOGY OF THE UPPER CARBONIFEROUS-PERMIAN ROCKS IN ZALADU SECTION AND ITS COMPARISON WITH OTHER AREAS IN IRAN

Pages

 Start Page 45 | End Page 56

Abstract

 A complete succesion of the Late Ghzelian-Asselian rocks crops out at the Zaladu section in Ozbak-kuh area. Three members have been identified in this section. Member 1 consists of conglomerate, sandstone, as well as green and red shales interbedded with sandy limestone.Member 2 is limestone. Member 3 consists of thick to massive dolomite. Index FUSULINIDs of the Late Ghezelian including, Rauserites, Rushenzevites, Schellwienia and Asselian genera like Pseudoschwagerina, Rugosofusulina have been recognized in member 2. Therefore, on the basis of these findings the Carboniferous-Permian boundary is considered to be continious in this area. This complete succesion of the Late Ghezelian-Asselian rocks is introduced for the first time in Iran. The succesion is similar to the other areas in southern Tethyan basin.

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