Writers : Vaezjavadi;Shahrabi;Pourlatifi
Refference : Geoscience Scientific Quartarly Journal,No.43_44
Publishing Year : 1381

Abstract :

Binalud Mountains are defined as a transitional zone between Central Iran and Alborz Mountains. It has a fairly thick sequence of sedimentary, metamorphic and plutonic rocks. The oldest deposits belong to Silurian age. In this paper Rhaetian Early Liassic deposits are studied which has more than 2000 m thickness. They are mostly included of phylitte, slate, sandstone, quartzite and thin-bedded limestones which is called as "Mashad Phyllites". In the study of 1:100000 map of Torghabeh several macrofossil are collected. Four plant macrofossil species are identified. They are Clathropteris p/alvphylla, Clathropteris sp., Thawnatopteris sp. and Otozarnites sp. According to their stratigraphical distribution Rhaetian .

Subject List : age