GEOLOGY AND THE AGE OF THE MASHHAD PHYLLITES IN DIZBAD AREA IN THE BINALUD MOUNTAIN

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VAEZ JAVADI F.; POUR LATIFI A.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Journal: GEOSCIENCES Year:2002 | Volume:11 | Issue:43-44 Page(s): 80-87

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Information Journal Paper

Title

GEOLOGY AND THE AGE OF THE MASHHAD PHYLLITES IN DIZBAD AREA IN THE BINALUD MOUNTAIN

Author(s)

VAEZ JAVADI F. | POUR LATIFI A. | Issue Writer Certificate

Keywords

BINALUDQ2

MASHHAD PHYLLITESQ4

RHAETIAN -EARLY LIASQ4

PLANT MACROFOSSILQ3

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 platyphylla, Clathropteris sp. Thaumatopteris sp. and Otozamites sp. According to their strati graphical distribution Rhaetian Early Liassic age can be suggested for this assemblage.

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APA: Copy

VAEZ JAVADI, F., & POUR LATIFI, A.. (2002). GEOLOGY AND THE AGE OF THE MASHHAD PHYLLITES IN DIZBAD AREA IN THE BINALUD MOUNTAIN. GEOSCIENCES, 11(43-44), 80-87. SID. https://sid.ir/paper/31335/en

Vancouver: Copy

VAEZ JAVADI F., POUR LATIFI A.. GEOLOGY AND THE AGE OF THE MASHHAD PHYLLITES IN DIZBAD AREA IN THE BINALUD MOUNTAIN. GEOSCIENCES[Internet]. 2002;11(43-44):80-87. Available from: https://sid.ir/paper/31335/en

IEEE: Copy

F. VAEZ JAVADI, and A. POUR LATIFI, “GEOLOGY AND THE AGE OF THE MASHHAD PHYLLITES IN DIZBAD AREA IN THE BINALUD MOUNTAIN,” GEOSCIENCES, vol. 11, no. 43-44, pp. 80–87, 2002, [Online]. Available: https://sid.ir/paper/31335/en

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