Journal of the Geological Society of India, ( ISI ), Volume (82), No (12), Year (2013-12) , Pages (701-711)

Title : ( depositional history and sequence stratigraphy of Tirgan Formation (Barremian-Aptian) in Central Kopet-Dagh, NE Iran )

Authors: M. Javanbakhat , S. Ghazi , Sayyed Reza Moussavi Harami , Asadollah Mahboubi ,

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Abstract

The Tirgan Formation (Barremian-Aptian) is exposed in the Kopet-Dagh in NE Iran. Two stratigraphic sections in Radkan and Chenaran were measured. Their thickness are 238m and 119 m respectively. This Formation in measured sections consists of three parts (including lower carbonate, middle limy shale-marl and upper carbonate rocks). Based on study of 164 thin sections, 15 carbonate and 2 siliciclastic lithofacies have been identified. Carbonate lithofacies are deposited in a ramp platformin fore shoal, shoal, lagoon and tidal flat environments. Sea level changes duringlower Cretaceous led to the formation ofdifferent large scale depositional sequences Radkan (two) and Chenaran (two) respectively.The present study highlight the reconstruction of tectonic history of the area during lower Cretaceous.

Keywords

, Lower Cretaceous, Tirgan Formation, Kopet-Dagh, Depositional sequence, Iran
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@article{paperid:1038102,
author = {M. Javanbakhat and S. Ghazi and Moussavi Harami, Sayyed Reza and Mahboubi, Asadollah},
title = {depositional history and sequence stratigraphy of Tirgan Formation (Barremian-Aptian) in Central Kopet-Dagh, NE Iran},
journal = {Journal of the Geological Society of India},
year = {2013},
volume = {82},
number = {12},
month = {December},
issn = {0016-7622},
pages = {701--711},
numpages = {10},
keywords = {Lower Cretaceous; Tirgan Formation; Kopet-Dagh; Depositional sequence; Iran},
}

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%0 Journal Article
%T depositional history and sequence stratigraphy of Tirgan Formation (Barremian-Aptian) in Central Kopet-Dagh, NE Iran
%A M. Javanbakhat
%A S. Ghazi
%A Moussavi Harami, Sayyed Reza
%A Mahboubi, Asadollah
%J Journal of the Geological Society of India
%@ 0016-7622
%D 2013

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