scholarly journals Facies Analysis, Depositional Environment and Cyclostratigraphy of the Lower Permian deposits Chili Formation in the Kalmard Block, East Central Iran (Godar-e-Gachal section)

2014 ◽  
Vol 7 (10) ◽  
pp. 1588-1602
Author(s):  
Javad Shahraki
Keyword(s):  
Depositional Environment ◽  
Facies Analysis ◽  
Central Iran ◽  
Lower Permian ◽  
East Central

scholarly journals Facies Analysis, Depositional Environment of the Lower Permian Deposits of Chili Formation in Kalmard Block, Eastern Central Iran (Darin Section)

2015 ◽  
Vol 05 (08) ◽  
pp. 539-551 ◽  
Author(s):  
Javad Shahraki ◽  
Mohammad Javad Javdan ◽  
Seyed Mahmood Pahlavan Hashemi ◽  
Mohsen Jami ◽  
Mahdiyeh Nastooh ◽  
...  
Keyword(s):  
Depositional Environment ◽  
Facies Analysis ◽  
Central Iran ◽  
Lower Permian

scholarly journals Facies Analysis and Depositional Environment of Upper Permian Rocks in Darin Section, East-Central Iran

2017 ◽  
Vol 07 (03) ◽  
pp. 242-256 ◽  
Author(s):  
Bibi Haniyeh Emraninasab ◽  
Mohammad Hossein Adabi ◽  
Mahmood Reza Majidifard ◽  
Nader Kohansal Ghadimvand ◽  
Sohei Erfani
Keyword(s):  
Depositional Environment ◽  
Facies Analysis ◽  
Central Iran ◽  
Upper Permian ◽  
East Central

Facies analysis of a large-scale Jurassic shelf-lagoon: the Kamar-e-Mehdi Formation of east-central Iran

Facies ◽  
2009 ◽  
Vol 56 (1) ◽  
pp. 59-87 ◽  
Author(s):  
Markus Wilmsen ◽  
Franz T. Fürsich ◽  
Kazem Seyed-Emami ◽  
Mahmoud R. Majidifard ◽  
Massoud Zamani-Pedram
Keyword(s):  
Large Scale ◽  
Facies Analysis ◽  
Central Iran ◽  
East Central

scholarly journals Facies Interpretation, Depositional Environment and Sequence Stratigraphy of the Gachal Formation in the Madbeiki Section, Kalmard Block, East Central Iran

2016 ◽  
Vol 06 (06) ◽  
pp. 439-458 ◽  
Author(s):  
Soheil Erfani ◽  
Mohammad Hossein Adabi ◽  
Mahmood Reza Majidifard ◽  
Nader Kohansal Ghadimvand
Keyword(s):  
Sequence Stratigraphy ◽  
Depositional Environment ◽  
Central Iran ◽  
East Central

Facies Analysis and Sequence Stratigraphy of the Qal'eh Dokhtar Formation (Middle-Upper Jurassic) in the West of Boshrouyeh, East Central Iran

2017 ◽  
Vol 91 (5) ◽  
pp. 1797-1819 ◽  
Author(s):  
Mahnaz SABBAGH BAJESTANI ◽  
Asadollah MAHBOUBI ◽  
Reza MOUSSAVI-HARAMI ◽  
Ihsan AL-AASM ◽  
Mehdi NADJAFI
Keyword(s):  
Sequence Stratigraphy ◽  
Facies Analysis ◽  
Upper Jurassic ◽  
Central Iran ◽  
The West ◽  
East Central

Stratigraphy, facies analysis and ammonite fauna of the Qal'eh Dokhtar Formation (Middle - Upper Jurassic) at the type locality west of Boshrouyeh (east-central Iran).

2000 ◽  
Vol 216 (1) ◽  
pp. 35-66 ◽  
Author(s):  
Gerhard Schairer ◽  
Kazem Seyed-Emami ◽  
Franz T. Fürsich ◽  
Baba Senowbari-Daryan ◽  
Seyed Ali Aghanabati ◽  
...  
Keyword(s):  
Facies Analysis ◽  
Upper Jurassic ◽  
Central Iran ◽  
Type Locality ◽  
East Central

scholarly journals Depositional environment of the Bagh-e-Vang Formation – the only occurrence of upper Lower Permian in Iran

Geologos ◽  
2021 ◽  
Vol 27 (1) ◽  
pp. 1-14
Author(s):  
Bizhan Yousefi Yegane ◽  
A.J. van Loon Tom ◽  
Sakine Arefi Fard ◽  
Mohammad Mehdi Farahpour ◽  
Safoora Yasbolaghi Sharahi
Keyword(s):  
Field Data ◽  
Depositional Environment ◽  
Carbonate Platform ◽  
Lower Permian ◽  
Early Permian ◽  
East Central ◽  
Tethys Ocean ◽  
Thin Section Analysis ◽  
Intertidal Mud Flats ◽  
Section Analysis

Abstract A transgression of the Tethys Ocean occurred in east central Iran, like in other areas of the Tethys Ocean, around the Yakhtashian/Bolorian (regional chronostratigraphical units corresponding with the Artinskian/Kungurian of the Early Permian) transition. This led to the development of a carbonate platform that is represented in the Shirgesht area on the northern part of the Tabas Block by the Bagh-e-Vang Formation, which constitutes the only known sedimentary unit from the late Early Permian in Iran. Field data and thin-section analysis indicate deposition on a carbonate ramp with barriers separating a lagoonal area with intertidal mud flats from the open-marine environment. The overall transgressive development is indicated by the presence of open-marine sediments on top of the barrier and lagoonal sediments.

Sign in / Sign up

Export Citation Format

Share Document