Palaeoenvironment and basin architecture of the Lower Jurassic Ab-Haji Formation, east-central Iran

The Lower Jurassic Ab-Haji Formation of the Kalmard, Tabas and Lut blocks, east-central Iran, has been studied using an integrated stratigraphic-sedimentologic approach. The Ab-Haji Formation is mostly composed of greenish sandstones and siltstones and locally contains thin coal seams. Four well e...

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Autores principales: Salehi, Mohammad Ali, Moussavi-Harami, Reza, Mahboubi, Asadollah, Rahimi, Behnam
Formato: article artículo publishedVersion
Lenguaje:Inglés
Publicado: Instituto de Fisiografía y Geología. Facultad de Ciencias Exactas, Ingeniería y Agrimensura. Universidad Nacional de Rosario 2015
Materias:
Acceso en línea:http://hdl.handle.net/2133/5142
http://hdl.handle.net/2133/5142
Aporte de:
id I15-R121-2133-5142
record_format dspace
institution Universidad Nacional de Rosario
institution_str I-15
repository_str R-121
collection Repositorio Hipermedial de la Universidad Nacional de Rosario (UNR)
language Inglés
orig_language_str_mv eng
topic Early Jurassic
Lithofacies
Facies association
Palaeoenvironment
East-central Iran
spellingShingle Early Jurassic
Lithofacies
Facies association
Palaeoenvironment
East-central Iran
Salehi, Mohammad Ali
Moussavi-Harami, Reza
Mahboubi, Asadollah
Rahimi, Behnam
Palaeoenvironment and basin architecture of the Lower Jurassic Ab-Haji Formation, east-central Iran
topic_facet Early Jurassic
Lithofacies
Facies association
Palaeoenvironment
East-central Iran
description The Lower Jurassic Ab-Haji Formation of the Kalmard, Tabas and Lut blocks, east-central Iran, has been studied using an integrated stratigraphic-sedimentologic approach. The Ab-Haji Formation is mostly composed of greenish sandstones and siltstones and locally contains thin coal seams. Four well exposed sections were measured and studied in order to identify lithofacies and facies associations and to interpret the palaeoenvironment. This formation reaches a thickness up to 350 m in northern Tabas Block but may locally be reduced to few tens of meters or even missing. Field studies have led to the recognition of sixteen lithofacies grouped into five facies associations: fluvial plain, coastal plain, delta front, prodelta and shallow siliciclastic shelf. Reconstruction of the palaeogeography of east-central Iran marks a west–east continental-to-marine gradient. Thickness variations, lateral facies changes and basal unconformity of the siliciclastic rocks of the Ab-Haji Formation on the Kalmard, Tabas and Lut blocks show palaeo-relief on the fault-bounded Yazd Block in the west and the Shotori Swell at the eastern edge of the Tabas Block. The pattern of thickness variations and rapid EW facies changes is best explained by a tectonic model showing large tilted fault blocks in an extensional basin. The obtained results are important for palaeogeographic and palaeoenvironmental reconstructions of the east-central Iran since its sediments record the geodynamic history of this region, as well as an even larger area, during and in the aftermath of the main Cimmerian event, from the beginning of the Early Jurassic.
format article
artículo
publishedVersion
author Salehi, Mohammad Ali
Moussavi-Harami, Reza
Mahboubi, Asadollah
Rahimi, Behnam
author_facet Salehi, Mohammad Ali
Moussavi-Harami, Reza
Mahboubi, Asadollah
Rahimi, Behnam
author_sort Salehi, Mohammad Ali
title Palaeoenvironment and basin architecture of the Lower Jurassic Ab-Haji Formation, east-central Iran
title_short Palaeoenvironment and basin architecture of the Lower Jurassic Ab-Haji Formation, east-central Iran
title_full Palaeoenvironment and basin architecture of the Lower Jurassic Ab-Haji Formation, east-central Iran
title_fullStr Palaeoenvironment and basin architecture of the Lower Jurassic Ab-Haji Formation, east-central Iran
title_full_unstemmed Palaeoenvironment and basin architecture of the Lower Jurassic Ab-Haji Formation, east-central Iran
title_sort palaeoenvironment and basin architecture of the lower jurassic ab-haji formation, east-central iran
publisher Instituto de Fisiografía y Geología. Facultad de Ciencias Exactas, Ingeniería y Agrimensura. Universidad Nacional de Rosario
publishDate 2015
url http://hdl.handle.net/2133/5142
http://hdl.handle.net/2133/5142
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