Title : ( Provenance, palaeoclimate, and tectonic setting of the Shishtu-1 Formation (Late Devonian) in East-Central Iran: Based on geochemical evidence )
Authors: samane kianpour , Mohammad Khanehbad , Mohamad Hosein Mahmudy Gharaie , Sayyed Reza Moussavi Harami ,
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Abstract
The Shishtu-1 Formation in the Central Iran region developed during the Late Devonian with a succession of carbonate and siliciclastic rocks. The current study focuses on siliciclastic intervals to detect provenance, tectonic settings, palaeoclimatic conditions, and palaeogeographic reconstruction. Sandstones and shales were investigated separately in this study. According to petrographic and geochemical studies, the sandstones are quartzarenite and sublitharnite. The geochemical analysis revealed that SiO2, Al2O3, and Fe2O3 are the most abundant oxides in the samples of the study area. Also, trace elements such as Ba, Cr, Sr, V & Zr have a high concentration. .
Keywords
, Siliciclastic rocks, Shishtu-1 Formation, Late Devonian, Provenance, Tectonic setting.
@article{paperid:1106374,
author = {Kianpour, Samane and Khanehbad, Mohammad and Mahmudy Gharaie, Mohamad Hosein and Moussavi Harami, Sayyed Reza},
title = {Provenance, palaeoclimate, and tectonic setting of the Shishtu-1 Formation (Late Devonian) in East-Central Iran: Based on geochemical evidence},
journal = {Iranian Journal of Earth Science},
year = {2025},
volume = {18},
number = {2},
month = {July},
issn = {2008-8779},
pages = {27--39},
numpages = {12},
keywords = {Siliciclastic rocks; Shishtu-1 Formation; Late Devonian; Provenance; Tectonic setting.},
}
%0 Journal Article
%T Provenance, palaeoclimate, and tectonic setting of the Shishtu-1 Formation (Late Devonian) in East-Central Iran: Based on geochemical evidence
%A Kianpour, Samane
%A Khanehbad, Mohammad
%A Mahmudy Gharaie, Mohamad Hosein
%A Moussavi Harami, Sayyed Reza
%J Iranian Journal of Earth Science
%@ 2008-8779
%D 2025
