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Celestine deposits in the oligo-miocene Qom formation of the Abardej anticline, Central Iran: stratigraphic distribution, geochemistry, S-O-C isotopes and fluid inclusions
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DOI：10.1016/j.oregeorev.2026.107389.png)
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Abstract
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• Kazemabad, Abardej and Qaleh-Boland deposits hosted by carbonate and marl in the Qom Formation. • Diagenetic crystallization rhythmites (DCRs) are common textures in the celestine deposits of the Abardej anticline. • The geological, geometrical and geochemical features offered in this research strongly propose a sedimentary-diagenetic origin for Abardej anticline celestine deposits.
Keywords:
Celestine
Abardej: diagenesis
Qom formation
Central Iran
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