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Mineralogical and geochemical significance of secondary burial-related barite and celestine : evidence from Late Paleozoic evaporites in the Karawanke Mountains (Slovenia)
ID Šoster, Aleš (Author), ID Dolenec, Matej (Author), ID Grum Verdinek, Luna (Author), ID Zavašnik, Janez (Author)

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Abstract
The evaporites in the Karawanke Mountains (northwestern Slovenia) are hosted in a structurally complex lithological sequence, intercalated between Carboniferous-Permian and Permo-Triassic rocks. These evaporites are primarily composed of gypsum, with minor amounts of anhydrite, dolomite, and barite-celestine. Geochemically, the evaporites are characterized by elevated Sr (2000–2700 mg kg$^{−1}$) and low Ba (210–400 mg kg$^{−1}$) contents, reflecting the contrasting solubility behaviors of these elements in low-temperature syngenetic environments. Thermal dehydration, induced by peak burial temperatures ranging from 190 to 260 °C facilitated the transformation of gypsum to anhydrite. Subsequent cooling below the anhydrite stability threshold enabled gradual rehydration, accounting for the coexistence of both minerals. Thermal alteration also mobilized trace elements from the evaporites, which precipitated as secondary celestine and barite through dissolution-reprecipitation mechanisms, producing compositionally zoned fracture infills. The observed zoning, transitioning from Ba-rich to Sr-rich endmembers, likely reflects shifts in temperature, solubility and the chemical reactivity of evaporite-derived brine. Sulfur isotope analyses reveal δ$^{34}$S values of +11.8 to +13.7 ‰ for the evaporitic sulfates, showing minimal variation and only a small difference relative to coexisting sulfides. This small isotopic offset indicates nearly complete sulfate reduction under high-temperature conditions, consistent with thermal alteration inferred from burial temperatures. These geochemical and isotopic results put forward not only the thermal and diagenetic evolution of the Karawanke evaporites but also their broader significance as minor reservoirs of strontium, a critical element with growing industrial and technological importance.

Language:English
Keywords:evaporites, gypsum, barite, celestine, geochemistry, critical elements
Work type:Article
Typology:1.01 - Original Scientific Article
Organization:NTF - Faculty of Natural Sciences and Engineering
Publication status:Published
Publication version:Version of Record
Year:2025
Number of pages:12 str.
Numbering:Vol. 85, iss. 4, art. 126354
PID:20.500.12556/RUL-182779 This link opens in a new window
UDC:55
ISSN on article:0009-2819
DOI:10.1016/j.chemer.2025.126354 This link opens in a new window
COBISS.SI-ID:258757379 This link opens in a new window
Publication date in RUL:22.05.2026
Views:226
Downloads:237
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Record is a part of a journal

Title:Chemie der Erde
Shortened title:Chem. Erde
Publisher:Gustav Fischer Verlag
ISSN:0009-2819
COBISS.SI-ID:25211136 This link opens in a new window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Projects

Funder:ARRS - Slovenian Research Agency
Project number:P1-0195
Name:Geookolje in geomateriali

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:N1-0164
Name:Geobiokemijski cikel molibdena v kamninah in sedimentih

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