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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
(
Avtor
),
ID
Dolenec, Matej
(
Avtor
),
ID
Grum Verdinek, Luna
(
Avtor
),
ID
Zavašnik, Janez
(
Avtor
)
PDF - Predstavitvena datoteka,
prenos
(11,39 MB)
MD5: C3EBF5C14571E76594CDDE76A0F91F62
URL - Izvorni URL, za dostop obiščite
https://www.sciencedirect.com/science/article/pii/S0009281925001096
Galerija slik
Izvleček
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.
Jezik:
Angleški jezik
Ključne besede:
evaporites
,
gypsum
,
barite
,
celestine
,
geochemistry
,
critical elements
Vrsta gradiva:
Članek v reviji
Tipologija:
1.01 - Izvirni znanstveni članek
Organizacija:
NTF - Naravoslovnotehniška fakulteta
Status publikacije:
Objavljeno
Različica publikacije:
Objavljena publikacija
Leto izida:
2025
Št. strani:
12 str.
Številčenje:
Vol. 85, iss. 4, art. 126354
PID:
20.500.12556/RUL-182779
UDK:
55
ISSN pri članku:
0009-2819
DOI:
10.1016/j.chemer.2025.126354
COBISS.SI-ID:
258757379
Datum objave v RUL:
22.05.2026
Število ogledov:
242
Število prenosov:
240
Metapodatki:
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Objavi na:
Gradivo je del revije
Naslov:
Chemie der Erde
Skrajšan naslov:
Chem. Erde
Založnik:
Gustav Fischer Verlag
ISSN:
0009-2819
COBISS.SI-ID:
25211136
Licence
Licenca:
CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:
http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:
To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.
Projekti
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Številka projekta:
P1-0195
Naslov:
Geookolje in geomateriali
Financer:
ARIS - Javna agencija za znanstvenoraziskovalno in inovacijsko dejavnost Republike Slovenije
Številka projekta:
N1-0164
Naslov:
Geobiokemijski cikel molibdena v kamninah in sedimentih
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