Pregled bibliografske jedinice broj: 1262230
The Miocene Western Balkan lithium-boron metallogenic zone
The Miocene Western Balkan lithium-boron metallogenic zone // Mineralium deposita, 58 (2023), 639-658 doi:10.1007/s00126-022-01151-x (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1262230 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
The Miocene Western Balkan lithium-boron
metallogenic zone
Autori
Borojević Šoštarić, Sibila ; Brenko, Tomislav
Izvornik
Mineralium deposita (0026-4598) 58
(2023);
639-658
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Lithium-boron mineralization ; Extensional setting ; Li-bearing granitic rocks ; Miocene lacustrine basins ; Sava-Vardar zone ; Izmir-Ankara-Erzincan zone
Sažetak
The Western Balkan lithium-boron metallogenic zone can be traced for 1500 km, extending subparallel to the Sava-Vardar and Western Vardar zones toward its Turkish counterpart, the Izmir-Ankara-Erzincan zone. Common features are: (1) lithium-boron mineralization is hosted in Lower-Middle Miocene extensional lacustrine basins ; (2) lacustrine series consisting of fine-grained siliciclastic sediments and scarce evaporites with intercalations of volcaniclastics, tuff, or travertine indicating syndepositional volcanic activity ; (3) lacustrine basins that are usually normal-fault-controlled extensional grabens, with the fault system probably acting as a major fluid pathway ; (4) northernmost sodium borate/borosilicate deposits (Jadar, Valjevo, Rekovac ; with jadarite, borax, probertite, searlesite) gradually transition to calcium borate deposits southward (Jarandol-Piskanja, Pobrđe ; with colemanite ± ulexite) ; (5) Oligocene/Miocene granitic rocks from the westernmost part of the zone host pegmatite and greisen occurrences with surface lithium anomalies of 0.02–0.08 wt% Li2O extending for several km2 ; (6) igneous Li enrichment by fractionation processes is indicated for some younger (?Early/mid-Miocene) peraluminous granite plutons ; (7) the formation of the lacustrine basins and associated Li-B mineralization was contemporaneous with the emplacement of the younger phase of Li-bearing granitic intrusions and exhumation of metamorphic core complexes which provided the large-scale heat flow for hydrothermal systems and syngenetic Li-B mineralization.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
EK-H2020-18036 - Innovative targeting & processing of W-Sn-Ta-Li ores: towards EU's self-supply (iTARG3T) (Borojević Šoštarić, Sibila, EK - EIT RawMaterials KAVA Call 5) ( CroRIS)
Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus