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Pregled bibliografske jedinice broj: 661669

Magmatic provenance and diagenesis of Miocene tuffs from the Dinaride Lake System (the Sinj Basin, Croatia)


Šegvić, Branimir; Mileusnić, Marta; Aljinović, Dunja; Vranjković, Alan; Mandić, Oleg; Pavelić, Davor; Dragičević, Ivan; Ferreiro Mählmann, Rafael
Magmatic provenance and diagenesis of Miocene tuffs from the Dinaride Lake System (the Sinj Basin, Croatia) // European journal of mineralogy, 26 (2014), 1; 83-101 doi:10.1127/0935-1221/2013/0025-2350 (međunarodna recenzija, članak, znanstveni)


CROSBI ID: 661669 Za ispravke kontaktirajte CROSBI podršku putem web obrasca

Naslov
Magmatic provenance and diagenesis of Miocene tuffs from the Dinaride Lake System (the Sinj Basin, Croatia)

Autori
Šegvić, Branimir ; Mileusnić, Marta ; Aljinović, Dunja ; Vranjković, Alan ; Mandić, Oleg ; Pavelić, Davor ; Dragičević, Ivan ; Ferreiro Mählmann, Rafael

Izvornik
European journal of mineralogy (0935-1221) 26 (2014), 1; 83-101

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
Sinj basin; smectitic tuffs; Dinaride Lake System; trachyandesitic arc-related volcanism; clay mineral alterations; Croatia

Sažetak
This study presents new insights on the provenance, genesis, and post-depositional history of the Miocene pyroclastic tuffaceous layers (~18 and ~15 Ma) preserved in argillaceous sediments and interbedded within the lacustrine sedimentary succession of the Sinj Basin in central Dalmatia (Dinaride Lake System, Croatia). Analysed tuffs are classified as smectitic tuffs composed of three main lithotypes: (a) vitriclastic tuffs, (b) altered vitriclastic tuff, and (c) tuffaceous clays. The high field strength element (HFSE) contents of the tuffs, as well as the major- element chemistry of the vitric glass, suggests that parental magmas were high-K calc-alkaline trachyandesites. This is consistent with the distinctive heavy-mineral assemblages including clinopyroxene, zircon and apatite, identified in less evolved parental magmas, and biotite in more evolved ones. The regional geological data imply the placement of the parent volcano(es) outside the Dinaric Alps region, most probably in an area corresponding to the present-day southern margin of the Pannonian Basin where volcanic rock suites of analogous age and geochemistry are reported. Minor compaction and high permeability of coarse ash-sized pyroclastic material allowed for extensive in situ diagenetic clay mineral formation dominated by smectite. Following discrete smectite formation, the illite-smectite mixed-layering took place as a result of mica/illite alteration or surface illitization processes. On the basis of the very-low grade alteration of volcanic materials, it is suggested that diagenesis operated in an open hydrologic system of a lacustrine environment.

Izvorni jezik
Engleski

Znanstvena područja
Geologija



POVEZANOST RADA


Projekti:
195-0000000-3202 - Definicija facijesa u bazi Dinarida i usporedba sa širim tetiskim prostorom (Aljinović, Dunja, MZOS ) ( POIROT)
195-1951126-3205 - Tektonomagmatska korelacija fragmentirane oceanske litosfere u Dinaridima (Mileusnić, Marta, MZOS ) ( POIROT)
195-1951293-0237 - Stratigrafska i geomatematička istraživanja naftnogeoloških sustava u Hrvatskoj (Velić, Josipa, MZOS ) ( POIROT)
195-1951293-2703 - Neogenski kopneni okoliši Panonskog bazena i krških područja (Pavelić, Davor, MZOS ) ( POIROT)
195-1953068-2704 - Dinarski krš: geološka evolucija, mineralne sirovine, paleotla i tla (Durn, Goran, MZOS ) ( POIROT)

Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb

Poveznice na cjeloviti tekst rada:

doi dx.doi.org www.ingentaconnect.com

Citiraj ovu publikaciju:

Šegvić, Branimir; Mileusnić, Marta; Aljinović, Dunja; Vranjković, Alan; Mandić, Oleg; Pavelić, Davor; Dragičević, Ivan; Ferreiro Mählmann, Rafael
Magmatic provenance and diagenesis of Miocene tuffs from the Dinaride Lake System (the Sinj Basin, Croatia) // European journal of mineralogy, 26 (2014), 1; 83-101 doi:10.1127/0935-1221/2013/0025-2350 (međunarodna recenzija, članak, znanstveni)
Šegvić, B., Mileusnić, M., Aljinović, D., Vranjković, A., Mandić, O., Pavelić, D., Dragičević, I. & Ferreiro Mählmann, R. (2014) Magmatic provenance and diagenesis of Miocene tuffs from the Dinaride Lake System (the Sinj Basin, Croatia). European journal of mineralogy, 26 (1), 83-101 doi:10.1127/0935-1221/2013/0025-2350.
@article{article, year = {2014}, pages = {83-101}, DOI = {10.1127/0935-1221/2013/0025-2350}, keywords = {Sinj basin, smectitic tuffs, Dinaride Lake System, trachyandesitic arc-related volcanism, clay mineral alterations, Croatia}, journal = {European journal of mineralogy}, doi = {10.1127/0935-1221/2013/0025-2350}, volume = {26}, number = {1}, issn = {0935-1221}, title = {Magmatic provenance and diagenesis of Miocene tuffs from the Dinaride Lake System (the Sinj Basin, Croatia)}, keyword = {Sinj basin, smectitic tuffs, Dinaride Lake System, trachyandesitic arc-related volcanism, clay mineral alterations, Croatia} }
@article{article, year = {2014}, pages = {83-101}, DOI = {10.1127/0935-1221/2013/0025-2350}, keywords = {Sinj basin, smectitic tuffs, Dinaride Lake System, trachyandesitic arc-related volcanism, clay mineral alterations, Croatia}, journal = {European journal of mineralogy}, doi = {10.1127/0935-1221/2013/0025-2350}, volume = {26}, number = {1}, issn = {0935-1221}, title = {Magmatic provenance and diagenesis of Miocene tuffs from the Dinaride Lake System (the Sinj Basin, Croatia)}, keyword = {Sinj basin, smectitic tuffs, Dinaride Lake System, trachyandesitic arc-related volcanism, clay mineral alterations, Croatia} }

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


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