Pregled bibliografske jedinice broj: 1280863
Košna conglomerates in the Velebit Mt., Croatia: particle composition, provenance and depositional environment
Košna conglomerates in the Velebit Mt., Croatia: particle composition, provenance and depositional environment // 36th IAS Dubrovnik Meeting of Sedimentology, Book of Abstracts / Vlahović, Igor ; Matešić, Darko (ur.).
Zagreb: Hrvatsko geološko društvo, 2023. str. 489-489 (poster, međunarodna recenzija, sažetak, znanstveni)
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Naslov
Košna conglomerates in the Velebit Mt., Croatia: particle composition, provenance and depositional environment
Autori
Fio Firi, Karmen ; Palatinuš, Iva ; Gobo, Katarina ; Marković, Frane ; Sremac, Jasenka
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
36th IAS Dubrovnik Meeting of Sedimentology, Book of Abstracts
/ Vlahović, Igor ; Matešić, Darko - Zagreb : Hrvatsko geološko društvo, 2023, 489-489
ISBN
978-953-6907-79-3
Skup
36th IAS Dubrovnik Meeting of Sedimentology
Mjesto i datum
Dubrovnik, Hrvatska, 12.06.2023. - 16.06.2023
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Košna conglomerates, Velebit Mt., Early Permian, Hercynian Mountains
Sažetak
In the vicinity of the ‘Košna voda’ spring in the Brušane area (Velebit Mt., Croatia), multicoloured Košna conglomerates attract attention due to their red matrix and clasts of various size and lithological composition (sandstones, limestones, chert and quartz). The conglomerates are poorly sorted, but locally show normal grading, imbricated clasts and stratified matrix, suggesting tractive particle transport. Sandstone clasts are classified as: lithic arenites, subarkoses and arkoses, with fragments of fusulinid foraminifera. Limestone clasts are mostly shallow-marine wackestones to packstones of Late Carboniferous/Early Permian age, with foraminifers, ostracods, echinoid and bryozoan fragments. Microcodium and calcispherae are also present in clasts, suggesting different sources and resedimentation. Based on field observations and conducted petrographic, ore microscopy and X-ray diffraction analyses, the Košna conglomerates are defined as Early Permian polymict clast-supported and matrix-supported conglomerates derived from the uplifted Hercynian Mountains and deposited and reworked in a shallow marine environment. Due to their structural and textural features, they are comparable with Late Paleozoic conglomerates from other areas in the Dinarides, Eastern and Southern Alps.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
HRZZ-IP-2019-04-7042 - Taložni paleobazeni, vodeni prolazi i migracije biote (SEDBAS) (Kovačić, Marijan, HRZZ - 2019-04) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski geološki institut
Profili:
Katarina Gobo
(autor)
Iva Palatinuš
(autor)
Karmen Fio Firi
(autor)
Jasenka Sremac
(autor)
Frane Marković
(autor)