Pregled bibliografske jedinice broj: 969365
Statistical analyses of Late Cretaceous clastic deposits from Mali Potok Creek (Medvednica Mt., Northern Croatia)
Statistical analyses of Late Cretaceous clastic deposits from Mali Potok Creek (Medvednica Mt., Northern Croatia) // Mathematical methods and terminology in geology 2018 / Malvić, Tomislav ; Velić, Josipa ; Rajić, Rajna (ur.).
Zagreb: Rudarsko-geološko-naftni fakultet Sveučilišta u Zagrebu, 2018. str. 87-93 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 969365 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Statistical analyses of Late Cretaceous clastic deposits from Mali Potok Creek (Medvednica Mt., Northern Croatia)
Autori
Sremac, Jasenka ; Kudrnovski, Davor ; Velić, Josipa ; Bošnjak, Marija ; Velić, Ivo
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Mathematical methods and terminology in geology 2018
/ Malvić, Tomislav ; Velić, Josipa ; Rajić, Rajna - Zagreb : Rudarsko-geološko-naftni fakultet Sveučilišta u Zagrebu, 2018, 87-93
ISBN
978-953-6923-40-3
Skup
2. hrvatski znanstveni skup iz geomatematike i nazivlja u geologiji
Mjesto i datum
Zagreb, Hrvatska, 06.10.2018
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Clastic deposits, statistics, Santonian-Campanian, Medvednica Mt., Croatia
Sažetak
Statistical analyses were applied to the Late Cretaceous clastic deposits exposed along the flanks of the Mali Potok creek in Medvednica Mt., as an auxiliary tool in order to help determining the source of pebbles, depositional processes and position within the sedimentary basin. Particularly interesting is the comparison of the conglomerate matrix with the overlying sandstone. Matrix grain size exhibits normal distribution, with most abundant fractions between 0.125 and 0.5 mm and sorting coefficient 2.14. Sandstones are grain- supported, well sorted, with coefficient value 1.55. Asymmetrical distribution, with domination of small-sized clasts between 0.032 and 0.125 mm in diameter characterizes these deposits. Such distribution is in concordance with interpretation of sandstones as synorogenic turbidites. Clastic succession from Mali Potok Creek can be well compared with contemporaneous deposits in the wider area, particularly with recently studied clastic succession in the vicinity of the Medvedgrad Castle.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb,
Hrvatski geološki institut,
Hrvatski prirodoslovni muzej,
Rudarsko-geološko-naftni fakultet, Zagreb
Profili:
Josipa Velić
(autor)
Ivo Velić
(autor)
Davor Kudrnovski
(autor)
Jasenka Sremac
(autor)
Marija Bošnjak Makovec
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Web of Science Core Collection (WoSCC)
- Conference Proceedings Citation Index - Science (CPCI-S)