Pregled bibliografske jedinice broj: 57947
Albian-Cenomanian arenites overlying Dinaric platform carbonates contain detritus derived from continental and ophiolitic rocks
Albian-Cenomanian arenites overlying Dinaric platform carbonates contain detritus derived from continental and ophiolitic rocks // Abstracts PANCARDI 2000 / Tomljenović, Bruno ; Balen, Dražen ; Saftić, Bruno (ur.).
Zagreb: Hrvatsko geološko društvo, 2000. str. 28-29 (poster, domaća recenzija, sažetak, znanstveni)
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Naslov
Albian-Cenomanian arenites overlying Dinaric platform carbonates contain detritus derived from continental and ophiolitic rocks
Autori
Crnjaković, Marta ; Babić, Ljubomir ; Zupanič, Jožica
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Abstracts PANCARDI 2000
/ Tomljenović, Bruno ; Balen, Dražen ; Saftić, Bruno - Zagreb : Hrvatsko geološko društvo, 2000, 28-29
Skup
PANCARDI 2000
Mjesto i datum
Dubrovnik, Hrvatska, 01.10.2000. - 03.10.2000
Vrsta sudjelovanja
Poster
Vrsta recenzije
Domaća recenzija
Ključne riječi
Cretaceous; Albian; detritus; provenance; deformation; Dinarides
Sažetak
Albian-Cenomanian sediments of the inner marginal portion of carbonate Dinarides in northwesten Croatia are represented by turbidites and pelagites. We have studied heavy-mineral associations and non-carbonate particle composition from Albian-Cenomanian arenites in order to obtain data on relevant source rocks. The heavy mineral associations are highly dominated by the ultrastable minerals. However, chromspinel grains make 6-24 percent. Non-carbonate paticles include lithoclasts of low-grade metamorphic, and subordinately sediments, volcanics and mafic/ultramafic rocks. These data reflect a pre-Albian deformation in the areas situated to the NE of the basin.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
