Eocene Incised Valley Fill Clastics of the Island of Rab, Facies and Sequence Architecture (CROSBI ID 52362)
Prilog u knjizi | izvorni znanstveni rad
Podaci o odgovornosti
Marjanac, Tihomir ; Marjanac, Ljerka
engleski
Eocene Incised Valley Fill Clastics of the Island of Rab, Facies and Sequence Architecture
The Rab and Pag island Eocene sediments have common general stratigraphic composition, which comprises so-called Foraminiferal limestones, which overlie bauxites, Transitional beds, and the succession of quartz-rich clastics. The Eocene clastics on both islands bear significant differences which are the focus of this paper. In the first place, the major difference are their depositional environments and operating sedimentary processes. The largest part of the Rab clastics was deposited in an incised-valley tide-dominated setting, whereas Pag island clastics were deposited in storm-dominated shallow shoreface setting. The paper describes individual facies, facies associations and provides reconstruction of sequence-stratigraphic architecture.
Eocene, stratigraphy, sequence stratigraphy, facies, sea-level change
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Podaci o prilogu
28-51.
objavljeno
Podaci o knjizi
Excursion Guidebook. Easteren Adriatic Eocene clastic successions: Islands of Rab and Pag.
Marjanac, Tihomir
Zagreb: Prirodoslovno-matematički fakultet Sveučilišta u Zagrebu
2014.
978-953-6076-34-5