The Promina Beds in Canyon of Krka River and Bribirske Mostine (CROSBI ID 551492)
Prilog sa skupa u zborniku | ostalo
Podaci o odgovornosti
Mrinjek, Ervin
engleski
The Promina Beds in Canyon of Krka River and Bribirske Mostine
The Canyon Krka and northwestern part of basin revealed several transgressive and regressive systems tracts (FSST, LST, HST) during underfilled and fulfilled phases is and one low- and one high- accommodation systems tracts during overfilled phase. The regressive systems tracts are composed of various gravely delta to braided-plain facies and sandy to gravely beach and shoreface facies whereas fine-sandy inner shelf and muddy outer shelf facies are dominant characteristics of transgressive systems tracts. The low- and one high- accommodation systems tracts are exclusively composed of gravelly to sandy channel braided and flood plain facies. The systems tracts show significant facies changes in their strike direction as well.
gravely delta; gravely braided-plain; gravely beach; sandy shoreface; muddy outer shelf; Canyon Krka; Promina Beds northern Dalmatia
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nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
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Podaci o prilogu
37-77.
2008.
objavljeno
Podaci o matičnoj publikaciji
Guidebook, 5th ProGEO International Symposium, Rab Island, Croatia
(Marjanac, Tihomir)
Zagreb: ProGEO-Hrvatska
953-6076-15-2
Podaci o skupu
th 5 ProGEO International Symposium
ostalo
01.10.2008-05.10.2008
Rab, Hrvatska