The Benkovac Stone – a building stone from the Promina Beds: A Late Eocene heterolithic succession of storm-dominated shelf deposits with highly diverse trace fossils (CROSBI ID 551512)
Prilog sa skupa u zborniku | ostalo
Podaci o odgovornosti
(Mrinjek, Ervin ; Pencinger Vili)
engleski
The Benkovac Stone – a building stone from the Promina Beds: A Late Eocene heterolithic succession of storm-dominated shelf deposits with highly diverse trace fossils
The Benkovac Stone Unit is about 100 m thick and consists of carbonate sandstones (up to 35 cm thick, but mainly thinner) interbedded with finer-grained calcareous deposits. Its Late Eocene age was established on the basis of large benthic foraminifera (nummulitids, discocyclinids) and small pelagic globigerinids. Benkovac Stone Unit consists of the offshore transition deposits of a storm-dominated, microtidal shelf variously affected by oscillatory waves and sediment-laden geostrophic currents.
shelf; shoreface; offshore transition zone; tempestites; hummocky cross-lamination; combined flow; trace fossils; northern Dalmatia
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Podaci o prilogu
105-125.
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
5th ProGEO International Symposium
ostalo
01.10.2008-05.10.2008
Rab, Hrvatska