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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

(Mrinjek, Ervin ; Pencinger Vili) 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 // Guidebook, 5th ProGEO International Symposium, Rab Island, Croatia / (Marjanac, Tihomir) (ur.). Zagreb: ProGEO-Hrvatska, 2008. str. 105-125

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

Povezanost rada

Geologija