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Deposition of megabeds (megaturbidites) and sea-level change in a proximal part of Eocene-Miocene flysch of central Dalmatia (Croatia) (CROSBI ID 202049)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Marjanac, Tihomir Deposition of megabeds (megaturbidites) and sea-level change in a proximal part of Eocene-Miocene flysch of central Dalmatia (Croatia) // Geology (Boulder), 24 (1996), 6; 543-546. doi: 10.1130/0091-7613(1996)024<0543:DOMMAS>2.3.CO;2

Podaci o odgovornosti

Marjanac, Tihomir

engleski

Deposition of megabeds (megaturbidites) and sea-level change in a proximal part of Eocene-Miocene flysch of central Dalmatia (Croatia)

Some carbonate megabeds of the proximal part of Dalmatian Eocene-Miocene flysch basin (eastern Adriatic Sea) are underlain and overlain by conglomeratic fan-deltas, whereas thinner-bedded turbidites interfinger with fan-delta conglomerates. Fan deltas and interfingering turbidites are interpreted as deposited during lowstand(s) and early sea-level rise(s), whereas deposition of megabeds is attributed to periods of accelerated sea-level rises which aborted growth of fan deltas. Attribution of megabeds to periods of sea-level rise is based on the following observations: (1) they overlie some conglomeratic fan deltas, (2) skeletal and lithical debris in megabeds originated by subaerial weathering of older sediments, (3) their large thickness indicates considerable primary accumulation of debris and low frequency of flows. Sea-level changes inferred from megabeds are different from that of thinner classical turbidites, and distinction of the two is important for sequence stratigraphy in deep-marine sediments.

turbidites; sea-level change; Dalmatia; Croatia

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Podaci o izdanju

24 (6)

1996.

543-546

objavljeno

0091-7613

1943-2682

10.1130/0091-7613(1996)024<0543:DOMMAS>2.3.CO;2

Povezanost rada

Geologija

Poveznice
Indeksiranost