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Pliocene Alluvial Sediments in the Drava Depression pf the Virovotica-Slatina Area, Northern Croatia (CROSBI ID 126160)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Mrinjek, Ervin ; Sremac, Jasenka ; Velić, Josipa Pliocene Alluvial Sediments in the Drava Depression pf the Virovotica-Slatina Area, Northern Croatia // Geologia Croatica, 59 (2006), 1; 65-84-x

Podaci o odgovornosti

Mrinjek, Ervin ; Sremac, Jasenka ; Velić, Josipa

engleski

Pliocene Alluvial Sediments in the Drava Depression pf the Virovotica-Slatina Area, Northern Croatia

Clastic sediments in the vicinity of Virovitica (Northern Croatia) consists of gravels, sands, silt clays and marls. Gravels with discontinuous sheet-like geometry are typical for an alluvial fan system. The most abundant sediment, quartz rich sand, originates from a sandy braided river system. Silt, clays, and marls were deposited in the flood plain. They contain fossil macroflora indicative of moderate climate conditions, including maidenhair leaves (Ginkgo), the presence of which suggests that these sediments were deposited before Pleistocene glaciation.

Sheet floww; Alluvial fan; Sandy braided river system; Fossil flora; Drava river depression; Northern Croatia; Pliocene.

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Podaci o izdanju

59 (1)

2006.

65-84-x

objavljeno

1330-030X

Povezanost rada

Geologija

Indeksiranost