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Quaternary clastics of Jablanac cove in the foothills of the Velebit Mt. (CROSBI ID 751891)

Druge vrste radova | ostali članci/prilozi

Marjanac, Ljerka ; Marjanac, Tihomir Quaternary clastics of Jablanac cove in the foothills of the Velebit Mt. // Harold Readinǵs IAS Lecture Tour ́99 - Field-trip guidebook: Some Carbonate and Clastic Successions. 1999.

Podaci o odgovornosti

Marjanac, Ljerka ; Marjanac, Tihomir

engleski

Quaternary clastics of Jablanac cove in the foothills of the Velebit Mt.

Jablanac and its environs are composed of Paleogene-Neogene limestones and breccias. Quaternary sediments were deposited unconformably over thic Cenozoic basement. Quaternary sediments of Jablanac environs are represented by colluvial slope deposits, which are overlain by alluvial fans. The deposition acted in enclosed circular depression, which was opened towards the sea by later tectonical deformation. The debis was transported from the present-day Velebit channel. Very similar Quaternary sediments are exposed also on the Island of Rab, in Mišnjak Cove, but the paleotransport direction is opposite to the one of Jablanac. The source of sediment was evidently in the Velebit Channel area.

Quaternary; clastics; glaciation; Velebit Mt.

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Podaci o izdanju

Harold Readinǵs IAS Lecture Tour ́99 - Field-trip guidebook: Some Carbonate and Clastic Successions

1999.

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objavljeno

Povezanost rada

Geologija