Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)

Bedded radiolarites of Mt. Kalnik are of Carnian-Norian age, while similar rocks of Mt. Medvednica are of Late Ladinian - Carnian age, as determined on the basis of radiolarian assemblages. Radiolarites from Mt. Kalnik concordantly rest upon the pillow-lavas, or are interbedded with them. Their foot...

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Main Authors: Josip Halamić, Špela Goričan
Format: Article
Language:English
Published: Croatian Geological Survey 2010-11-01
Series:Geologia Croatica
Subjects:
Online Access:http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/372
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spelling doaj-52ada5beefed48b8b60705fdb8465f432020-11-25T00:33:03ZengCroatian Geological SurveyGeologia Croatica1330-030X1333-48752010-11-0148212914610.4154/GC.1995.10274Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)Josip Halamić0Špela Goričan1Croatian Geological SurveyIvan Rakovec Institute of PalaentologyBedded radiolarites of Mt. Kalnik are of Carnian-Norian age, while similar rocks of Mt. Medvednica are of Late Ladinian - Carnian age, as determined on the basis of radiolarian assemblages. Radiolarites from Mt. Kalnik concordantly rest upon the pillow-lavas, or are interbedded with them. Their footwall at Mt. Medvednica is not known, due to tectonic reduction. The sedimentary rocks described were deposited from low-density turbidity currents, therefore representing fine-grained turbidites. They were deposited closely below, and partially above the CCD. Results of petrological, sedimentological and geochemical investigations indicate sedimentation under terrigenous influence with contemporaneous hydrothermal activity. The studied sections are correlated with the nearest outcrops of Triassic radiolarites associated with basic effusive rocks, i.e. with the Vardar Zone and the Meliata Unit.http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/372Triassic, Radiolarites, Meliata Basin, Vardar Basin, Mt. Kalnik, Mt. Medvednica, Croatia
collection DOAJ
language English
format Article
sources DOAJ
author Josip Halamić
Špela Goričan
spellingShingle Josip Halamić
Špela Goričan
Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)
Geologia Croatica
Triassic, Radiolarites, Meliata Basin, Vardar Basin, Mt. Kalnik, Mt. Medvednica, Croatia
author_facet Josip Halamić
Špela Goričan
author_sort Josip Halamić
title Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)
title_short Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)
title_full Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)
title_fullStr Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)
title_full_unstemmed Triassic Radiolarites from Mts. Kalnik and Medvednica (Northwestern Croatia)
title_sort triassic radiolarites from mts. kalnik and medvednica (northwestern croatia)
publisher Croatian Geological Survey
series Geologia Croatica
issn 1330-030X
1333-4875
publishDate 2010-11-01
description Bedded radiolarites of Mt. Kalnik are of Carnian-Norian age, while similar rocks of Mt. Medvednica are of Late Ladinian - Carnian age, as determined on the basis of radiolarian assemblages. Radiolarites from Mt. Kalnik concordantly rest upon the pillow-lavas, or are interbedded with them. Their footwall at Mt. Medvednica is not known, due to tectonic reduction. The sedimentary rocks described were deposited from low-density turbidity currents, therefore representing fine-grained turbidites. They were deposited closely below, and partially above the CCD. Results of petrological, sedimentological and geochemical investigations indicate sedimentation under terrigenous influence with contemporaneous hydrothermal activity. The studied sections are correlated with the nearest outcrops of Triassic radiolarites associated with basic effusive rocks, i.e. with the Vardar Zone and the Meliata Unit.
topic Triassic, Radiolarites, Meliata Basin, Vardar Basin, Mt. Kalnik, Mt. Medvednica, Croatia
url http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/372
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