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The Triassic metabasalts of Dudin Krs, near Kosovska Mitrovica, Serbia
Author(s) -
Emin Memovic,
Vladica Cvetković,
Vera Knezevic,
Guram Zakariadze
Publication year - 2003
Publication title -
geoloski anali balkanskog poluostrva
Language(s) - English
Resource type - Journals
eISSN - 2406-0747
pISSN - 0350-0608
DOI - 10.2298/gabp0301085m
Subject(s) - geology , rift , basalt , geochemistry , volcanic rock , flood basalt , volcano , petrology , paleontology , volcanism , structural basin , tectonics
This paper presents the geochemical characteristics of the metabasalts of Dudin Krš, near Kosovska Mitrovica. The Dudin Krš is the easternmost occurrence of Middle Triassic rift-related volcanic rocks in the Dinarides. Generally, these rocks show similarities to other Triassic volcanic rocks of the Dinarides. They are high-magnesian, ol and ne-normative basalts, with low Zr/Nb and medium/low Ti/Zr and Ti/Y ratios. They exhibit transitional geochemical characteristics, between E-MORB and subalkaline basalts of continental rift zones. Their presence and geochemical affinity is evidence of rifting processes along the continental slope of the Adria block during Middle Triassic

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