Geološki Anali Balkanskoga Poluostrva (Jan 2003)

The Triassic metabasalts of Dudin Krš, near Kosovska Mitrovica, Serbia

  • Memović Emin,
  • Cvetković Vladica D.,
  • Knežević Vera,
  • Zakariadze Guram

DOI
https://doi.org/10.2298/GABP0301085M
Journal volume & issue
Vol. 2003, no. 65
pp. 85 – 91

Abstract

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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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