Geochronology of granitoids from Psunj and Papuk Mts., Croatia-Reference-Cited by-同舟云学术

Geochronology of granitoids from Psunj and Papuk Mts., Croatia

Published:2018-01-01 Issue:1 Volume:45 Page:198-210
ISSN:1897-1695
Container-title:Geochronometria
language:en
Short-container-title:

Author:

Horvat Marija¹,Klötzli Urs²,Jamičić Domagoj³,Buda György⁴,Klötzli Eva²,Hauzenberger Christoph⁵

Affiliation:

1. Croatian Geological Survey , Department of Geology , Sachsova 2, 10000 Zagreb , Croatia

2. University of Vienna , Department of Lithospheric Research , Althanstraße 14, A-1090 Vienna , Austria

3. Svetojanska 21, 10000 Zagreb , Croatia

4. Eötvös Lóránd University , Institute of Geology , Department of Mineralogy , Pázmány Péter sétány 1/c, H-1117 Budapest , Hungary

5. Karl-Franzens-University , Department of Earth Sciences , Universitätsplatz 2, 8010 Graz , Austria

Abstract

Abstract Detailed cathodoluminescence (CL) and back scattered electron (BSE) imaging of zircon crystals, coupled with in-situ U-Pb zircon dating by Laser Ablation Multi-Collector Inductively Coupled Plasma Mass Spectrometry (LA-MC-ICP-MS) were used to develop new insights into the evolution of a monzogranite from Omanovac Quarry (Psunj Mt.), and of monzogranites from Šandrovac Quarry and Kišeljevac Creek (Papuk Mt.), both located in the Slavonian Mountains (Croatia). U-Pb isotopic data yielded a concordia age of 380 ± 4 Ma for the monzogranite from Omanovac Quarry, and 382 ± 2 Ma and 383 ± 5 Ma for monzogranites from Šandrovac Quarry and Kišeljevac Creek. The results suggest Late Devonian magmatic activity.

Publisher

Walter de Gruyter GmbH

Subject

Earth and Planetary Sciences (miscellaneous)

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