U-Pb zircon age of the youngest magmatic activity in the High Tatra granites (Central Western Carpathians)

Author(s)
Jolanta Burda, Aleksandra Gaweda, Urs Kloetzli
Abstract

Detailed cathodoluminescence (CL) imaging of zircon crystals, coupled with Laser Ablation Multi-Collector Inductively Coupled Plasma Mass Spectrometry (LA-MC-ICP-MS) U-Pb zircon dating was used to develop new insights into the evolution of granitoids from the High Tatra Mountains. The zircon U-Pb results show two distinct age groups (350±5 Ma and 337±6 Ma) recorded from cores and rims domains, respectively. Obtained results point that the last magmatic activity in the Tatra granitoid intrusion occurred at ca. 330 Ma. The previously suggested age of 314 Ma reflects rather the hydrothermal activity and Pb-loss, coupled with post-magmatic shearing.

Organisation(s)
Department of Lithospheric Research
External organisation(s)
University of Silesia in Katowice
Journal
Geochronometria
Volume
40
Pages
134-144
No. of pages
11
ISSN
1733-8387
DOI
https://doi.org/10.2478/s13386-013-0106-9
Publication date
06-2013
Peer reviewed
Yes
Austrian Fields of Science 2012
105101 General geology
Keywords
Portal url
https://ucrisportal.univie.ac.at/en/publications/4e36555f-ba86-479d-996f-4896a228198c