Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8911818 | Lithos | 2018 | 69 Pages |
Abstract
The detrital zircon age spectra suggest a Neoproterozoic ancestry of the Glaneck Metamorphic Suite, which was located west of the Arabian Nubian Shield, probably next to the Trans-Saharan Belt. The early Paleozoic evolution of the recent Seckau Complex shows similarities to basement units of the Southalpine Unit, parts of the Austroalpine Unit and the Tatric and Veporic units of the Central Western Carpathians.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Magdalena Mandl, Walter Kurz, Christoph Hauzenberger, Harald Fritz, Urs Klötzli, Ralf Schuster,