Post-Variscan metamorphism in the Apuseni and Rodna Mountains (Romania): evidence from Sm–Nd garnet and U–Th–Pb monazite dating

Author:

Reiser Martin Kaspar,Săbău GavrilORCID,Negulescu Elena,Schuster Ralf,Tropper Peter,Fügenschuh Bernhard

Funder

Austrian Science Fund

Romanian Executive Unit for Financing Research and Higher Education

Publisher

Springer Science and Business Media LLC

Subject

Geology

Reference131 articles.

1. Antić, M. D., Kounov, A., Trivić, B., Spikings, R., & Wetzel, A. (2017). Evidence of Variscan and Alpine tectonics in the structural and thermochronological record of the central Serbo-Macedonian Massif (south-eastern Serbia). International Journal of Earth Sciences, 106(5), 1665–1692.

2. Antić, M. D., Kounov, A., Trivić, B., Wetzel, A., Peytcheva, I., & von Quadt, A. (2016). Alpine thermal events in the central Serbo-Macedonian Massif (southeastern Serbia). International Journal of Earth Sciences, 105(5), 1485–1505.

3. Anton, D.C. (1999). Petrographical, Geochemical and Isotopic Study of Mt. Mare Granitoids, North Apuseni Mountains: Evolution of Peraluminous Magma. Ph.D. dissertation, Tokyo University, Japan, pp. 176.

4. Árkai, P. (2001). Alpine regional metamorphism in the main tectonic units of Hungary: A review. Acta Geologica Hungarica, 44(2–3), 329–344.

5. Árkai, P., Bérczi-Makk, A., & Balogh, K. (2000). Alpine low-T prograde metamorphism in the post-Variscan basement of the Great Plain, Tisza Unit (Pannonian Basin, Hungary). Acta Geologica Hungarica, 43(1), 43–63.

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