Subduction of a rifted passive continental margin: the Pohorje case of Eastern Alps–constraints from geochronology and geochemistry

Swiss Journal of Geosciences

Table 4 P-T conditions of EGU from previous research

Igneous Rocks	Age	P (GPa)	T (℃)	References
Mica schists	320–280	0.6–0.8	650	Schulz 2017
Mica schists	275 ± 25	0.24–0.42	530	Schuster 2015
Garnet mica schists	269.2 ± 6.2	0.46	540	Thöni and Miller 2009)
Mica gneiss	250–270	0.38–0.4	590–600	Habler and Thöni 2001)
Mica gneiss	249 ± 3	0.38–0.65	600–650	Schorn 2018
Eclogites	90	2.4	700–730	Miller et al. 2007
Garnet lherzolite	87–93	4	900	De Hoog et al. 2009
Eclogites	87–95	2.4–2.5	640–740	Thöni et al. 2008a, Table 1
Eclogites	90	2.4	630–650	Miller et al. 2007
Eclogites	90.7 ± 1	2.1	750	Miller et al. 2005a
Eclogite facies		2.4	650–730	Miller 1990
Gneiss	92.5	2.2–2.7	700–800	Janák et al. 2009
Gneiss	92–95	3.5	800–850	Janák et al. 2015
Kyanite-eclogite	92	3.0–3.7	710–940	Vrabec et al. 2012
Eclogite	94–95	2.2	630–740	Thöni et al. 2008b
Eclogites	Cretaceous	1.8–2.5	630–700	Sassi et al. 2004
Garnet peridotites	Cretaceous	3.4–4	890–960	Janák et al. 2006
Kyanite eclogites	Cretaceous	3.0–3.1	760–825	Janák et al. 2004
Eclogites	–	2.5	750–800	Hauzenberger et al. 2016
Garnet lherzolite	91.6 ± 4.1	4	900	Sandmann et al. 2016