High-temperature overprint in (U) HPM rocks exhumed from subduction zones; A product of isothermal decompression or a consequence of slab break-off (slab …
SW Faryad, SJ Cuthbert - Earth-Science Reviews, 2020 - Elsevier
This paper presents and discusses petrological observations from high-to ultrahigh-pressure
(U) HP metamorphic terrains in relation to existing geophysical and numerical models for …
(U) HP metamorphic terrains in relation to existing geophysical and numerical models for …
The moldanubian zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities
In order to portray the main differences and similarities between the Northeastern Variscan
segments (French Massif Central (FMC), Vosges, Black Forest and Bohemian Massif (BM)) …
segments (French Massif Central (FMC), Vosges, Black Forest and Bohemian Massif (BM)) …
Ultrapotassic magmatism in the heyday of the Variscan Orogeny: the story of the Třebíč Pluton, the largest durbachitic body in the Bohemian Massif
V Janoušek, P Hanžl, M Svojtka, JM Hora… - International Journal of …, 2020 - Springer
The Třebíč Pluton (TP) comprises plutonic rocks of the 'durbachite series', ie, ultrapotassic
biotite–amphibole quartz melasyenites–melagranites with conspicuous K-feldspar …
biotite–amphibole quartz melasyenites–melagranites with conspicuous K-feldspar …
Late orogenic heating of (ultra) high pressure rocks: slab rollback vs. slab breakoff
E Sizova, C Hauzenberger, H Fritz, SW Faryad… - Geosciences, 2019 - mdpi.com
Some (ultra) high-pressure metamorphic rocks that formed during continental collision
preserve relict minerals, indicating a two-stage evolution: first, subduction to mantle depths …
preserve relict minerals, indicating a two-stage evolution: first, subduction to mantle depths …
Isotopic compositions of sulfides in exhumed high‐pressure terranes: implications for sulfur cycling in subduction zones
JB Walters, AM Cruz‐Uribe… - Geochemistry …, 2019 - Wiley Online Library
Subduction is a key component of Earth's long‐term sulfur cycle; however, the mechanisms
that drive sulfur from subducting slabs remain elusive. Isotopes are a sensitive indicator of …
that drive sulfur from subducting slabs remain elusive. Isotopes are a sensitive indicator of …
First finding of microdiamond, coesite and other UHP phases in felsic granulites in the Moldanubian Zone: Implications for deep subduction and a revised geodynamic …
Heavy mineral fractions and polished thin sections from felsic granulites from the
Moldanubian Zone of the Bohemian Massif were thoroughly studied by means of Raman …
Moldanubian Zone of the Bohemian Massif were thoroughly studied by means of Raman …
[HTML][HTML] Reconstruction of the mid-Devonian HP-HT metamorphic event in the Bohemian Massif (European Variscan belt)
Mid-Devonian high-pressure (HP) and high-temperature (HT) metamorphism represents an
enigmatic early phase in the evolution of the Variscan Orogeny. Within the Bohemian Massif …
enigmatic early phase in the evolution of the Variscan Orogeny. Within the Bohemian Massif …
Altenberg–Teplice Caldera sourced Westphalian fall tuffs in the central and western Bohemian Carboniferous basins (eastern Variscan belt)
Timing of magmatic activity of the late-Variscan Altenberg–Teplice Caldera was rather
vaguely constrained. In this paper, we present five new laser ablation inductively coupled …
vaguely constrained. In this paper, we present five new laser ablation inductively coupled …
Ultrapotassic dykes in the Moldanubian Zone and their significance for understanding of the post-collisional mantle dynamics during Variscan orogeny in the …
We report mineral textures, geochemistry and age relations of two ultrapotassic dykes from a
dyke swarm in the Western part of the Moldanubian Zone at contact to the Teplá-Barrandian …
dyke swarm in the Western part of the Moldanubian Zone at contact to the Teplá-Barrandian …
Implication of corona formation in a metatroctolite to the granulite facies overprint of HP–UHP rocks in the Moldanubian Zone (Bohemian Massif)
Corona and inclusion textures of a metatroctolite at the contact between felsic granulite and
migmatites of the Gföhl Unit from the Moldanubian Zone provide evidence of the magmatic …
migmatites of the Gföhl Unit from the Moldanubian Zone provide evidence of the magmatic …