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Granulites, partial melting and the rheology of the lower crust
BROWN, M.; SCHULMANN, K.; WHITE, R. W.
Geodynamic regimes of subduction under an active margin: effects of rheological weakening by fluids and melts
GERYA, T. V.; MEILICK, F. I.
Coeval thrusting and extension during lower crustal ductile flow – implications for exhumation of high-grade metamorphic rocks
JAMIESON, R. A.; BEAUMONT, C.
Model of syn-convergent extrusion of orogenic lower crust in the core of the Variscan belt: implications for exhumation of high-pressure rocks in large hot orogens
FRANĚK, J.; SCHULMANN, K.; LEXA, O.; TOMEK, Č.; EDEL, J.-B.
Heat sources and trigger mechanisms of exhumation of HP granulites in Variscan orogenic root
LEXA, O.; SCHULMANN, K.; JANOUŠEK, V.; ŠTÍPSKÁ, P.; GUY, A.; RACEK, M.
Origin of felsic granulite microstructure by heterogeneous decomposition of alkali feldspar and extreme weakening of orogenic lower crust during the Variscan orogeny
FRANĚK, J.; SCHULMANN, K.; LEXA, O.; ULRICH, S.; ŠTÍPSKÁ, P.; HALODA, J.; TÝCOVÁ, P.
On the interpretation of retrograde reaction textures in granulite facies rocks
WHITE, R. W.; POWELL, R.
Progress in linking accessory mineral growth and breakdown to major mineral evolution in metamorphic rocks: a thermodynamic approach in the Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2-ZrO2 system
KELSEY, D. E.; POWELL, R.