Podrobnosti záznamu

Klíčové slovo
    Thickened
Článek
    Carboniferous exhumation of thickened lower crust through wedge tectonics and subsequent lateral spreading in the middle crust: Moldanubian zone of the Bohemian Massif
    Carboniferous exhumation of thickened lower crust through wedge tectonics and subsequent lateral spreading in the middle crust: Moldanubian zone of the Bohemian Massif
    Contrasting Early Carboniferous field geotherms - evidence for accretion of a thickened orogenic root and subducted Saxothuringian crust (Central European Variscides)
    Contrasting Early Carboniferous field geotherms: evidence for accretion of a thickened orogenic root and subducted Saxothuringian crust (Central European Variscides)
    Decoupling near the moho: weakening beneath rigid mantle or lower crustal layers in thickened mountain roots and extensional zones
    Extrusion tectonics due to thermal softening of a thickened crustal root: The Bohemian Massif in Lower Carboniferous times
    Late-Variscan Extensional collapse of the thickened Moldanubian crust in the southern Bohemia
    Lower Carboniferous lift tectonics in the Bohemian Massif: a special kind of gravitational collapse in thickened orogenic crust
    Rapid exhumation and cooling of the thickened crust: evidence from the granulite clasts within the Upper Visean Conglomerates (Rhenohercynikum).
    Structural and metamorphic record of exhumation of the thickened lower crust in the hot orogenic root (NE Moldanubian domain, Bohemian Massif)
    Structural and metamorphic record of exhumation of the thickened lower crust in the hot orogenic root (Bohemian Massif)
    Structural and metamorphic record of exhumation of the thickened lower crust in the hot orogenic root (NE Moldanubian domain, Bohemian Massif)
    Thermal and mechanical interactions during exhumation of orogenic lower crust in thickened crustal root (Bohemian Massif)
    Thermal evolution of the orogenic lower crust during exhumation within a thickened Moldanubian root of the Variscan belt of Central Europe
    Thermal evolution of the orogenic lower crust during exhumation within a thickened Moldanubian root of the Variscan belt of Central Europe
    Thermally softened continental crust as precursor to thickened orogenic belts
    Thermally softened continental extensional zones (arcs and rifts) as precursors to thickened orogenic zones
    What drives remelting of thickened continental crust in the Bohemian Massif?