. . "NL - Nizozemsko" . "2"^^ . "Boundaries of mantle\u2013lithosphere domains in the Bohemian Massif as extinct exhumation channels for high-pressure rocks"@en . . . . "23" . "P(GA205/07/1088), P(GAP210/12/2381), P(IAA300120709), Z(AV0Z30120515)" . . "10.1016/j.gr.2012.07.005" . "Boundaries of mantle\u2013lithosphere domains in the Bohemian Massif as extinct exhumation channels for high-pressure rocks" . "3" . . "Boundaries of mantle\u2013lithosphere domains in the Bohemian Massif as extinct exhumation channels for high-pressure rocks" . . "Gondwana Research" . . "000315543400010" . "Babu\u0161ka, Vladislav" . "Bohemian Massif; mantle lithosphere domains; fossil olivine fabric; high pressure"@en . . "Five domains (microplates) have been recognized by seismic anisotropy in themantle lithosphere of the Bohemian Massif. The mantle domains correspond to major crustal units and each of the domains bears a consistent fossil olivine fabric formed before their Variscan assembly. The present-day mantle fabric indicates that this process consisted of at least three oceanic subductions, each followed by an underthrusting of the continental lithosphere. The seismic anisotropy does not detect remnants of the oceanic subductions, but it can trace boundaries of the preserved continental domains subsequently underthrust along the paths of previous oceanic subductions. The most robust continent\u2013continent collision was followed by westward underthrusting of the Brunovistulian mantle lithosphere, still detectable by seismic anisotropy more than 100 km beneath the Moldanubian mantle lithosphere."@en . . . . . "Five domains (microplates) have been recognized by seismic anisotropy in themantle lithosphere of the Bohemian Massif. The mantle domains correspond to major crustal units and each of the domains bears a consistent fossil olivine fabric formed before their Variscan assembly. The present-day mantle fabric indicates that this process consisted of at least three oceanic subductions, each followed by an underthrusting of the continental lithosphere. The seismic anisotropy does not detect remnants of the oceanic subductions, but it can trace boundaries of the preserved continental domains subsequently underthrust along the paths of previous oceanic subductions. The most robust continent\u2013continent collision was followed by westward underthrusting of the Brunovistulian mantle lithosphere, still detectable by seismic anisotropy more than 100 km beneath the Moldanubian mantle lithosphere." . "63780" . . "[F77304080577]" . "Boundaries of mantle\u2013lithosphere domains in the Bohemian Massif as extinct exhumation channels for high-pressure rocks"@en . . . "1342-937X" . "RIV/67985530:_____/13:00379337!RIV13-AV0-67985530" . . "Plomerov\u00E1, Jaroslava" . "15"^^ . "RIV/67985530:_____/13:00379337" . "2"^^ . . . . .