. . . "10" . "The Brunovistulian Terrane (BT) is a fragment of northern Gondwana margin regarded as a part of Avalonian group of terranes (KALVODA 1995). The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentation of Gondwana. It is assumed that BT was amalgamated to Baltica along the TESZ in Lower Paleozoic and during the Variscan orogeny was a southern promontory of Laurussia. The Devonian extension is assumed to be connected with intraplate stresses due to the collision of the Brunovistulian promontory with Moldanubian and Armorican Superterrane. Orogeny leads to rifting at high angle to the compression direction and rifts form first near the collision site and propagate later away from it. As a consequence, the amount of total extension and correlatively, the magnitude of the total subsidence, is commonly greatest near the suture and decreases away from it. The Moravosilesian basin bears features of both impactogen and strike-slip rela"@en . "0"^^ . "1"^^ . "0"^^ . . . "Paleozoic evolution of the Moravosilesian Basin"@en . "1210-9606" . . "1"^^ . . "14310" . "1"^^ . "RIV/00216224:14310/00:00002603" . "The Brunovistulian Terrane (BT) is a fragment of northern Gondwana margin regarded as a part of Avalonian group of terranes (KALVODA 1995). The lithological record of the Cambrian marine sediments may indicate the extension and rifting connected with the fragmentation of Gondwana. It is assumed that BT was amalgamated to Baltica along the TESZ in Lower Paleozoic and during the Variscan orogeny was a southern promontory of Laurussia. The Devonian extension is assumed to be connected with intraplate stresses due to the collision of the Brunovistulian promontory with Moldanubian and Armorican Superterrane. Orogeny leads to rifting at high angle to the compression direction and rifts form first near the collision site and propagate later away from it. As a consequence, the amount of total extension and correlatively, the magnitude of the total subsidence, is commonly greatest near the suture and decreases away from it. The Moravosilesian basin bears features of both impactogen and strike-slip rela" . . "Paleozoic evolution of the Moravosilesian Basin"@en . "Geolines" . "Paleozoic evolution of the Moravosilesian Basin" . . . "CZ - \u010Cesk\u00E1 republika" . . "721080" . "Paleozoic evolution of the Moravosilesian Basin" . . . "40" . . "P(GA205/99/1640), Z(MSM 143100004)" . "4" . "[D4767D537AD1]" . . . "RIV/00216224:14310/00:00002603!RIV/2002/MSM/143102/N" . . . "Kalvoda, Ji\u0159\u00ED" . . "Brunovistulian terrane, extension, rifting, Devonian, Carboniferous"@en .