"K\u00F6ln" . "The Brunovistulian terrane represents a microcontinent of an enigmatic Proterozoic provenance that was located at the southern margin of Baltica in the early Paleozoic. During the Variscan orogeny, it represented the southern passive margin of Laurussia, in this respect resembling the Istanbul Zone to the east and the Avalonian terrane to the west. Nevertheless, the presence of a Silurian-Devonian back-arc basin cannot be excluded at the southermost margin of the terrane. The early Variscan phase was characterized the by the formation of Devonian extensional basins and WPA volcanic activity. The compressive phase is recorded in synorogenic flysch sedimentation, which shows a distinct polarity. The oldest flysch (Protivanov and Andelska Hora Fm.) contains clastic micas from early Paleozoic crystalline rocks that are assumed to be derived either from an active Brunovistulian margin, now covered by the Lugodanubian nappes, or from the terranes of Armorican affinity. The development of the Moravo-Silesian"@en . "Melichar, Rostislav" . . "K\u00F6ln" . "Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane" . . "3-934027-18-0" . . "[614408C8F6EB]" . "5"^^ . "503212" . . "Carboniferous Conference Cologne. From Platform to Basin, Sept. 4-10 2006. K\u00F6lner Forum f\u00FCr Geologie und Pal\u00E4ontologie, 15." . "The Brunovistulian terrane represents a microcontinent of an enigmatic Proterozoic provenance that was located at the southern margin of Baltica in the early Paleozoic. During the Variscan orogeny, it represented the southern passive margin of Laurussia, in this respect resembling the Istanbul Zone to the east and the Avalonian terrane to the west. Nevertheless, the presence of a Silurian-Devonian back-arc basin cannot be excluded at the southermost margin of the terrane. The early Variscan phase was characterized the by the formation of Devonian extensional basins and WPA volcanic activity. The compressive phase is recorded in synorogenic flysch sedimentation, which shows a distinct polarity. The oldest flysch (Protivanov and Andelska Hora Fm.) contains clastic micas from early Paleozoic crystalline rocks that are assumed to be derived either from an active Brunovistulian margin, now covered by the Lugodanubian nappes, or from the terranes of Armorican affinity. The development of the Moravo-Silesian" . "Tektonostratigrafick\u00FD v\u00FDvoj devonu a karbonu brunovistulick\u00E9ho ter\u00E1nu, \u010Cesk\u00E1 republika"@cs . . "2006-09-04+02:00"^^ . "stratigraphy; Brunovistulian terrane; Rhenohercynian zone; Variscan orogeny; tectonostratigraphy; Devonian; Carboniferous"@en . . "Z(MSM0021622412)" . . "Tektonostratigrafick\u00FD v\u00FDvoj devonu a karbonu brunovistulick\u00E9ho ter\u00E1nu, \u010Cesk\u00E1 republika"@cs . "\u0160pa\u010Dek, Petr" . "Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane"@en . . . . . . "Institut f\u00FCr Geologie und Mineralogie der Universit\u00E4t zu K\u00F6ln" . "RIV/00216224:14310/06:00017189" . . . . . . . "Tektonostratigrafick\u00FD v\u00FDvoj devonu a karbonu brunovistulick\u00E9ho ter\u00E1nu, \u010Cesk\u00E1 republika"@cs . "Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane"@en . . "Leichmann, Jarom\u00EDr" . "14310" . . . "RIV/00216224:14310/06:00017189!RIV08-MSM-14310___" . "2"^^ . . "53-54" . "Tectonostratigraphic development of the Devonian and Carboniferous in the Brunovistulian terrane" . . "Kalvoda, Ji\u0159\u00ED" . . "B\u00E1bek, Ond\u0159ej" . "5"^^ .