Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems

The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Franke, Wolfgang [verfasserIn] Żelaźniewicz, Andrzej [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc

Übergeordnetes Werk:	Enthalten in: Gondwana research - Amsterdam [u.a.] : Elsevier, 1997, 124, Seite 351-377
Übergeordnetes Werk:	volume:124 ; pages:351-377

DOI / URN:	10.1016/j.gr.2023.06.012

Katalog-ID:	ELV065448057

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650		4	\|a Variscan bohemian massif
650		4	\|a Plate-tectonic and geodynamic evolution
650		4	\|a Formation and exhumation of (ultra)-high-grade metamorphic rocks
650		4	\|a Anorogenic heating
650		4	\|a Bohemian arc
700	1		\|a Żelaźniewicz, Andrzej \|e verfasserin \|4 aut
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allfields	10.1016/j.gr.2023.06.012 doi (DE-627)ELV065448057 (ELSEVIER)S1342-937X(23)00174-0 DE-627 ger DE-627 rda eng 550 VZ Franke, Wolfgang verfasserin aut Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed. Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc Żelaźniewicz, Andrzej verfasserin aut Enthalten in Gondwana research Amsterdam [u.a.] : Elsevier, 1997 124, Seite 351-377 Online-Ressource (DE-627)504859692 (DE-600)2213685-X (DE-576)259273449 1342-937X nnns volume:124 pages:351-377 GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 124 351-377
spelling	10.1016/j.gr.2023.06.012 doi (DE-627)ELV065448057 (ELSEVIER)S1342-937X(23)00174-0 DE-627 ger DE-627 rda eng 550 VZ Franke, Wolfgang verfasserin aut Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed. Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc Żelaźniewicz, Andrzej verfasserin aut Enthalten in Gondwana research Amsterdam [u.a.] : Elsevier, 1997 124, Seite 351-377 Online-Ressource (DE-627)504859692 (DE-600)2213685-X (DE-576)259273449 1342-937X nnns volume:124 pages:351-377 GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 124 351-377
allfields_unstemmed	10.1016/j.gr.2023.06.012 doi (DE-627)ELV065448057 (ELSEVIER)S1342-937X(23)00174-0 DE-627 ger DE-627 rda eng 550 VZ Franke, Wolfgang verfasserin aut Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed. Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc Żelaźniewicz, Andrzej verfasserin aut Enthalten in Gondwana research Amsterdam [u.a.] : Elsevier, 1997 124, Seite 351-377 Online-Ressource (DE-627)504859692 (DE-600)2213685-X (DE-576)259273449 1342-937X nnns volume:124 pages:351-377 GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 124 351-377
allfieldsGer	10.1016/j.gr.2023.06.012 doi (DE-627)ELV065448057 (ELSEVIER)S1342-937X(23)00174-0 DE-627 ger DE-627 rda eng 550 VZ Franke, Wolfgang verfasserin aut Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed. Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc Żelaźniewicz, Andrzej verfasserin aut Enthalten in Gondwana research Amsterdam [u.a.] : Elsevier, 1997 124, Seite 351-377 Online-Ressource (DE-627)504859692 (DE-600)2213685-X (DE-576)259273449 1342-937X nnns volume:124 pages:351-377 GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 124 351-377
allfieldsSound	10.1016/j.gr.2023.06.012 doi (DE-627)ELV065448057 (ELSEVIER)S1342-937X(23)00174-0 DE-627 ger DE-627 rda eng 550 VZ Franke, Wolfgang verfasserin aut Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed. Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc Żelaźniewicz, Andrzej verfasserin aut Enthalten in Gondwana research Amsterdam [u.a.] : Elsevier, 1997 124, Seite 351-377 Online-Ressource (DE-627)504859692 (DE-600)2213685-X (DE-576)259273449 1342-937X nnns volume:124 pages:351-377 GBV_USEFLAG_U GBV_ELV SYSFLAG_U GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 124 351-377
language	English
source	Enthalten in Gondwana research 124, Seite 351-377 volume:124 pages:351-377
sourceStr	Enthalten in Gondwana research 124, Seite 351-377 volume:124 pages:351-377
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc
dewey-raw	550
isfreeaccess_bool	false
container_title	Gondwana research
authorswithroles_txt_mv	Franke, Wolfgang @@aut@@ Żelaźniewicz, Andrzej @@aut@@
publishDateDaySort_date	2023-01-01T00:00:00Z
hierarchy_top_id	504859692
dewey-sort	3550
id	ELV065448057
language_de	englisch
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author	Franke, Wolfgang
spellingShingle	Franke, Wolfgang ddc 550 misc Variscan bohemian massif misc Plate-tectonic and geodynamic evolution misc Formation and exhumation of (ultra)-high-grade metamorphic rocks misc Anorogenic heating misc Bohemian arc Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems
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topic_title	550 VZ Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems Variscan bohemian massif Plate-tectonic and geodynamic evolution Formation and exhumation of (ultra)-high-grade metamorphic rocks Anorogenic heating Bohemian arc
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title	Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems
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title_full	Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems
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title_sort	variscan evolution of the bohemian massif (central europe): fiction, facts and problems
title_auth	Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems
abstract	The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed.
abstractGer	The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed.
abstract_unstemmed	The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed.
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title_short	Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems
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up_date	2024-07-06T23:03:52.113Z
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fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">ELV065448057</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20231106093007.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">231106s2023 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.gr.2023.06.012</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV065448057</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S1342-937X(23)00174-0</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Franke, Wolfgang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and Bohemia (S-Armorica), is unrelated to the Rheic and records Cambrian to early Ordovician rifting and Silurian/early Devonian drift. Allochthonous flysch sediments record onset of convergence (Late Frasnian), and flysch onlap on the passive margin (early Famennian). A felsic tuff near the base of the autochthonous flysch has yielded a U-Pb TIMS age of 333.4 ± 0.6 Ma (late Asbian). It corresponds to the emplacement and cooling of (U)HP rocks in the Saxo-Thuringian Erzgebirge and Granulite antiforms, thus confirming extrusion of the high-grade rocks from the asthenospheric mantle into the upper crust of the foreland. Subsequent folding and thrusting relate to dextral, oblique collision. An alleged mid-Viséan phase of constriction is discarded. The northern part of Bohemia sourced the Saxo-Thuringian flysch, but shows no evidence of high elevations. The southern (Barrandian) part remained close to sea-level from the Cambrian to early Carboniferous. Granulite facies metamorphism (340 Ma), thermalanomalies during deformation of the foreland (c. 330 Ma), granite intrusion and Ar-loss in sheet silicates (325 to 275 Ma) relate to the plume-generation zone “TUZO” active under Europe. The Moldanubian zone with its (U)HP metamorphic rocks represents subducted and exhumed fill of a separate, Galicia-Moldanubian basin. Models interpreting the Moldanubian as subducted Saxo-Thuringian rocks exhumed in the rear of the Teplá-Barrandian can be discarded by elementary considerations. Re-evaluation of tectono-stratigraphic units confirms that the German Saxo-Thuringian is linked with the Polish West Sudetes by the Bohemian orocline, which formed by the molding of Armorican terranes into an embayment defined by the margins of Avalonia and Baltica. The plate-tectonic paths of the Bruno-Vistulian and related terranes (TETA) remains controversial. Relations of the Moldanubian Thrust with the ENE-trending East-Variscan Shear Zone of the Alps are discussed.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Variscan bohemian massif</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Plate-tectonic and geodynamic evolution</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Formation and exhumation of (ultra)-high-grade metamorphic rocks</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Anorogenic heating</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Bohemian arc</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Żelaźniewicz, Andrzej</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Gondwana 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