FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4381952845> ?p ?o ?g. }

• W4381952845 endingPage "377" @default.
• W4381952845 startingPage "351" @default.
• W4381952845 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), thermal anomalies 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." @default.
• W4381952845 created "2023-06-26" @default.
• W4381952845 creator A5009693865 @default.
• W4381952845 creator A5070260854 @default.
• W4381952845 date "2023-12-01" @default.
• W4381952845 modified "2023-10-17" @default.
• W4381952845 title "Variscan evolution of the Bohemian Massif (Central Europe): Fiction, facts and problems" @default.
• W4381952845 cites W1500090572 @default.
• W4381952845 cites W1510043202 @default.
• W4381952845 cites W1513549803 @default.
• W4381952845 cites W1533032719 @default.
• W4381952845 cites W1963985336 @default.
• W4381952845 cites W1966282673 @default.
• W4381952845 cites W1966800387 @default.
• W4381952845 cites W1967998028 @default.
• W4381952845 cites W1970255541 @default.
• W4381952845 cites W1972720261 @default.
• W4381952845 cites W1973467564 @default.
• W4381952845 cites W1977237606 @default.
• W4381952845 cites W1980074014 @default.
• W4381952845 cites W1980662389 @default.
• W4381952845 cites W1983545609 @default.
• W4381952845 cites W1988142388 @default.
• W4381952845 cites W1988848768 @default.
• W4381952845 cites W1993859923 @default.
• W4381952845 cites W2000891256 @default.
• W4381952845 cites W2003365780 @default.
• W4381952845 cites W2005369357 @default.
• W4381952845 cites W2006771127 @default.
• W4381952845 cites W2009321606 @default.
• W4381952845 cites W2009797018 @default.
• W4381952845 cites W2010078765 @default.
• W4381952845 cites W2012999674 @default.
• W4381952845 cites W2013184978 @default.
• W4381952845 cites W2013333853 @default.
• W4381952845 cites W2013653698 @default.
• W4381952845 cites W2014979614 @default.
• W4381952845 cites W2015444608 @default.
• W4381952845 cites W2015688271 @default.
• W4381952845 cites W2019583774 @default.
• W4381952845 cites W2020137865 @default.
• W4381952845 cites W2023195690 @default.
• W4381952845 cites W2025057597 @default.
• W4381952845 cites W2025544970 @default.
• W4381952845 cites W2025753772 @default.
• W4381952845 cites W2026968334 @default.
• W4381952845 cites W2031255348 @default.
• W4381952845 cites W2031561150 @default.
• W4381952845 cites W2032358870 @default.
• W4381952845 cites W2033699592 @default.
• W4381952845 cites W2034283772 @default.
• W4381952845 cites W2035422192 @default.
• W4381952845 cites W2035644134 @default.
• W4381952845 cites W2037092946 @default.
• W4381952845 cites W2040305185 @default.
• W4381952845 cites W2041033683 @default.
• W4381952845 cites W2041431089 @default.
• W4381952845 cites W2041921116 @default.
• W4381952845 cites W2044135322 @default.
• W4381952845 cites W2044861519 @default.
• W4381952845 cites W2045723495 @default.
• W4381952845 cites W2048620848 @default.
• W4381952845 cites W2050306746 @default.
• W4381952845 cites W2051187287 @default.
• W4381952845 cites W2057045386 @default.
• W4381952845 cites W2057903897 @default.
• W4381952845 cites W2063241423 @default.
• W4381952845 cites W2064150201 @default.
• W4381952845 cites W2067258571 @default.
• W4381952845 cites W2067698088 @default.
• W4381952845 cites W2071054080 @default.
• W4381952845 cites W2071094008 @default.
• W4381952845 cites W2071925129 @default.
• W4381952845 cites W2075333690 @default.
• W4381952845 cites W2076034511 @default.
• W4381952845 cites W2076274920 @default.
• W4381952845 cites W2076397048 @default.
• W4381952845 cites W2076402704 @default.
• W4381952845 cites W2076906005 @default.
• W4381952845 cites W2077047480 @default.
• W4381952845 cites W2079285326 @default.
• W4381952845 cites W2079462285 @default.
• W4381952845 cites W2081623570 @default.
• W4381952845 cites W2086513054 @default.
• W4381952845 cites W2086654360 @default.
• W4381952845 cites W2089131102 @default.
• W4381952845 cites W2089585228 @default.
• W4381952845 cites W2090409117 @default.
• W4381952845 cites W2093843849 @default.
• W4381952845 cites W2093936359 @default.
• W4381952845 cites W2095878716 @default.
• W4381952845 cites W2099974850 @default.
• W4381952845 cites W2101295512 @default.
• W4381952845 cites W2103371634 @default.
• W4381952845 cites W2107497422 @default.
• W4381952845 cites W2107607517 @default.
• W4381952845 cites W2110913810 @default.
• W4381952845 cites W2112223739 @default.

• next