Anagram & Information om | Engelska ordet NAPPES

Exempel på hur man kan använda NAPPES i en mening

• An ellipse has two Dandelin spheres touching the same nappe of the cone, while hyperbola has two Dandelin spheres touching opposite nappes.
• The Central Alps consist mainly of the gneiss and slate rocks of the various Austroalpine nappes (Lower and Upper Austroalpine), with the exception of the Hohe Tauern and Engadine windows, where they are composed mostly of Jurassic rock and limestones and, locally, (Bergell and Rieserferner) also of granite.
• The South Carpathians represent an intricate pile of tectonic nappes, overthrusted from west eastwards during the Austrian (Middle Cretaceous) and Laramian paroxysmal phases, corresponding to various plate fragments.
• The Monte Rosa Nappe lies below the Zermatt-Saas zone and is part of the Penninic nappes in the Briançonnais microcontinent zone, although its paleographic origin is controversial and is sometimes assigned to the Sub-Penninic nappes.
• Almost all of Switzerland's tectonic structural units are represented, dating back in geological history between five and a thousand million years: the crystalline basement of the Aarmassif and Gotthard Massif mountain ranges, the Helvetic and Penninic nappes, the Southern Alps, the limestone of the Jura Mountains, and the molasses of the Swiss Plateau.
• Tectonically, Despotiko, Antiparos, and Paros belong to the Attic-Cycladic Crystalline of the Central Hellenides, a stack of metamorphic tectonic nappes, mainly comprising variable types of gneiss, schist, marble and amphibolite, and tectonic slices of unmetamorphosed sediments on top, separated by low-angle normal faults from the metamorphic units below.
• The "Helvetic nappes" are a nappe stack that was thrust over the molasse of the Molasse basin in the Alpine foreland.
• The Penninic nappes or the Penninicum, commonly abbreviated as Penninic, are one of three nappe stacks and geological zones in which the Alps can be divided.
• Because the Austroalpine nappes consist of material from the former Apulian or Adriatic plate, that was thrust over the European plate, they are called allochthon nappes.
• The nappe is tectonostratigraphically on top of the Penninic nappes and by most researchers seen as Austroalpine.
• It is a window (in German fenster) in the Austroalpine nappes where high-grade metamorphic rocks of the underlying Penninic nappes crop out.
• The Sesia zone is (just as the correlated Dent Blanche nappe) tectonostratigraphically on top of (ophiolitic) Zermatt-Saas zone of the Penninic nappes.
• The Bündner schists can be found throughout the Penninic zone of the Alps, often forming zones of high strain between or large infolded synclines (so called Mulde or Mulden) in the crystalline nappes that are made of more competent gneiss.
• Fragments of Valais oceanic crust have been obducted and can be found as ophiolites in the Penninic nappes of the Alps.
• The Briançonnais zone or Briançonnais terrane is a piece of continental crust found in the Penninic nappes of the Alps.
• Fragments of Piemont-Ligurian oceanic crust were preserved as ophiolites in the Penninic nappes of the Alps and the Tuscan nappes of the Apennines.
• The thrustfront moves over a developing decollement horizon, and separates the (internal) high grade metamorphic rocks of the Penninic nappes from the (external) sedimentary rocks and crystalline basement of the Helvetic nappes.
• In contrast to the completely detached Helvetic nappes, the Infrahelvetic complex is still lying conformably on top of a Hercynian basement which forms the external massifs of the Aar and Gotthard nappes.
• In geology, tectonostratigraphy is stratigraphy that refers either to rock sequences in which large-scale layering is caused by the stacking of thrust sheets, or nappes, in areas of thrust tectonics or to the effects of tectonics on lithostratigraphy.
• The Zermatt-Saas zone is tectonostratigraphically the highest part of the Penninic nappes and lies directly under the Sesia zone and Dent Blanche klippe, that are interpreted as belonging to the Austroalpine nappes.

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