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Geology of the Alps ~ Kindle < RTFEZSWARK Geology of the Alps By Source Reference Series Books LLC Nov 2011, 2011. Taschenbuch. Book Condition: Neu. 246x189x2 mm. Neuware - Source: Wikipedia. Pages: 24. Chapters: Glarus thrust, Flims, Iberian plate, Wetterstein limestone, Elm, Switzerland, Molasse basin, Penninic, Austroalpine nappes, Betic corridor, Alpine orogeny, Gotthard nappe, Helvetic, Ha¿eg Island, Sesia zone, Periadriatic Seam, Aarmassif, External massif, Valais Ocean, Piemont-Liguria Ocean, Apulian Plate, Helvetic nappes, Piz Dolf, Southern Alps, Giudicárie line, Ringelspitz, Bündner schist, Piz Segnas, Greywacke zone, Ivrea zone, Lepontin dome, Briançonnais zone, Infrahelvetic complex, Hohe Tauern window, Dent Blanche nappe, Zermatt-Saas zone, Rhône- Simplon line, Penninic thrustfront, Mürtschenstock. Excerpt: The Alps form a part of a Tertiary orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic all the way to the Himalayas. This belt of mountain chains was formed during the Alpine orogeny. A gap in these mountain chains in central Europe separates the Alps from the Carpathians to the east. Orogeny took place continuously and tectonic subsidence has produced the gaps in between. The Alps arose as a result of the collision of the African and European tectonic plates, in which the Alpine Tethys, which was formerly in between these continents, disappeared. Enormous stress was... READ ONLINE [ 2.03 MB ] Reviews This is the greatest pdf i actually have go through right up until now. It is actually packed with knowledge and wisdom I found out this book from my dad and i advised this publication to find out. -- Arely Rath I actually started reading this pdf. It can be rally exciting throgh reading period of time. Your lifestyle span is going to be enhance as soon as you total reading this ebook. -- Nya Bechtelar DMCA Notice | Terms.

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The Structure of the Alps: an Overview 1 Institut Fiir Geologie Und Paläontologie, Hellbrunnerstr. 34, A-5020 Salzburg, Austria
Carpathian-Balkan Geological pp. 7-24 Salzburg Association, XVI Con ress Wien, 1998 The structure of the Alps: an overview F. Neubauer Genser Handler and W. Kurz \ J. 1, R. 1 2 1 Institut fiir Geologie und Paläontologie, Hellbrunnerstr. 34, A-5020 Salzburg, Austria. 2 Institut fiir Geologie und Paläontologie, Heinrichstr. 26, A-80 10 Graz, Austria Abstract New data on the present structure and the Late Paleozoic to Recent geological evolution ofthe Eastem Alps are reviewed mainly in respect to the distribution of Alpidic, Cretaceous and Tertiary, metamorphic overprints and the corresponding structure. Following these data, the Alps as a whole, and the Eastem Alps in particular, are the result of two independent Alpidic collisional orogens: The Cretaceous orogeny fo rmed the present Austroalpine units sensu lato (including from fo otwall to hangingwall the Austroalpine s. str. unit, the Meliata-Hallstatt units, and the Upper Juvavic units), the Eocene-Oligocene orogeny resulted from continent continent collision and overriding of the stable European continental lithosphere by the Austroalpine continental microplate. Consequently, a fundamental difference in present-day structure of the Eastem and Centrai/Westem Alps resulted. Exhumation of metamorphic crust fo rmed during Cretaceous and Tertiary orogenies resulted from several processes including subvertical extrusion due to lithospheric indentation, tectonic unroofing and erosional denudation. Original paleogeographic relationships were destroyed and veiled by late Cretaceous sinistral shear, and Oligocene-Miocene sinistral wrenching within Austroalpine units, and subsequent eastward lateral escape of units exposed within the centrat axis of the Alps along the Periadriatic fault system due to the indentation ofthe rigid Southalpine indenter.
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