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  2. Tectonostratigraphy - Wikipedia

    en.wikipedia.org/wiki/Tectonostratigraphy

    Print/export Download as PDF; Printable version; In other projects ... One example of such a tectonostratigraphy is the Scandinavian Caledonides. [1]

  3. Reynaldo Charrier - Wikipedia

    en.wikipedia.org/wiki/Reynaldo_Charrier

    Reynaldo Charrier (born 1945) is a Chilean geologist who has contributed to the tectonostratigraphy of Chile. In 2000 he received the award "Premio Juan Brüggen". In 2000 he received the award "Premio Juan Brüggen".

  4. Moldanubian Zone - Wikipedia

    en.wikipedia.org/wiki/Moldanubian_Zone

    The tectonostratigraphy of the Moldanubian Zone sensu stricto is divided into three main units: At the top the Gföhl unit, a stack of south-vergent crystalline nappes. It consists mostly of rocks of high metamorphic grade (up to amphibolite or granulite facies). These can be metamorphic sediments but also orthogneisses.

  5. Pablo Groeber - Wikipedia

    en.wikipedia.org/wiki/Pablo_Groeber

    Print/export Download as PDF; Printable version; In other projects ... Tectonostratigraphy, Tectonics, Paleogeography, Structural geology:

  6. Category:Stratigraphy - Wikipedia

    en.wikipedia.org/wiki/Category:Stratigraphy

    This page was last edited on 8 September 2016, at 02:53 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.

  7. Krempachy Marl Formation - Wikipedia

    en.wikipedia.org/wiki/Krempachy_Marl_Formation

    The Krempachy Marl Formation is a geological formation in Poland and Slovakia, dating to about 179 million years ago, and covering the middle Toarcian stage of the Jurassic Period. [1]

  8. Category:Tectonics - Wikipedia

    en.wikipedia.org/wiki/Category:Tectonics

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Pages for logged out editors learn more

  9. Svecofennian orogeny - Wikipedia

    en.wikipedia.org/wiki/Svecofennian_orogeny

    The Svecofennian orogeny developed as a succession of four orogenies which by chronological order are: the Lapland-Savo orogeny, the Fennian orogeny, the Svecobaltic orogeny and the Nordic orogeny. [6]