east european craton wikipedia - EAS

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  1. The East European Craton (EEC) is the core of the Baltica proto- plate and consists of three crustal regions/segments: Fennoscandia to the northwest, Volgo-Uralia to the east, and Sarmatia to the south.
    en.wikipedia.org/wiki/East_European_craton
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    What is the East European Craton (EEC)?
    The East European Craton ( EEC) is the core of the Baltica proto- plate and consists of three crustal regions/segments: Fennoscandia to the northwest, Volgo-Uralia to the east, and Sarmatia to the south.
    en.wikipedia.org/wiki/East_European_craton
    What is a craton?
    Jump to navigation Jump to search. A craton is an ancient part of the Earth's continental crust which has been more or less stable since Precambrian times. Cratons whose ancient rocks are widely exposed at the surface, often with relatively subdued relief, are known as shields.
    en.wikipedia.org/wiki/List_of_shields_and_cratons
    What is a Shield craton?
    A craton is an ancient part of the Earth's continental crust which has been more or less stable since Precambrian times. Cratons whose ancient rocks are widely exposed at the surface, often with relatively subdued relief, are known as shields.
    en.wikipedia.org/wiki/List_of_shields_and_cratons
    What is Eastern Europe?
    Eastern Europe is the eastern region of Europe. Originally, it referred to the countries that were under the influence of the Eastern Orthodox Church in Constantinople during the middle ages, which was in contrast to the West which referred to the countries under the influence of the Roman Catholic and later Protestant Churches.
    simple.wikipedia.org/wiki/Eastern_Europe
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    East European Craton - Wikipedia

    https://en.wikipedia.org/wiki/East_European_craton

    The East European Craton (EEC) is the core of the Baltica proto-plate and consists of three crustal regions/segments: Fennoscandia to the northwest, Volgo-Uralia to the east, and Sarmatia to the south. Fennoscandia includes the Baltic Shield (also referred to as the Fennoscandian Shield) and has

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    The most distinguishable physiographic aspect of the East European Craton is the extensive 3-km and more-thick Riphean (middle to late Proterozoic) sedimentary cover over its 3000-km-wide platformarea (East European Platform,

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    The East European Craton has a very complex tectonic history with extensive Proterozoic and Paleozoic rifting, a large portion of which is of early deep mantle plume

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  4. List of shields and cratons - Wikipedia

    https://en.wikipedia.org/wiki/List_of_shields_and_cratons

    Listed by modern continent and Gondwana, include:
    • Amazonian Craton
    • Sao Francisco Craton (Congo Craton)
    • Rio Apa Craton
    • Río de la Plata Craton

    Wikipedia · Nội dung trong CC-BY-SA giấy phép
  5. East European Craton - Wikiwand

    https://www.wikiwand.com/en/East_European_Craton

    The East European Craton is the core of the Baltica proto-plate and consists of three crustal regions/segments: Fennoscandia to the northwest, Volgo-Uralia to the east, and Sarmatia to the south. Fennoscandia includes the Baltic Shield and has a diversified accretionary Archaean and early Proterozoic crust, while Sarmatia has an older Archaean crust.

  6. East European Craton - Wikipedia

    https://it.abcdef.wiki/wiki/East_European_Craton

    L' East European Craton ( CEE) è il nucleo del Baltica proto piatto e si compone di tre crostali regioni / segmenti: Fennoscandia a nord-ovest, Volgo-Uralia a est, e Sarmazia a sud. Fennoscandia include lo Scudo Baltico (noto anche come Scudo Fennoscandiano) e ha una crosta diversificata di accrescimento Archeano e primo Proterozoico, mentre la Sarmatia ha …

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