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Paleokontinint


kontinintgeologyskeskiednisplatetektonykorogenesesubduksje












Paleokontinint




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In paleokontinint is in kontinint dat yn de geologyske skiednis bestie en opgien is yn kontininten fan no, mooglik troch earst yn oare paleokontininten oergien te wêzen. Troch it proses fan platetektonyk ferskowe de kontininten en troch orogenese en subduksje ûntsteane nije kontininten.



Paleokontininten |



  • Lauraazje (ôfspjalte fan Pangea; Noard-Amearika, Europa, Aazje)


  • Gondwana (ôfspjalte fan Pangea; Súd-Amearika, Afrika, Austraalje, Antarktika)


  • Pangea (oaniensletten superkontinint)

  • Laurensja

  • Baltika

  • Avaloanja

  • Siberysk Kraton

  • West-Gondwanalân

  • East-Gondwanalân

  • Nigerblok

  • Baikalblok

  • Pannosja

  • Rodynje

  • Protolauraazje

  • Arktika

  • Kenorlân

  • Vaalbara


Sjoch ek |


  • Superkontinint



Untfongen fan "https://fy.wikipedia.org/w/index.php?title=Paleokontinint&oldid=641995"










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