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Siberia (continent)

From Wikipedia, the free encyclopedia
Ancient craton forming the Central Siberian Plateau
Current location of the remains of the ancient landmass of Siberia in northAsia

Siberia, also known asSiberian Craton,Angaraland (or simplyAngara) andAngarida,[1] is an ancientcraton in the heart ofSiberia. Today forming theCentral Siberian Plateau, it formed an independent landmass prior to its fusion intoPangaea during the lateCarboniferous-Permian. TheVerkhoyansk Sea, a passive continental margin, was fringing the Siberian Craton to the east in what is now theEast Siberian Lowland.[2]

Angaraland was named in the 1880s by Austrian geologistEduard Suess who erroneously believed that in thePaleozoic Era there were two large continents in the Northern Hemisphere: "Atlantis", which was North America connected to Europe via a peninsula (Greenland and Iceland), and "Angara-land", which would have been eastern Asia, named after theAngara River in Siberia.[3]

Tectonics

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About 2.5 billion years ago (in theSiderian Period), Siberia was part of a continent calledArctica, along with theCanadian Shield. Around 1.1 billion years ago (in theStenian Period), Siberia became part of thesupercontinent ofRodinia, which lasted until theTonian about 750 million years ago when it broke up, and Siberia became part of the landmass ofProtolaurasia. During theEdiacaran Period around 600 million years ago, Protolaurasia became part of the southern supercontinent ofPannotia. Around 550 million years ago, both Pannotia and Protolaurasia split up to become the continents ofLaurentia,Baltica and Siberia.[citation needed]

Map of Earth's continents and oceans in the middle of theOrdovician Period, about 470 million years ago (SI=Siberia, LA=Laurentia, BA=Baltica)

Siberia was an independent continent through the early Paleozoic until, during theCarboniferous Period, it collided with the minor continent ofKazakhstania. A subsequent collision withEuramerica/Laurussia during the LateCarboniferous-Permian formedPangaea.[4]

Pangaea split up during theJurassic though Siberia stayed withLaurasia. Laurasia gradually split up during theCretaceous with Siberia remaining part of present-day northeasternEurasia. Today, Siberia forms part of the landmass ofAfro-Eurasia. To the east it is joined to theNorth American plate at theChersky Range. In around 250 million years from now Siberia may be in thesubtropical region and part of the new supercontinent ofPangaea Proxima.[citation needed]

Features

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See also

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References

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  1. ^Klets, A. G.; Budnikov, I. V.; Kutygin, R. V.; Biakov, A. S.; Grinenko, V. S. (2006)."The Permian of the Verkhoyansk–Okhotsk region, NE Russia".Journal of Asian Earth Sciences.26 (3):258–268.Bibcode:2006JAESc..26..258K.doi:10.1016/j.jseaes.2005.10.001.
  2. ^Permian bivalve mollusks of Northeast Asia, Fig. 1
  3. ^Sprague de Camp, L. (1970).Lost Continents: The Atlantis Theme in History, Science, and Literature. Courier Corporation.ISBN 9780486226682. Retrieved25 October 2015.
  4. ^Xu, Yan; Han, Bao-Fu; Liao, Wen; Li, Ang (March 2022)."The Serpukhovian–Bashkirian Amalgamation of Laurussia and the Siberian Continent and Implications for Assembly of Pangea".Tectonics.41 (3).doi:10.1029/2022TC007218.ISSN 0278-7407.S2CID 247459291.
  5. ^Schematic map of the Siberian craton showing boundaries of the craton and its terranes
  6. ^Schematic map of ancient terrains and kimberlitic fields in the Siberian craton
  7. ^YAKUTIAN KIMBERLITE PROVINCE: POSITION IN THE STRUCTURE OF THE SIBERIAN CRATON AND COMPOSITION OF THE UPPER AND LOWER CRUST

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