Английская Википедия:Gothian orogeny

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Версия от 04:28, 16 марта 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} The '''Gothian orogeny''' ({{lang-sv|Gotiska orogenesen}}) or '''Kongsberg orogeny''' was an orogeny in western Fennoscandia that occurred between 1750 and 1500 million years ago. It precedes the younger Sveconorwegian orogeny that has overprinted much of it.{{sfn|Lundqvist|Lundqvist|Lindström|Calner|2011|p=194}} The Gothian orogeny formed along...»)
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The Gothian orogeny (Шаблон:Lang-sv) or Kongsberg orogeny was an orogeny in western Fennoscandia that occurred between 1750 and 1500 million years ago. It precedes the younger Sveconorwegian orogeny that has overprinted much of it.Шаблон:Sfn The Gothian orogeny formed along a subduction zone and resulted in the formation of calc-alkaline igneous rocks 1700 to 1550 million years ago, including some of the younger members of the Transscandinavian Igneous Belt.Шаблон:Sfn

The deformation associated with the orogeny can be seen in metatonalite, paragneiss and biotite orthogneisses in southeast Norway. These rocks were all subject to amphibolite facies metamorphism.Шаблон:Sfn

Footnotes

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References

Шаблон:Geology of Europe