Английская Википедия:Glenburgh orogeny

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Версия от 18:28, 14 марта 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} {{Use dmy dates|date=April 2022}} {{more citations needed|date=November 2019}} The '''Glenburgh orogeny''' was a mountain building event in the Proterozoic from 2.0 to 1.96 billion years ago. The Glenburgh Terrane collided with the Yilgarn Craton, creating the Errabiddy Shear Zone. Mineral lineation from the orogeny is common although it is sometimes overprinted in...»)
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The Glenburgh orogeny was a mountain building event in the Proterozoic from 2.0 to 1.96 billion years ago. The Glenburgh Terrane collided with the Yilgarn Craton, creating the Errabiddy Shear Zone. Mineral lineation from the orogeny is common although it is sometimes overprinted in greenschist by the later Capricorn orogeny.[1]

See also

References

Шаблон:Reflist


Шаблон:Australia-geology-stub