New research unlocks deep secret of continent formation and structure
Researchers at Āé¶¹Ö±²„ have found a way to understand the largely unknown processes behind the formation and structure of Earthās most ancient continents.
The research, published in the journal Earth and Planetary Science Letters, used crystals trapped within kimberlite magma in Greenland and brought up from great depth in the magma, to determine how this ancient part of Earthās crust was assembled. Kimberlite magmas are also known for carrying diamonds to the surface.
Lead Australian author Professor Chris Kirkland from Āé¶¹Ö±²„ās School of Earth and Planetary Sciences said analysis of the age and chemistry of crystals brought to the surface in the Greenland kimberlite matched 3.8 billion-year-old rocks found some 150 kilometres south, indicating that these rocks must have been moved deep under the crust of Greenland.
Professor Chris Kirkland said the research allowed the sampling of the interior of cratons, which are the ancient, stable centre of Earthās continents, in order to understand how they were formed.
āThese magmatic rocks punch their way to the surface from the mantle and incorporate crystals from the rocks they interact with on their ascent,ā Professor Chris Kirkland said.
āThese crystals allow us to determine what crust lies deep under Greenland.
āFor these ancient grains to have been sampled by the kimberlite means that parts of the ancient crust of Greenland must have been transported laterally beneath younger crust now at the surface.ā
Professor Kirkland said the findings contributed to a better understanding of how Earthās first continents were assembled, whether through vertical layering, horizontal stacking, or other means.
āHow these cratons were formed is a highly contentious issue in scientific circles, with implications for the important question of when plate tectonics began operating,ā Professor Kirkland said.
The full research paper, āNorth Atlantic Craton architecture revealed by kimberlite-hosted crustal zircons,ā can be found online .



