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Published in 2018 at "Precambrian Research"
DOI: 10.1016/j.precamres.2017.11.017
Abstract: Abstract According to present views, the crustal terranes of the Anabar province of the Siberian craton were initially independent blocks, separated from the convecting mantle at 3.1 (Daldyn terrane), 2.9 (Magan terrane) and 2.5 Ga (Markha…
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Keywords:
province siberian;
siberian craton;
crust beneath;
markha terrane ... See more keywords