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Published in 2017 at "Lithos"
DOI: 10.1016/j.lithos.2017.06.001
Abstract: Abstract From the Neoproterozoic to the early Paleozoic, the northern Gondwana margin was sequentially shaped by the Cadomian accretionary and the Variscan collisional orogens which offers the opportunity to investigate the relative extent of crust…
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Keywords:
cadomian type;
crustal evolution;
gondwana margin;
massif central ... See more keywords