Magma flow pattern of the 1.78 Ga dyke swarm of the North China Craton during the initial assembly of the Supercontinent Nuna/Columbia: Constraints from rock magnetic and anisotropy of magnetic susceptibility studies
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DOI: 10.1016/j.precamres.2020.105773
Abstract: Abstract The geodynamic origin of the 1.78 Ga dyke swarm in the North China Craton (NCC) is long debated. It is considered either a post-collision process or paleoplume-related. Constraining its origin is essential for the reconstruction… read more here.
Keywords: swarm north; magma flow; supercontinent nuna; north china ... See more keywords