Origin and evolution of the deep thermochemical structure beneath Eurasia
N. Flament, S. Williams, R. D. Müller and 2 more
Nature Communications · 2017
doi:10.1038/ncomms14164 (opens in a new tab)
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Abstract
The Perm anomaly is found in the lower mantle beneath Eurasia, but how this structure formed has remained unclear. Here, the authors show that the anomaly has been mobile since it formed in isolation within a closed subduction network and propose that the anomaly is linked to the Emeishan volcanics.
Abstract licence: CC BY-NC-ND
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