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زمینشناسی و معدن::
فرورانش
and most likely punctuated by short-lived subduction events.
heat flux, some authors argue these data are compatible with a short subduction episode at the Hadean-Archean boundary (causing
subduction, crustal growth and differentiation at the Hadean-Archean boundary.
strongly convecting mantle, the intense formation of volcanic plateaus, flat subduction systems, and limited episodes of steep
subduction.
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