Journal
LITHOS
Volume 70, Issue 3-4, Pages 61-75Publisher
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DOI: 10.1016/S0024-4937(03)00092-6
Keywords
Kokchetav Massif; ultrahigh-pressure metamorphism; excess argon; exhumation rate
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The diamond-bearing, ultrahigh-pressure Kokchetav Massif recrystallized at eclogite-facies conditions deep in the mantle at 180-km depth at 535 +/- 3 Ma, and yet new 40Ar/39Ar ages suggest that it may have been exhumed to crustal depths (as indicated by closure of mica to Ar loss) by similar to529 Ma. These data indicate a possible exhumation rate of tens of kilometers per million years, i.e., a rate that is comparable to rates of horizontal plate motion and subduction. (C) 2003 Elsevier B.V. All rights reserved.
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