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Updated: Jul 15, 2026

High Pressure Single Crystal Diffraction at PX^2
Published on: January 16, 2017
Early Proterozoic ultrahigh pressure metamorphism: evidence from microdiamonds
Pierre Cartigny1, Ingrid Chinn, K S Viljoen
1Laboratoire de Géochimie des Isotopes Stables, Institut de Physique du Globe, UMR 7047, 2 Place Jussieu, F-75251 Paris, Cedex 05, France. cartigny@ipgp.jussieu.fr
Abstract:
Microdiamonds from the Akluilâk minette dykes (Nunavut, Canada) are similar to diamonds formed in subducted metamorphic rocks. High concentrations of unaggregated nitrogen and positive delta(15)N suggest that the microdiamonds formed within rocks subducted to ultrahigh pressures before being sampled by the minette magma 1.8 billion years ago. This ultrahigh pressure metamorphism in North America, probably related to the Trans-Hudson orogen (about 2 billion years ago), extends the occurrence of ultrahigh pressure metamorphism from 0.6 billion years to before 1.8 billion years ago and suggests that Phanerozoic-type subductions were active by the Early Proterozoic.

