title: Early Proterozoic ultrahigh pressure metamorphism: evidence from microdiamonds.
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.
authors.affiliation: Laboratoire 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
authors.forename: Pierre
authors.initials: P
authors.lastname: Cartigny
authors.forename: Ingrid
authors.initials: I
authors.lastname: Chinn
authors.forename: K S
authors.initials: KS
authors.lastname: Viljoen
authors.forename: Derek
authors.initials: D
authors.lastname: Robinson