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From each purchase you get bonuses with which you may pay for new tickets.Buy flight tickets, get 1% from each purchase on your account, and save on you further travels. We collaborate with 750 airline companies and will find for you a ticket to any destination at the lowest price.The magmatic event at 931 ± 2 Ma postdates latest regional deformation by about 60 Myr and, therefore, anorthosite genesis is clearly anorogenic in nature, representing a thermal pulse that followed the Sveconorwegian-Grenville orogeny.Inherited zircon components and initial Pb isotopic compositions substantiate that the anorthosite parent magmas were generated to a large degree by melting of old continental material having ages of about 1690, 1450, and 1240 Ma.In the margin of massif anorthosites secondary baddeleyite was formed at 915 ± 4 Ma, in association with later deformation produced by the diapiric mode of emplacement.Zircon cannot have formed in the primary magmas and more differentiated, quartz-mangeritic liquid within mega-orthopyroxene aggregates seems to be the most plausible liquid to precipitate zircon.This surprisingly short period of magmatic activity also includes the injection of 931 ± 5 Ma old jotunite dikes.Intrusion of the ilmenite norite, which constitutes the Tellnes Fe Ti deposit took place about 10 Myr later at 920 ± 3 Ma.