Resumé
The remains of the deeply exhumed, 3 Ga Maniitsoq impact structure are hosted by granulite-facies orthogneisses and relict metavolcanic belts. Its 35 x 50 km large core (Finnefjeld domain) is thoroughly comminuted by impact-induced seismic oscillations. The surrounding melt zone displays direct mineral melting, localised crush zones and subsequent fluid-assisted anatectic melting triggered by the impacting.
Originalsprog | Engelsk |
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Artikelnummer | 5005 |
Tidsskrift | Meteoritics and Planetary Science |
Vol/bind | 48 |
Udgave nummer | s1 |
DOI | |
Status | Udgivet - 2013 |
Begivenhed | 76th Annual meeting of the Meteoritical Society - Edmonton, Canada Varighed: 29 jul. 2013 → 2 aug. 2013 Konferencens nummer: 76 |
Programområde
- Programområde 4: Mineralske råstoffer