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 |
|---|---|
| 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