Abstract
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.
| Original language | English |
|---|---|
| Article number | 5005 |
| Journal | Meteoritics and Planetary Science |
| Volume | 48 |
| Issue number | s1 |
| DOIs | |
| Publication status | Published - 2013 |
| Event | 76th Annual meeting of the Meteoritical Society - Edmonton, Canada Duration: 29 Jul 2013 → 2 Aug 2013 Conference number: 76 |
Programme Area
- Programme Area 4: Mineral Resources
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