Article ID Journal Published Year Pages File Type
4722736 Precambrian Research 2015 15 Pages PDF
Abstract
Highlights
- The Mesoarchaean arc Kapisilik and Isukasia Eoarchaean terranes collided at 2970 Ma.
- Melting the Isukasia terrane's buried edge gave the granites in the Ivisaartoq dome.
- The Mesoarchaean collisional architecture was partitioned by ∼2690 Ma shear zones.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Mesoarchaean collision of Kapisilik terrane 3070 Ma juvenile arc rocks and >3600 Ma Isukasia terrane continental crust (Greenland)
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