Sequence of Events
A simplified sequence of events known from the Narryer Gneiss Terrane of the Western Gneiss Belt of the Yilgarn craton is reproduced after A. F. Trendall (1991);
- 2000-1600 Ma;
Basic dykes, related to the Gascoyne Complex and Capricorn Orogeny - 2700-2600 Ma;
Granite sheets and juxtaposition with the Yilgarn craton. - 3350-3300 Ma; Amphibolite to granulite facies metamorphism
- ~3350-3400 Ma; deposition of metasedimentary rocks
- 3400 Ma; Intrusion of syenogranites to form Dugel Gneiss, basic and ultramafic dykes
- >3400-3680 Ma; Deformation
- ~3680 Ma; Meeberrie Gneiss
- >3680-3730 Ma; Deformation
- ~3780 Ma; Manfred Complex ultramafic-mafic layered intrusion
- >4100 Ma; Metasedimentary precursor gneiss to host the Manfred Complex
Read more about this topic: Narryer Gneiss Terrane
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