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| Titel |
Proterozoic granitization and charnockitization in the Central Zone of the Limpopo granulite belt, South Africa |
| VerfasserIn |
Elizaveta Moiseeva, Leonid Perchuk, Oleg Safonov |
| Konferenz |
EGU General Assembly 2010
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 12 (2010) |
| Datensatznummer |
250032008
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| Zusammenfassung |
| Precambrian Limpopo granulite facies terrain experienced two regional high-grade events.
The first one, D2/M2 (2.67-2.53 Ga), was marked by numerous sheath folds, while the
subsequent overprinting event D3/M3 (2.02 Ga) formed both regional and local
linear shear zones. The Z-shaped P-T path shows two metamorphic events reflecting
the polymetamorphic nature of the Limpopo Belt (LB) [1 and refs. therein]. The
D2/M2 event represents the oldest decompression cooling path from P < 9.0 kbar
and T |
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