Pressure-temperature evolution during two granulite-facies metamorphic events (2.62 and 2.02 Ga) in rocks from the Central Zone of the Limpopo Belt, South Africa

Article

Abstract: The Central Zone of the Limpopo Belt in southern Africa is a classical example of a polymetamorphic

Palabras claves:

Delamination, granulite, Limpopo Belt, Neoarchean, P-T path, Pseudosection

Autores:

Alfred Kron̈er, Bobek P., Brandl G., Brandt S., Fischer A., Klemd R., Li Q., Zhou T.

Fuentes:

scopus