PARTIAL MELTING AND THE FORMATION OF GRANULITE FACIES ASSEMBLAGES IN NAMAQUALAND, SOUTH-AFRICA

Granulite facies metapelite, biotite gneiss and metabasic gneiss in Namaqualand contain coarse-grained, discordant, unfoliated, anhydrous segregations, surrounded by a finer grained, foliated matrix that commonly includes hydrous minerals. The segregations have modes consistent with the hypothesis t...

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Hlavní autor: Waters, D
Médium: Journal article
Jazyk:English
Vydáno: 1988