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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| Aineistotyyppi: | Journal article |
| Kieli: | English |
| Julkaistu: |
1988
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