The significance of prograde and retrograde quartz-bearing intergrowth microstructures in partially melted granulite-facies rocks
Príomhchruthaitheoir: | Waters, D |
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Formáid: | Conference item |
Foilsithe / Cruthaithe: |
2001
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Míreanna comhchosúla
Míreanna comhchosúla
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The significance of prograde and retrograde quartz-bearing intergrowth microstructures in partially melted granulite-facies rocks
de réir: Waters, D
Foilsithe / Cruthaithe: (2001) -
Partial melting and the formation of granulite facies assemblages in Namaqualand, South Africa
de réir: Waters, D
Foilsithe / Cruthaithe: (1988) -
PARTIAL MELTING AND THE FORMATION OF GRANULITE FACIES ASSEMBLAGES IN NAMAQUALAND, SOUTH-AFRICA
de réir: Waters, D
Foilsithe / Cruthaithe: (1988) -
HERCYNITE-QUARTZ GRANULITES - PHASE-RELATIONS, AND IMPLICATIONS FOR CRUSTAL PROCESSES
de réir: Waters, D
Foilsithe / Cruthaithe: (1991) -
HERCYNITE-QUARTZ GRANULITES - PHASE-RELATIONS, AND IMPLICATIONS FOR CRUSTAL PROCESSES
de réir: Waters, D
Foilsithe / Cruthaithe: (1991)