The significance of prograde and retrograde quartz-bearing intergrowth microstructures in partially melted granulite-facies rocks
المؤلف الرئيسي: | Waters, D |
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التنسيق: | Conference item |
منشور في: |
2001
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مواد مشابهة
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The significance of prograde and retrograde quartz-bearing intergrowth microstructures in partially melted granulite-facies rocks
حسب: Waters, D
منشور في: (2001) -
Partial melting and the formation of granulite facies assemblages in Namaqualand, South Africa
حسب: Waters, D
منشور في: (1988) -
PARTIAL MELTING AND THE FORMATION OF GRANULITE FACIES ASSEMBLAGES IN NAMAQUALAND, SOUTH-AFRICA
حسب: Waters, D
منشور في: (1988) -
HERCYNITE-QUARTZ GRANULITES - PHASE-RELATIONS, AND IMPLICATIONS FOR CRUSTAL PROCESSES
حسب: Waters, D
منشور في: (1991) -
HERCYNITE-QUARTZ GRANULITES - PHASE-RELATIONS, AND IMPLICATIONS FOR CRUSTAL PROCESSES
حسب: Waters, D
منشور في: (1991)