The significance of prograde and retrograde quartz-bearing intergrowth microstructures in partially melted granulite-facies rocks

The significance of prograde and retrograde quartz-bearing intergrowth microstructures in partially melted granulite-facies rocks

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Bibliográfalaš dieđut
Váldodahkki:	Waters, D
Materiálatiipa:	Conference item
Almmustuhtton:	2001

Geahča maid

The significance of prograde and retrograde quartz-bearing intergrowth microstructures in partially melted granulite-facies rocks
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PARTIAL MELTING AND THE FORMATION OF GRANULITE FACIES ASSEMBLAGES IN NAMAQUALAND, SOUTH-AFRICA
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HERCYNITE-QUARTZ GRANULITES - PHASE-RELATIONS, AND IMPLICATIONS FOR CRUSTAL PROCESSES
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Holocene progradation and retrogradation of the Central Texas Coast regulated by alongshore and cross‐shore sediment flux variability
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Prograde and Retrograde Terms of Gravimetric Polar Motion Excitation Estimates from the GRACE Monthly Gravity Field Models
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The occurrence of osumilite in pelitic granulites of the Namaqualand metamorphic complex, South Africa
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