Progressive shape evolution of a mineral inclusion under differential stress at high temperature: Example of garnet inclusions within a granulite‐facies quartzite from the Lützow‐Holm Complex, East Antarctica

Publisher: John Wiley & Sons Inc

E-ISSN: 2156-2202|110|B11|2004JB003526-2004JB003526

ISSN: 0148-0227

Source: Journal Of Geophysical Research, Vol.110, Iss.B11, 2005-11, pp. : n/a-n/a

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Abstract