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June 01, 1989
Sapphirine-quartz-orthopyroxene symplectites after cordierite in the Archaean Napier Complex, Antarctica; evidence for a counterclockwise P-T path?
Y. Motoyoshi;
Y. Motoyoshi
Univ. N.S.W., Dep. Appl. Geol., Kensington, N.S.W. 2033, Australia
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European Journal of Mineralogy (1989) 1 (3): 467–471.
Article history
first online:
02 Mar 2017
Citation
Y. Motoyoshi, B. J. Hensen; Sapphirine-quartz-orthopyroxene symplectites after cordierite in the Archaean Napier Complex, Antarctica; evidence for a counterclockwise P-T path?. European Journal of Mineralogy 1989;; 1 (3): 467–471. doi:
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Index Terms/Descriptors
- aenigmatite group
- Antarctica
- Archean
- chain silicates
- chemical composition
- cordierite
- framework silicates
- granulites
- intergrowths
- metamorphic rocks
- minerals
- Napier Complex
- orthopyroxene
- P-T conditions
- petrology
- polar regions
- Precambrian
- pyroxene group
- quartz
- ring silicates
- sapphirine
- silica minerals
- silicates
- symplectite
Latitude & Longitude
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