THE ring-shaped
SUMMARY. Titaniferous clinohumite occurs as a major constituent in the centres of late magmatic veins in the Tertiary ultramafic, strongly alkaline Gardiner Plateau Complex in East Greenland (69 * N. and 32 " W.). The complex isbriefly described and an electron microprobe analysis of titanifero...
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.607.5328 http://www.minersoc.org/pages/Archive-MM/Volume_42/42-321-99.pdf |
Summary: | SUMMARY. Titaniferous clinohumite occurs as a major constituent in the centres of late magmatic veins in the Tertiary ultramafic, strongly alkaline Gardiner Plateau Complex in East Greenland (69 * N. and 32 " W.). The complex isbriefly described and an electron microprobe analysis of titaniferous clinohumite is presented. This |
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