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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Bibliographic Details
Main Authors: T. F. D. Nielsen, O. Johnsen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Gardiner
Gardiner Plateau
Greenland
East Greenland
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
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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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