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On an unmetamorphosed iron-formation in the early precambrian of South-West Greenland

✍ Scribed by P. U. Appel


Book ID
104662159
Publisher
Springer
Year
1974
Tongue
English
Weight
722 KB
Volume
9
Category
Article
ISSN
0026-4598

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✦ Synopsis


During Renzy Mines Ltd. exploration programme in 1972, an iron-formation was found in the Midternaes area north east of Ivigtut, South-West Greenland. It contains up to 32.9 % Fe. The dominant mineral is greenalite, with minor amounts of magnetite, siderite and quartz. It was found in the northernmost part of the Ketilidian supracrustals (? 1800 m.y.), which are non-metamorphosed or very weakly metamorphosed. The iron-formation is suggested to be of submarine-exhalative origin, and precipitated in a moderately deep sea at low atmospheric 02 pressure.


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