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Economic Geology; August 1961; v. 56; no. 5; p. 994-995
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Conditions for ilmenite alteration

Langtry E. Lynd

Discussion of GeoScience Abstracts 3-1630. In order that Austin's postulation be applicable to sand ilmenites generally, it would be necessary to explain their high ferric iron content. The presence of ferric iron and lower intensity of alteration in New Jersey and other sand ilmenites is good evidence for a different alteration environment than that which prevailed at Ambrosia Lake.

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