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GEOREF RECORD

Native nickel-iron alloy, its mode of occurrence, distribution and origin

J. S. R. Krishna Rao
Native nickel-iron alloy, its mode of occurrence, distribution and origin
Economic Geology and the Bulletin of the Society of Economic Geologists (May 1964) 59 (3): 443-448

Abstract

Native nickel-iron as awaruite, souesite, josephinite occurs in serpentinized peridotites belonging to Alpine orogeny. New localities for the mineral are listed, the diagnostic properties enumerated and the paragenetic sequence as suggested by the ore microscopic methods is given. The mineral or mineral group is suggested to have originated by reduction of the nickel-bearing silicates or sulfides during serpentinization of the peridotites.


ISSN: 0361-0128
EISSN: 1554-0774
Coden: ECGLAL
Serial Title: Economic Geology and the Bulletin of the Society of Economic Geologists
Serial Volume: 59
Serial Issue: 3
Title: Native nickel-iron alloy, its mode of occurrence, distribution and origin
Pages: 443-448
Published: 196405
Text Language: English
Publisher: Economic Geology Publishing Company, Lancaster, PA, United States
Accession Number: 1964-012010
Categories: Mineralogy
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus.
N45°45'00" - N47°45'00", E05°49'60" - E10°30'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, Copyright, Society of Economic Geologists. Reference includes data from Bibliography and Index of North American Geology, U. S. Geological Survey, Reston, VA, United States
Update Code: 1964
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