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GEOREF RECORD

The Odara pegmatite

C. V. Paulose
The Odara pegmatite
Economic Geology and the Bulletin of the Society of Economic Geologists (September 1957) 52 (6): 702-708

Abstract

Concludes that structural features and zonal distribution of such minerals as mica, magnetite, columbite, and beryl in a zoned pegmatite dike in gneiss of the Odara area, Travancore, India, can be attributed to progressive crystallization of a pegmatitic magma, and that there is no evidence of hydrothermal replacement.


ISSN: 0361-0128
EISSN: 1554-0774
Coden: ECGLAL
Serial Title: Economic Geology and the Bulletin of the Society of Economic Geologists
Serial Volume: 52
Serial Issue: 6
Title: The Odara pegmatite
Author(s): Paulose, C. V.
Pages: 702-708
Published: 195709
Text Language: English
Publisher: Economic Geology Publishing Company, Lancaster, PA, United States
Accession Number: 1957-004004
Categories: Igneous and metamorphic petrology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. (incl. sk. map)
N07°00'00" - N37°00'00", E68°00'00" - E97°00'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States
Update Code: 1957
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