Journal article
THE PETROLOGY OF TWO ZONED SCAPOLITE SKARNS
Abstract
A spheroidal skarn body at Gib Lake, Pontiac County, Quebec, occurs in phlogopite marble, and shows concentric zones several centimeters thick. The zonal sequence is (a) core of blue scapolite; (b) pargasite–albite intergrowth; (c) pure phlogopite; (d) serpentinized forsterite–dolomite marble. The minerals have been analyzed. A zoned skarn with a similar sequence was found 15 miles south on Calumet Island.Phase assemblages are consistent with …
Authors
Shaw DM; Schwarcz HP; Sheppard SMF
Journal
Canadian Journal of Earth Sciences, Vol. 2, No. 6, pp. 577–595
Publisher
Canadian Science Publishing
Publication Date
December 1, 1965
DOI
10.1139/e65-043
ISSN
0008-4077