Journal
JOURNAL OF GEOCHEMICAL EXPLORATION
Volume 172, Issue -, Pages 151-166Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.gexplo.2016.10.004
Keywords
Indicator minerals; Till geochemistry; Cassiterite; Indium; Mineral exploration; Glaciated terrain
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A study of the till indicator mineral and matrix geochemical signature of theMount Pleasant W-Mo-Bi and Sn-ZnIn deposits in NewBrunswick, Canadawas undertaken using commercially availablemethods. Indicator minerals of the deposits include: cassiterite, wolframite, and molybdenite, as well as gangue minerals topaz, chalcopyrite, galena, sphalerite, arsenopyrite, pyrite, and loellingite and secondary Pb minerals beudantite, anglesite, plumboferrite, and plumbogummite in the 0.25-0.5mmheavy mineral (> 3.2 specific gravity) fraction, and fluorite in the 0.25-0.5 mmmid-density (3.0-3.2 specific gravity) fraction. The presence of coarse (0.5-2.0 mm) indicator minerals in till close (< 1 km) to the deposits marks the close proximity to mineralization. Indicator elements in the < 0.063 mm fraction of till overlying and down ice of the deposits include Sn, W, Mo, Bi, Zn, and In. Pathfinder elements in till include Ag, As, Cd, Cu, Pb, Re, Te, and Tl. This study reports In values of < 0.02 to 13 ppmin the matrix of till overlying the deposit; values >5 ppm are some of the highest ever reported for till. Crown Copyright (C) 2016 Published by Elsevier B. V. This is an open access article under the CC BY-NC-ND license.
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