| Reference Type | Journal (article/letter/editorial) |
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| Title | Dispersion Trends of Elements and Indicator Pebbles in Glacial Till around Mt. Pleasant, New Brunswick, Canada |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Szabo, N. L. | Author |
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| Govett, G. J. S. | Author |
| Lajta, E. Z. | Author |
| Year | 1975 (September 1) | Volume | 12 |
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| Issue | 9 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e75-139Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474608 | Long-form Identifier | mindat:1:5:474608:3 |
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| GUID | 0 |
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| Full Reference | Szabo, N. L., Govett, G. J. S., Lajta, E. Z. (1975) Dispersion Trends of Elements and Indicator Pebbles in Glacial Till around Mt. Pleasant, New Brunswick, Canada. Canadian Journal of Earth Sciences, 12 (9) 1534-1556 doi:10.1139/e75-139 |
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| Plain Text | Szabo, N. L., Govett, G. J. S., Lajta, E. Z. (1975) Dispersion Trends of Elements and Indicator Pebbles in Glacial Till around Mt. Pleasant, New Brunswick, Canada. Canadian Journal of Earth Sciences, 12 (9) 1534-1556 doi:10.1139/e75-139 |
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| In | (1975, September) Canadian Journal of Earth Sciences Vol. 12 (9) Canadian Science Publishing |
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| Abstract/Notes | Studies on the composition of glacial till around the Mt. Pleasant Mo-W-Bi-Cu-Sn-Zn mineralization show that the host rock at Mt. Pleasant, which can be regarded as a point source, can be detected by pebble counts in the till 7 km down-ice from Mt. Pleasant. Analysis of various size fractions of glacial till demonstrate that glacial transport can, in some situations, actually be an advantage in the use of exploration geochemical techniques. Whereas dispersion trains of Cu, Pb, and Zn in the fine fractions of till can be traced for only 2 to 5 km from the mineralized source, they extend for more than 16 km in the coarse fraction of the till. Analysis of the coarse fraction of glacial till is clearly a potentially powerful reconnaissance-scale exploration technique. |
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