Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ...
Appendix 5-Photo 1. Photograph of mountainous terrain in Fraser Plateau of south-central British Columbia, in western Canada. In this type of terrain, till can be sampled at higher elevations from thin till veneers (Tv) and thicker till blankets (Tb) on valley walls and from thick sediment sequences...
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Geological Society of London
2023
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ftdatacite:10.6084/m9.figshare.23932392.v1 2023-10-01T03:54:03+02:00 Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... McClenaghan, M. B. Paulen, R. C. Smith, I. R. Rice, J. M. Plouffe, A. McMartin, I. Campbell, J. E. Lehtonen, M. Parsasadr, M. Beckett-Brown, C. E. 2023 https://dx.doi.org/10.6084/m9.figshare.23932392.v1 https://geolsoc.figshare.com/articles/journal_contribution/Review_of_till_geochemistry_and_indicator_mineral_methods_for_mineral_exploration_in_glaciated_terrain/23932392/1 unknown Geological Society of London https://dx.doi.org/10.6084/m9.figshare.23932392 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Geology FOS Earth and related environmental sciences ScholarlyArticle article-journal Journal contribution Text 2023 ftdatacite https://doi.org/10.6084/m9.figshare.23932392.v110.6084/m9.figshare.23932392 2023-09-04T13:41:00Z Appendix 5-Photo 1. Photograph of mountainous terrain in Fraser Plateau of south-central British Columbia, in western Canada. In this type of terrain, till can be sampled at higher elevations from thin till veneers (Tv) and thicker till blankets (Tb) on valley walls and from thick sediment sequences in valleys filled with till and alluvium (A), using overburden drilling. Appendix 5-Photo 2. Oblique photo showing an area affected by marine incursion near Baker Lake in Arctic Canada. The thick black dashed line indicates the inland limit of marine incursion. Till unmodified by wave action can be collected above this limit (west side of photo). Till surfaces topographically lower than this limit may be significantly reworked and winnowed by waves and be overlain by a bouldery mantle or beach shingles of poorly sorted debris (washed till). Raised beach sediments derived from winnowed till are not suitable sample sites because of significant reworking of till and significant transport distances of sediment in ... Text Arctic Baker Lake DataCite Metadata Store (German National Library of Science and Technology) Arctic British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Canada Raised Beach ENVELOPE(163.783,163.783,-74.983,-74.983) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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Geology FOS Earth and related environmental sciences |
spellingShingle |
Geology FOS Earth and related environmental sciences McClenaghan, M. B. Paulen, R. C. Smith, I. R. Rice, J. M. Plouffe, A. McMartin, I. Campbell, J. E. Lehtonen, M. Parsasadr, M. Beckett-Brown, C. E. Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... |
topic_facet |
Geology FOS Earth and related environmental sciences |
description |
Appendix 5-Photo 1. Photograph of mountainous terrain in Fraser Plateau of south-central British Columbia, in western Canada. In this type of terrain, till can be sampled at higher elevations from thin till veneers (Tv) and thicker till blankets (Tb) on valley walls and from thick sediment sequences in valleys filled with till and alluvium (A), using overburden drilling. Appendix 5-Photo 2. Oblique photo showing an area affected by marine incursion near Baker Lake in Arctic Canada. The thick black dashed line indicates the inland limit of marine incursion. Till unmodified by wave action can be collected above this limit (west side of photo). Till surfaces topographically lower than this limit may be significantly reworked and winnowed by waves and be overlain by a bouldery mantle or beach shingles of poorly sorted debris (washed till). Raised beach sediments derived from winnowed till are not suitable sample sites because of significant reworking of till and significant transport distances of sediment in ... |
format |
Text |
author |
McClenaghan, M. B. Paulen, R. C. Smith, I. R. Rice, J. M. Plouffe, A. McMartin, I. Campbell, J. E. Lehtonen, M. Parsasadr, M. Beckett-Brown, C. E. |
author_facet |
McClenaghan, M. B. Paulen, R. C. Smith, I. R. Rice, J. M. Plouffe, A. McMartin, I. Campbell, J. E. Lehtonen, M. Parsasadr, M. Beckett-Brown, C. E. |
author_sort |
McClenaghan, M. B. |
title |
Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... |
title_short |
Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... |
title_full |
Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... |
title_fullStr |
Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... |
title_full_unstemmed |
Review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... |
title_sort |
review of till geochemistry and indicator mineral methods for mineral exploration in glaciated terrain ... |
publisher |
Geological Society of London |
publishDate |
2023 |
url |
https://dx.doi.org/10.6084/m9.figshare.23932392.v1 https://geolsoc.figshare.com/articles/journal_contribution/Review_of_till_geochemistry_and_indicator_mineral_methods_for_mineral_exploration_in_glaciated_terrain/23932392/1 |
long_lat |
ENVELOPE(-125.003,-125.003,54.000,54.000) ENVELOPE(163.783,163.783,-74.983,-74.983) |
geographic |
Arctic British Columbia Canada Raised Beach |
geographic_facet |
Arctic British Columbia Canada Raised Beach |
genre |
Arctic Baker Lake |
genre_facet |
Arctic Baker Lake |
op_relation |
https://dx.doi.org/10.6084/m9.figshare.23932392 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.6084/m9.figshare.23932392.v110.6084/m9.figshare.23932392 |
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1778521325688586240 |