Zobrazeno 1 - 10
of 20
pro vyhledávání: '"I M Kjarsgaard"'
The microscopic composition of thirteen samples of epidote related to porphyry Cu mineralization was mapped using laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) at the Geological Survey of Canada. The objective of this resear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07e61a1c269fd92568c8da224ea69f2d
https://doi.org/10.4095/331671
https://doi.org/10.4095/331671
Autor:
A. Plouffe, I. M. Kjarsgaard, T. Ferbey, D.H.C. Wilton, D. C. Petts, J. B. Percival, C. H. Kobylinski, R. McNeil
Publikováno v:
Economic Geology.
At the Gibraltar porphyry Cu-Mo deposit in south-central British Columbia, Canada, geochemical and mineralogical anomalies in till around a cluster of mineral occurrences form amoeboid-shaped dispersal patterns controlled by three phases of ice movem
Bedrock samples were collected from the Broken Hammer Cu-Ni-PGE-Au deposit and surrounding host lithologies by the Geological Survey of Canada (GSC) to determine which indicator minerals are indicative of this deposit type. The deposit is known for w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d94ce7201dbdd3333ab1148a1f2e733
https://doi.org/10.4095/308213
https://doi.org/10.4095/308213
Autor:
M B McClenaghan, I M Kjarsgaard, S A Averill, D Layton-Matthews, D Crabtree, G Matile, I McMartin, M Pyne
The Geological Survey of Canada (GSC) conducted an indicator mineral study around the komatiite-associated Ni-Cu deposits in the northern Thompson Nickel Belt, northern Manitoba, to document the indicator mineral signatures of the Ni-Cu deposits. Sam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0bab4bc2cdc34aa598aae9a487fe615
https://doi.org/10.4095/292543
https://doi.org/10.4095/292543
Glacial history studies and analysis of heavy mineral separates from glacial sediments (till and eskers) were undertaken in theBoothia mainland area of central Nunavut. Mapping of surficial macroforms and glacial striae has shown a complex, four phas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86290d77d19130c630441d4a819ab5ae
https://doi.org/10.4095/248154
https://doi.org/10.4095/248154