Zobrazeno 1 - 10
of 15
pro vyhledávání: '"C. E. Beckett-Brown"'
Publikováno v:
Economic Geology. 118:411-431
Case studies around porphyry Cu deposits in the glaciated regions of the Canadian Cordillera have identified the indicator mineral signatures of these deposits in till samples and demonstrated that these are useful methods for porphyry Cu exploration
As the exploration for porphyry Cu-Au-Mo deposits has become increasingly challenging, the development of more effective techniques directed at detecting buried deposits has become critical. One methodology is to focus on key minerals, one of which i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ac23f2164e40de9755b273c2db956eac
https://doi.org/10.4095/331349
https://doi.org/10.4095/331349
Autor:
M B McClenaghan, D M Brushett, C E Beckett-Brown, R C Paulen, J M Rice, A Haji Egeh, A Nissen
Indicator mineral research is currently being undertaken in partnership with the Nova Scotia Department of Natural Resources and Renewables at the Brazil Lake lithium-cesium-tantalum (LCT) pegmatites in southwest Nova Scotia as part of the Geological
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::de894e46401b9248bd05279389a9af15
https://doi.org/10.4095/331686
https://doi.org/10.4095/331686
Autor:
C E Beckett-Brown, J A Kidder
A detailed geochemical sampling survey at the remote Casino porphyry Cu-Mo-Ag-Au deposit in west central Yukon is described. This new sampling follows-up on previous sampling around the deposit by the Geological Survey of Canada (GSC) in 2017. In lat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::093eb008b3b76a8ffc155d1881e7769f
https://doi.org/10.4095/331831
https://doi.org/10.4095/331831
Autor:
J A Kidder, M B McClenaghan, M I Leybourne, M W McCurdy, P Pelchat, D Layton-Matthews, C E Beckett-Brown, A Voinot
This open file reports geochemical data for stream and groundwater samples collected around the Casino porphyry Cu-Au-Mo deposit, one of the largest and highest-grade deposits of its kind in Canada. The calc-alkaline porphyry is hosted in a Late Cret
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62474a3a3de5723c466bb988c990c13d
https://doi.org/10.4095/328862
https://doi.org/10.4095/328862
Colour, texture, and chemistry were used to determine the source of tourmaline grains in local surficial (detrital) sediments from two Canadian porphyry systems (Woodjam and Casino). Tourmaline from porphyry bedrock is generally dark brown to black.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c28fb825b7ccf0382d063b5d8c21a51
https://doi.org/10.4095/327989
https://doi.org/10.4095/327989
Autor:
M B McClenaghan, S G Casselman, C E Beckett-Brown, RG Garrett, Matthew I. Leybourne, P Pelchat, M W McCurdy
We report results of a detailed indicator mineral and geochemical study of the Casino calc-alkaline porphyry Cu-Au-Mo deposit in the unglaciated terrain of west-central Yukon. It is one of the largest and highest-grade porphyry Cu-Au-Mo deposits in C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9f6faf54abbaf550212a8dac1270e3b
https://doi.org/10.4095/327987
https://doi.org/10.4095/327987
This open file reports the results of an indicator mineral case study carried out around the Casino porphyry Cu-Mo-Au deposit in the unglaciated terrain of the west central Yukon. The research was part of the Geological Survey of Canada's (GSC) Targe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e07d6296beed5e188219bd9abef10b6b
https://doi.org/10.4095/322191
https://doi.org/10.4095/322191
Tourmaline has long been regarded as a petrogenetic indicator of its host environment, but its genesis in mineralized porphyry systems is poorly understood. Based on chemical and physical properties, tourmaline possesses essential features to be an e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6913c7cb35d9b0510719b4dac3b94de
https://doi.org/10.4095/313669
https://doi.org/10.4095/313669
Autor:
M B McClenaghan, C E Beckett-Brown, RG Garrett, S G Casselman, M W McCurdy, Matthew I. Leybourne, P Pelchat
This paper reports preliminary results for a detailed indicator mineral and geochemical study of the Casino porphyry Cu-Au-Mo-Ag deposit, one of the largest and highest grade porphyry deposits in Canada. The calc-alkaline porphyry is hosted in a Late
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d98a922ceadc7dd40074c96507876008
https://doi.org/10.4095/313667
https://doi.org/10.4095/313667