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- W2185200329 abstract "The electrical conductivity mechanisms have been determined for six mineralized sericite schist specimens cut from a large sample collected from the Gold Lake area of the Yellowknife mining district, Northwest Territories. This work consists of analysis and interpretation of 3-D electrical resistivity measurements. The sample was selected to characterize the resistivity of the alteration zone and determine the effect of crosscutting veins and the sections of fine-grained sulphides oriented parallel to foliation. The purpose of this paper is to document results of the electrical resistivity determinations obtained to assist interpretation of electromagnetic surveys currently being conducted in the area. The bulk electrical resistivities (ρr) of the six specimens investigated in this study are in the range of 5.9–140Ω·m with anisotropy values ranging from 3:1 to 7:1. The arsenopyrite-filled fractures showed the lowestρr values (5.9–17Ω·m). Current Research 2002-C5 1 S. Connell and N. Scromeda-Perez 1 Contribution to the 2000-2001 Yellowknife Mining District, Northwest Territories Exploration Science and Technology (EXTECH-III) Initiative. Resume : On a determine les mecanismes de la conductivite electrique dans six specimens de schiste a sericite mineralise extraits d’un gros echantillon recueilli dans la region du lac Gold, dans le district minier de Yellowknife (Territoires du Nord-Ouest). Le travail consistait a analyser et a interpreter les mesures de la resistivite electrique en trois dimensions. L’echantillon a ete choisi de maniere a pouvoir representer la resistivite de la zone d’alteration ainsi qu’a permettre de determiner les effets sur la resistivite de veines discordantes et d’intervalles de sulfures a grain fin paralleles a la foliation. Ce document presente les resultats des analyses de resistivite electrique obtenus dans le but de faciliter l’interpretation des leves electromagnetiques que l’on effectue presentement dans la region. Les six specimens analyses dans le cadre de cette etude presentent tous une valeur de la resistivite electrique apparente (ρr) comprise entre 5,9 et 140 Ω·m et des valeurs d’anisotropie s’echelonnant entre 3/1 et 7/1. Les fractures a remplissage d’arsenopyrite presentaient les plus basses valeurs de ρr (de 5,9 a 17 Ω·m)." @default.
- W2185200329 created "2016-06-24" @default.
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- W2185200329 date "2002-01-01" @default.
- W2185200329 modified "2023-09-30" @default.
- W2185200329 title "Electrical conductivity mechanism of sericite schist from Gold Lake area of the Yellowknife mining district, Northwest Territories" @default.
- W2185200329 cites W2183501599 @default.
- W2185200329 doi "https://doi.org/10.4095/213168" @default.
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