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Brixton Metals Corp V.BBB

Alternate Symbol(s):  BBBXF

Brixton Metals Corporation is a Canada-based exploration company focused on the advancement of its mining projects. The Company is engaged in the acquisition and exploration and evaluation of resource assets located in British Columbia and Ontario, Canada, and Montana, USA. Its projects include the Thorn copper-gold-silver-molybdenum Project, Hog Heaven copper-silver-gold Project, Langis-Hudson Bay silver-cobalt-nickel Project and Atlin Goldfields Project. Its wholly owned Thorn Project is a 2,867 square kilometer mineral claim group. The Thorn Project is located in northwestern British Columbia, Canada, approximately 90 km ENE from Juneau, Alaska. The Hog Heaven Project consists of over 10 sections of private land. The project is located in Northwest Montana, USA. The Langis and HudBay Silver-Cobalt-Nickel projects are located within the historic silver-cobalt mining camp over 500 km north of Toronto, Canada. The Atlin Goldfields Project is in Northwest British Columbia, Canada.


TSXV:BBB - Post by User

Bullboard Posts
Post by Blazesbon Jun 11, 2020 7:56pm
227 Views
Post# 31141090

'Induced Polarization Geophysics' Defined

'Induced Polarization Geophysics' DefinedSo, Brixton announces no driling near hole 150.  However to identify possible new drilling targets near 150 it is conducting these tests. If like me you are wondering what this term means here, from Wikipedia, it is:

Induced polarization (IP) is a geophysical imaging technique used to identify the electrical chargeability of subsurface materials, such as ore.[1][2]
 
The polarization effect was originally discovered by Conrad Schlumberger when measuring the resistivity of rock.[3]
 
The survey method is similar to electrical resistivity tomography (ERT), in that an electric current is transmitted into the subsurface through two electrodes, and voltage is monitored through two other electrodes.
 
Induced polarization is a geophysical method used extensively in mineral exploration and mine operations. Resistivity and IP methods are often applied on the ground surface using multiple four-electrode sites. In an IP survey, in addition to resistivity measurement, capacitive properties of the subsurface materials are determined as well. As a result, IP surveys provide additional information about the spatial variation in lithology and grain-surface chemistry.
 
The IP survey can be made in time-domain and frequency-domain mode:
 
In the time-domain induced polarization method, the voltage response is observed as a function of time after the injected current is switched off or on. [4]
 
In the frequency-domain induced polarization mode, an alternating current is injected into the ground with variable frequencies. Voltage phase-shifts are measured to evaluate the impedance spectrum at different injection frequencies, which is commonly referred to as spectral IP.
 
The IP method is one of the most widely used techniques in mineral exploration and mining industry and it has other applications in hydrogeophysical surveys, environmental investigations and geotechnical engineering projects.[5]
 
 
Measurement methods
Time domain
 
Typical transmitted current waveform and potential response for time domain resistivity and induced polarization measurements.
Time-domain IP methods measure considers the resulting voltage following a change in the injected current. The time domain IP potential response can be evaluated by considering the mean value on the resulting voltage, known as integral chargeability[2] or by evaluating the spectral information and considering the shape of the potential response, for example describing the response with a Cole-Cole model.[6]
 
Frequency domain
Main article: Spectral induced polarisation
Frequency-domain IP methods uses alternating currents (AC) to induce electric charges in the subsurface, and the apparent resistivity is measured at different AC frequencies.
 
See also
DC impedance spectroscopy
AC impedance spectroscopy
Electrical resistivity measurement of concrete
Geophysical Imaging
 
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