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- #61
Thread Owner
In reply to an earlier remark, "Phase angles all over the place".
Phase angle is used to discriminate between metals in FDEM (VLF) metal detectors. Phase angles are both stable and conformal. Conformal in this context means you can see the orderly definition of mineralization as a DIGHEM survey flightline crosses a deposit.
When a flightline is shown in graphic form, gold bearing zones are well defined.
Here's an example:

This example shows gold mineralization (in yellow) extending down from the 30 degree line. Thirty degrees is considered as copper. Less than 30 is a mixture of copper and gold. The red line is Resistivity. As resistivity decreases, conductivity increases. So it is understood that a mineral deposit is conductive and therefore is a low resistivity. Low resistivity combined with low phase angle has the greatest probability of being a gold deposit. This deposit is about 2400 feet across. Gold is supported by the fact this survey line is on a gold mine. This district has been mined over the past 200 years using placer methods. The lode deposit has not been discovered until now. This is the first time I have published this.
Please understand also, raw gold is a mixture of different metals and minerals. The purity of gold increases below the 10 degree phase line as per US Patent info that is in the public domain.
Notice, the grade of the gold diminishes toward the edges of the deposit. This is in keeping with the naturally expected degradation of purity from the center of the deposit into surrounding copper as expected in a normal copper-silver-gold deposit. There are exceptions. This deposit is in a fissure vein. The vein degrades out to wall rock having little or no mineralization.
- Geowizard
Phase angle is used to discriminate between metals in FDEM (VLF) metal detectors. Phase angles are both stable and conformal. Conformal in this context means you can see the orderly definition of mineralization as a DIGHEM survey flightline crosses a deposit.
When a flightline is shown in graphic form, gold bearing zones are well defined.
Here's an example:

This example shows gold mineralization (in yellow) extending down from the 30 degree line. Thirty degrees is considered as copper. Less than 30 is a mixture of copper and gold. The red line is Resistivity. As resistivity decreases, conductivity increases. So it is understood that a mineral deposit is conductive and therefore is a low resistivity. Low resistivity combined with low phase angle has the greatest probability of being a gold deposit. This deposit is about 2400 feet across. Gold is supported by the fact this survey line is on a gold mine. This district has been mined over the past 200 years using placer methods. The lode deposit has not been discovered until now. This is the first time I have published this.
Please understand also, raw gold is a mixture of different metals and minerals. The purity of gold increases below the 10 degree phase line as per US Patent info that is in the public domain.
Notice, the grade of the gold diminishes toward the edges of the deposit. This is in keeping with the naturally expected degradation of purity from the center of the deposit into surrounding copper as expected in a normal copper-silver-gold deposit. There are exceptions. This deposit is in a fissure vein. The vein degrades out to wall rock having little or no mineralization.
- Geowizard







