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Golden Rapture Mining Identifies Strong Linear Anomalies throughout the Project Area from Airborne Magnetic Survey
Edmonton, Alberta – TheNewswire - May 28, 2025. Golden Rapture Mining Corporation (CSE-GLDR) is pleased to announce the results of the recently completed low-al
About this update from Golden Rapture Mining Corporation
[{"type":"text","content":"Edmonton, Alberta – TheNewswire - May 28, 2025. Golden Rapture Mining Corporation (CSE-GLDR) is pleased to announce the results of the recently completed low-altitude, high-resolution drone magnetic surveys of its 100% owned 10,000+ acre Phillips Gold Project, Rainy River District, Ontario. The (UAV) airborne magnetics survey was conducted by Rosor Exploration of Burlington, Ontario. It was flown at a height of 50 meters with a MagArrow magnetometer by Geometrics suspended from a Matrice 300 RTK drone along 50-meter spaced lines with a total of 313 line-kilometers covering an area of approximately 16.7 km2 in size. The results identified new high-priority targets, confirming that the survey area is dominated by strong linear anomalies throughout the project area, with the strongest occurring in the northeast corner. It was also noted by Rosor Exploration in their report that there is intense deformation and folding in the eastern part of the survey area. Figure 1. Map of property showing survey border area in green New High-Priority Exploration Targets Discovered Richard Rivet said: “To our surprise, strong linear anomalies were found throughout the project area, with the strongest occurring in the northeast corner and not from the Combined Mine area itself, where all the drilling has occurred so far with great results as high as 285.00 g/t Au.” These significant anomalies trend E-W in the southwest corner before trending NE-SW to the northeast and range in amplitude from 250-100 nT, with the strongest anomalies localized in a 1 km band from 426730 E 5454600N to 428175 E 5456650 N. The maximum along this belt is located near the centre of the survey area (427130 E 5455120 N) with an amplitude of 1,800 nT. Figure 2. Drone Magnetic survey map (total magnetic intensity – reduced to pole) There are weakly magnetic N-S trending linear anomalies located in the middle of the survey area. Of importance is that these are overprinted by the stronger magnetic anomalies seen in the figures, implying that they are from a previous deformation event. There is a clear contrast on the eastern edge of the survey between the magnetically strong belt and a strong magnetic low, which is likely the boundary between the felsic volcanics to the east and the mafic volcanics that dominate the survey area. Figure 3. Image of the drone magnetic ...