District Copper Announces Results of Airborne Survey on Copper Keg Property
correlation to the two areas of coincident sporadic copper mineralization and anomalous chargeability. A 2,000m wide by 3,000m long positive magnetic signature hosted in Nicola Volcanics and Guichon Creek intrusive rocks spans the Barnes Creek fault. The survey has identified a circular magnetic anomaly underlying, the Kamloops Group, the source/cause of which is unknown at this time. The data suggests that the late Kamloops Group is bounded on the north and south by NE trending structures. The positive magnetic signatures are interpreted to be due to the presence of magnetite related to the potassic phase of a porphyry copper system. Magnetic Vector Inversion of the magnetic data is in progress to locate late-stage intrusive bodies exhibiting positive magnetic signatures within the chargeability anomalies in advance of a drilling program. The survey was flown by Precision GeoSurveys Inc. located in Langley B.C., utilizing a 100 m line
spacing on a heading of 178°/358°; tie lines were flown at 1000 m spacing on a heading of 088°/268°. The geodetic system used for the geophysical survey was WGS 84 in UTM Zone 10N. A total of 360-line
km was completed. After all data were collected, several procedures were undertaken to ensure that the
data met a high standard of quality. Magnetic and radiometric data recorded by the AGIS were
converted into Geosoft or ASCII file formats using Nuvia Dynamics software. Further processing was
carried out using Geosoft Oasis Montaj 2021.2.1.11 geophysical processing software along with
proprietary processing algorithms.