Core Assets Corp. announced the results and interpretation of a 3-Dimensional Magnetic Vector Inversion Model collected over the 2024 drilling area at the Silver Lime CRD-Porphyry Project (the "Silver Lime Project" or "Silver Lime"), central Blue Property (the "Blue Property"), Atlin Mining District of NW British Columbia. In early 2024, Core Assets contracted Fathom Geophysics to create a 3D magnetic inversion model utilizing the VTEM (Versatile Time Domain Electromagnetic) geophysical data collected over the Silver Lime CRD-Porphyry Project in 2021.

The 3D radial magnetic models at Silver Lime (isosurfaces; pale pink shapes, correlate well with highly chargeable zones below the Sulphide City, Pete's and Gally targets identified by the 2023 3D-IP (Three-Dimensional Induced Polarization) survey (high chargeability plotted as red and purple contours . In 2022, SLM22-006 drill-tested the Sulphide City Mo-Cu Porphyry to a true depth of 471m and encountered strong porphyry-style alteration, veining and increased Mo and Cu grades upon intersecting the top of the highly chargeable core (80mV/V) near 320m true depth. The 3D radial magnetic models (isosurface; pale pink shape indicate a continuation of the Sulphide City Mo-Cu Porphyry Stock to depth where it connects to a larger magnetic body interpreted as the source intrusion .

This source intrusion measures 3.7-kilometres wide and appears to be feeding at least three additional interpreted porphyry stocks situated below the Pete's CRD and Amp targets, and 750m south of the Gally CRD Target. Interpreted mineralized porphyry stocks (pale pink shapes) along the Pete's ­ Sulphide City ­ Gally Trend are associated with overlapping chargeable and conductive anomalies along their margins that are interpreted as probable zones of high-grade Zn-Fe-Cu massive sulphide skarn deposits. All prospective porphyry targets, including the interpreted main source intrusion, are bound by major deep- seated faults within a 13.7km2 area These structures are believed to have acted as the main pathways for the distal and widespread, high-grade massive sulphide Ag-Zn-Pb-Cu±Au carbonate replacement mineralization at the Silver Lime Project.