Jaxon Mining Inc. announced the preliminary results from the first in a series of Bulkley granite intrusion and sulfide quartz vein "rock" dating and zircon thermometry (melting temperatures) studies from Jaxon's 100% controlled Netalzul Mountain Project at its Hazelton Property in the Skeena Arch. The study results will allow Jaxon to vector 2021 drilling targets in on the hotter, younger, and more extensive Cu, Ag and Au polymetallic zones. The studies further describe the setting of the high-grade polymetallic Ag-Au-Cu-Zn-Pb Intermediate Sulfidation (IS) deposits at Netalzul. The deposits and their distal porphyritic sources were formed approximately 61.60 to 63.68 million years ago in the Late Cretaceous to Early Tertiary (Paleocene) period. This places the formation of the mineralized zones at Netalzul within a comparable age range and setting (underlain by rocks from the Stikine terrain) of other previously discovered polymetallic deposits in the region (i.e. the Blackwater Au/Ag project). Jaxon's work further indicates an eastward migration of the Coast Range continental arc magmatism across the Skeena Arch area. Daisy North Contact Zone: artisanal working zone, up to 1000m long and 12m wide, structure-controlled fault/shear zone developed along contact between granite and hornfelsed latite. 1.5m chip sample assayed 4577 g/t Ag, 3.04% Cu, 4.52% Zn, 3.40% Pb, 2.08% Sb. Grab samples assayed up to 5301 g/t Ag, 37.85% Zn, 29.18% Pb, 3.35% Cu, 2.32% Sb. Soil geochemical and aeromagnetic studies confirm zone extension. Two rock samples (Ellen-1 and A0020746) from within this zone have been subjected to age dating studies. Daisy South Adit Zone: artisanal adit area, up to 1000m long and 150m wide with multiple 2-5m wide sulfide quartz veins all fault-controlled and occur in a hydrothermally induced magnetite destruction area within strong magnetic granite. 2m outcrop samples assayed 486 g/t Ag, 1.40 g/t Au, 1.40% Cu. One rock sample from sulfide quartz vein has been collected for age dating. Neither zircon nor molybdenite mineral are available for dating study. 3. Daisy East Zone: occurs in a glacier retreating from the top of Netalzul, up to 1000m long and 2m wide within clay altered granite. Grab samples assayed 275 g/t Ag, 0.8 g/t Au, 1.53% Cu. One rock sample (A0027520) from Bulkley intrusive has been subjected to zircon age dating. Three of four rock samples (A0020746, A20027520 and Ellen-1) with available zircon grains collected (>150 grains) have been subjected to LA-ICMP Zircon U-Pb dating, chemistry composition and cathodoluminescence (CL) images studies. The CL images indicate the majority of these zircons are magmatic zircons and only a few of them have inherited cores. Most of these zircons contain inclusions of either minerals or fluids, which show these zircons were formed from hydrous magma and may be the result of late phase magma crystallization. The zircon concord ages of A0020746A20027520 and Ellen-1 are 63.67±0.21, 62.99±0.20 and 63.68 ±0.20, respectively. The weighted average 206U/238U ages of samples A0020746A20027520 and Ellen-1 are 63.70±0.3762.92±0.50 and 63.68±0.56, respectively. The dating age range is 62.9-63.7 within the range of errors. Three granite rocks' dating results from the Red Springs project in 2019 are also listed in Table 3 for discussion purposes. The Bulkley intrusive suite from Cretaceous to Eocene in the Stikine terrain is associated with a series of Cu-Mo porphyry deposits and Ag polymetallic epithermal deposits including past produced Cu and Ag mines including the Huckleberry Cu mine, Silver Standard, Blackwater and Equity Silver mines. The ages of the Bulkley intrusive suite have been reported to be 88 to 67 Ma in the Blackwater deposit area (Looby, 2015). The dated ages of Bulkley intrusive suite at the Hazelton property and the Rocher de Boule area show a similar eastward migration of the Coast Range continental arc magmatism to that in the Blackwater deposit area at that time. Zircon (Zr[Hf]SiO4) is a common accessory mineral in granitoid rocks including those that generate and host porphyry copper deposits. Zircon can indicate the evolution of its host magma and provide information on that magma's ability to generate a porphyry copper deposit (Bouzari et al., 2020). The trace and rare elements composition, the Th/U ratio, Yb/Gd ration, FMQ/Eu/Eu ratio, Ti-in-Zircon temperature have been studied using LA-ICP-MS. Majority zircons (>95%) from all three samples have lower Th/U (<0.45) and higher Yb/Gd (>15), which shows the typical chemistry characters of zircon formed from mineralized magma (Bouzari, et al., 2020). Oxygen and Deuterium Isotope Analysis shows oxygen fugacity buffered by fayalite-magnetite-quartz (FMQ) in the majority zircons are greater than +1.0 with Eu/Eu >0.45 show the oxidized magma features. Ti-in-zircon temperatures studies show the crystallization temperatures of samples A0020746A20027520 and Ellen-1 are C - 691° C - 756°C-683°C - 720°C 681°and C - 777°C, respectively and consistent with lower model temperatures of ca. 750C to 600C for most mineralized porphyry intrusives and are also consistent with zircon crystallization in near-eutectic conditions close to the solidus of hydrous granite.