Tillkännagivande • May 08

Irving Resources Inc. Encounters High-Grade Gold in its First Drill Hole at the East Yamagano Project, Kyushu, Japan and Receives Additional Results from the Omu Project

Irving Resources Inc. announced that the first diamond drill hole completed at the East Yamagano epithermal gold-silver vein project, Kyushu, Japan, has encountered high-grade gold mineralization. At a down hole depth of 184.0 metres, a 5.0-metre interval grading 9.62 gpt Au including 1.0 metre grading 45.90 gpt Au was encountered in hole 23SY-001. A second interval of 1.33 metres grading 5.81 gpt Au was encountered beginning at 407.0 metres down hole depth. Both zones of mineralization are comprised of stockwork quartz-carbonate veinlets measuring a few millimetres up to a couple centimetres width. Visible gold was observed in fractures. This style of veining was reportedly common in the adjacent historical Yamagano Mine. True widths of the mineralized intervals in hole 23SY-001 cannot be determined at this time. Hole 23SY-001 was collared approximately 550 metres east of the easternmost main historical Yamagano Mine workings and was drilled in a 30° east northerly direction at -55 degrees. This hole targeted a steeply oriented zone of resistivity evident in AMT data. Volcanic rocks were encountered over the entire length of the hole to its terminal depth of 549.7 metres. Hydrothermal silicification and argilization were observed down most of the length of the hole and appear coincident with the targeted AMT resistive zone. In addition to the gold intervals discussed above, two lower grade stockwork vein intervals were encountered deeper in the hole. The area where 23SY-001 is located is partly covered by young, post-mineral volcanic rocks making this high-grade intercept a blind intercept. It should be noted that the silver-to-gold ratio of all intercepts is generally very low, less than 1, a characteristic of gold veins at the nearby Hishikari deposit. Irving finds these early results very encouraging and provides supporting evidence that a potential extension of the Yamagano vein system might be found under cover within the East Yamagano project. Description of the Yamagano Mining License: The Yamagano mining district, situated approximately 11 km southwest of the large, high-grade Hishikari gold mine, is host to numerous historic gold mine workings, some dating back to 1640AD during the early Edo Period in Japan. Mining focused on a multitude of high-grade epithermal gold veins hosted by volcanic rocks blanketing this region. Gold veins at Yamagano appear associated with a particular geophysical feature, an area of anomalously high gravity, thought to represent a buried uplift, or dome, in underlying denser basement sedimentary rocks. Such a geologic feature is believed to have focused gold-depositing hydrothermal fluids to ascend into overlying faults and fissures where they formed extensive high-grade vein networks. A gravity high was recognized very early as an important general control in the so-called Hokusatsu gold deposits including Kushikino gold mine (56 tonnes or 1.80 Moz Au produced) situated approximately 39 km southwest of Yamagano. Based upon this geologic model, initial targeting of the famous Hishikari deposits (more than 260 tonnes or 8.3 Moz Au produced) was driven largely by recognition of an anomalous gravity high underlying that area. Irving believes the gravity high under East Yamagano reflects a buried dome of basement rock and that, given the large footprint of this feature, there is prospectivity for a potential vein system. Additional Results from the Omu Project: Maruyama Initial Drill Test: Irving drilled one diamond drill hole, 23MAR-001B, testing a breccia pipe underneath the Maruyama silica sinter deposit at the Company's 100% controlled Omu gold-silver project, Hokkaido, Japan. A resistive zone forming the core of the pipe was identified in CSAMT data. This hole was oriented to 325° northwest at an angle of -52 degrees and reached a depth of 542.0 metres. Although this hole did not encounter high-grade precious metal mineralization, five strongly anomalous intervals of mineralization were encountered ranging from 4 to 58 metres in length (please refer to the table below). All of these zones of mineralization were associated with variably hydrothermally silicified diatreme breccia material. Given the very large size of the Maruyama sinter and its underlying breccia pipe, Irving is intrigued by these early results. Additional drill targets are being considered to follow up on these results. East Omui Extension Drill Test: Three diamond drill holes, 23OMI-003, 23OMI-004 and 23OMI-005m were completed in an area east of the Omui mining license testing for vein extensions. Various steeply oriented resistive anomalies observed in CSAMT data were targeted. Narrow vein interecepts were encountered in each of these three holes, albeit generally lower grade and narrower than veins encountered in recent drilling within the centre area of the Omui mining license (please refer to the table below). Best results from each hole include (true widths are not known at this time): 1.00 m grading 7.13 gpt Au and 0.31 gpt Ag (7.13 gpt AuEq) in hole 23OMI-003; 1.00 m grading 1.47 gpt Au and 143.00 gpt Ag (3.26 gpt AuEq) in hole 23OMI-004; 0.70 m grading 2.85 gpt Au and 145.00 gpt Ag (4.66 gpt AuEq) in hole 23OMI-005. Also noteworthy, a 24.5 m silicified interval grading 0.40 gpt Au and 25.81 gpt Ag (0.72 gpt AuEq) was encountered at the top of hole 23OMI-004. Such shallow silicified rock is common to the west where it has been encountered in multiple drill holes around the Nanko area. Such rock is probably the erosional remains of a sinter terrace that once capped the feeder veins of Nanko. Irving is considering its next step for drilling in this area as well as other locations where veins are projected to extend beyond the Omui mining license. All samples discussed in this news release are ½ split sawn diamond core samples. Irving submitted samples to ALS Global, Perth, Australia for analysis. Au and Ag were analyzed by fire assay with AA finish. Overlimit samples were assayed by fire assay with gravimetric finish. Multielements were analyzed by mass spectrometry following four acid digestion. Irving routinely inserts standard and blank samples in assay batches submitted to the laboratory. Company staff are responsible for geologic logging and sampling of core. Au equivalent is calculated by adding Au (gpt) to Ag (gpt)/80.

Tillkännagivande • Aug 05

+ 1 more update

Irving Resources Announces Plans to Drill Omui Mine Site and Hokuryu in Third and Fourth Quarter of 2021; Provides Update on First and Second Quarter of 2021 Omu Sinter Drilling

The planned hole is expected to hit extensions of these veins. Nanko - One hole with test for deeper extensions of veins encountered in holes 20OMI-003, 20OMI-004 and 20OMI-005 last year. Most notably, hole 20OMI-003 encountered two veins, one grading 8.15 gpt Au and 147.29 gpt Ag over 1.76 m within a broader intercept of 3.55 gpt Au and 69.24 gpt Ag over 14.24 m and a second vein grading 21.65 gpt Au and 538.75 gpt Ag over 1.72 m including 56.10 gpt Au and 1,435.00 gpt Ag over 0.60 m. The planned hole will be drilled generally from north to south. A second hole will test an area northeast of holes 20OMI-006, 20OMI-007 and 20OMI-008 with vein intercepts of 2.39 m grading 5.22 gpt Au and 103.6 gpt Ag, 2.99 m grading 4.34 gpt Au and 26.8 gpt Ag and 2.00 m grading 3.98 gpt Au and 26.1 gpt Ag, respectively. The planned hole is designed to hit extensions of these veins. Hokuryu - Up to four holes are designed as a maiden drill test of the Hokuryu vein system. Mining was undertaken at Hokuryu for a few short years until it abruptly ceased in 1943. Irving’s recent controlled source audio-magnetotellurics geophysical program has identified a large corridor of resistive, presumably silicified, rock extending well beyond the historic mine area. These initial holes will test select areas along this corridor for vein extensions and new veins. Given the higher altitude at Hokuryu, completion of this program is dependant on weather. If holes remain uncompleted in 2021, Irving plans to complete this program as soon as possible in the spring of 2022. Honpi - Three holes will target extensions of veins encountered in some of the deeper holes completed over the past two years, particularly hole 19OMI-010 which encountered such notable intercepts including 3.00 m grading 27.0 gpt Au and 40.5 gpt Ag, 1.10 m grading 29.6 gpt Au and 36.5 gpt Ag, 3.77 m grading 12.3 gpt Au and 84.5 gpt Ag, and 1.20 m grading 7.8 gpt Au and 887.5 gpt Ag. The three planned holes will be positioned to test areas both east and west of hole 19OMI-010. One hole will test areas north of the historic Honpi vein where shallow holes completed in 2019 encountered high-grade veins. Intercepts include 1.00 m grading 19.25 gpt Au and 27.50 gpt Ag in hole 19OMI-001 and 1.80 m grading 6.05 gpt Au and 808.18 gpt Ag in hole 19OMI-002. The planned hole is expected to hit extensions of these veins. Nanko - One hole with test for deeper extensions of veins encountered in holes 20OMI-003, 20OMI-004 and 20OMI-005 last year. Most notably, hole 20OMI-003 encountered two veins, one grading 8.15 gpt Au and 147.29 gpt Ag over 1.76 m within a broader intercept of 3.55 gpt Au and 69.24 gpt Ag over 14.24 m and a second vein grading 21.65 gpt Au and 538.75 gpt Ag over 1.72 m including 56.10 gpt Au and 1,435.00 gpt Ag over 0.60 m. The planned hole will be drilled generally from north to south. A second hole will test an area northeast of holes 20OMI-006, 20OMI-007 and 20OMI-008 with vein intercepts of 2.39 m grading 5.22 gpt Au and 103.6 gpt Ag, 2.99 m grading 4.34 gpt Au and 26.8 gpt Ag and 2.00 m grading 3.98 gpt Au and 26.1 gpt Ag, respectively. The planned hole is designed to hit extensions of these veins. Hokuryu - Up to four holes are designed as a maiden drill test of the Hokuryu vein system. Mining was undertaken at Hokuryu for a few short years until it abruptly ceased in 1943. Irving’s recent controlled source audio-magnetotellurics geophysical program has identified a large corridor of resistive, presumably silicified, rock extending well beyond the historic mine area. These initial holes will test select areas along this corridor for vein extensions and new veins. Given the higher altitude at Hokuryu, completion of this program is dependant on weather. If holes remain uncompleted in 2021, Irving plans to complete this program as soon as possible in the spring of 2022. Earlier this year, Irving completed a series of four diamond drill holes at the Omu Sinter target. Holes 21OMS-002 and 21OMS-004 tested an area underlain by a broad expanse of silica sinter terrace in the southern part of this project area. Both holes encountered multiple long intervals of low grade gold and silver mineralization in bedded silica sinter and highly silicified, often hydrothermally brecciated, rocks beneath. Short intervals of higher grade mineralization were intersected. Remarkably, mineralized rock extends from surface to a vertical depth of approximtely 180 m. Although a high-grade feeder was not encountered, Irving believes potential for such a structure is good given the remarkable strength of this system and the presence of short, higher grade intervals in these holes. Irving plans to review this data and acquire additional structural data in an effort to identify a potential feeder structure prior to future drilling. Holes 21OMS-001 and 21OMS-003 tested CSAMT anomalies to the west and east of the main Omu Sinter trend, respectively. Although each hole encountered hydrothermally altered volcanic rocks, only anomalous Au and Ag values were encoutered. Therefore, Irving believes all mineralization at Omu Sinter occurs within the 1.2 km long north-south corridor now tested by multiple holes.

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