Duyuru • Jun 14

Collective Mining Ltd. Drills 56.60 Metres at 10.05 g/t Gold Equivalent Within 329.75 Metres at 3.10 g/t Gold Equivalent in Step Out Drilling Along the Contact Zone and Discovers a New Vein System at Apollo

Collective Mining Ltd. announce assay results for the first four holes drilled from newly constructed Pads 9 and 10 within the Apollo porphyry system (‘Apollo’) at the Guayabales project located in Caldas, Colombia. Apollo is a high-grade, bulk tonnage copper-silver-gold system, which owes its excellent metal endowment to an older copper-silver and gold porphyry system being overprinted by younger precious metal rich, carbonate base metal vein systems (intermediate sulphidation porphyry veins) within a magmatic, hydrothermal inter-mineral breccia and diorite porphyry bodies currently measuring 435 metres x 395 metres x 915 metres and open for expansion. The 2023 Phase II drilling program is advancing on schedule with twenty-two holes completed and results announced. A further seven holes have been drilled and await assay results from the lab. The objectives of the 2023 program are to define high-grade mineralization and the dimensions of the Apollo porphyry system near surface, expand the overall size of the system through step-out and directional drilling and drill test multiple new targets generated through grassroots exploration. Since the announcement of the discovery hole at Apollo in June 2022, a total of 54 drill holes (approximately 22,997 metres) have been completed and announced. This press release outlines results from four new holes testing the Apollo system. APC-50 and APC-51 were shallow holes drilled from Pad 9 and were designed to test gaps in the current mineralization block model. APC-52 and APC-53 were also drilled into untested areas from Pad 10 with APC-53 designed to step out along the Contact Zone (where the inter-mineral breccia ends at a contact with quartz diorite porphyry and is overprinted by multiple zones of sheeted CBM veins) to the northeast. APC-50 was the first hole ever drilled from Pad 9 and was completed at a maximum downhole depth of 264.20 metres. The hole was designed to test the eastward extension of the shallow portion of the central high-grade core of the deposit where no drilling had yet to be completed. The hole intercepted angular breccia commencing at 53.30 metres downhole (30 metres vertical) with sulphide mineralization flooding the matrix and consisting of chalcopyrite (up to 1.3%), pyrite (up to 1.5%) and 1% pyrrhotite. The complete assay results for the hole: 137.70 metres @ 2.60 g/t gold equivalent from 53.30 metres downhole (consisting of 0.74 g/t gold, 52 g/t silver and 0.66% copper) including: 28.55 metres @ 0.93% copper, 0.87 g/t gold and 79 g/t silver from 64.95 metres downhole. The hole outlines the presence of shallow mineralization with high copper grades and adds volume to the mineralization block model as this area had not previously been drill tested. As expected, a well-defined post mineral dyke was encountered from surface until the start of mineralization. APC-51 was drilled to the south from Pad 9 and was designed to test the extension of high-grade mineralization at depth within the southern portion of the Apollo system. The hole was drilled steeply to a maximum downhole depth of 435.65 metres and intercepted mineralized breccia from 163.30 metres downhole (160 metres vertical). Sulphides impregnating the breccia matrix consisted of chalcopyrite (up to 1%), pyrite (0.5%-1.5%) and pyrrhotite (1.2%) with assay results as follows: 112.55 metres @ 2.26 g/t gold equivalent from 163.30 metres downhole (consisting of 1.27 g/t gold, 22 g/t silver and 0.41% copper) including; 21.10 metres @ 3.25 g/t gold equivalent from 198.25 metres downhole which includes 0.72% copper. The hole confirms the continuity of the high-grade zone in the south part of the Apollo Porphyry System and again adds volume to the mineralization block model as the area had not been previously drill tested. APC-52 was the first shallow hole drilled to the west from Pad 10 and was designed to test for shallow mineralization in an untested area of the current mineralization block model. Surprisingly, the hole encountered a robust sheeted vein system directly from surface before transitioning to breccia until a downhole depth of 190.20 metres (160 metres vertical). The intercept begins with iron oxide veinlets and veins within porphyry host rock down to 20 metres followed by disseminated sulphides of pyrite (0.3%-1.0%) and pyrrhotite (0.1%-0.3%) within crackle brecciated quartz diorite associated with strong sericite-chlorite alteration to 56 metres downhole. From 56 metres, typical angular breccia was encountered with high-grade copper-silver-gold mineralization relating to a sulphide matrix of chalcopyrite (0.5%), pyrite (up to 1%) and 0.5% pyrrhotite. Additionally, the hole was overprinted by late stage CBM sheeted vein fluid with sphalerite and galena sulphides in association with carbonate. A zone with a higher percentage of chalcopyrite (+2%) was also encountered downhole from 157 metres to 182.80 metres with overall assay results as follows: 190.30 metres @ 2.46 g/t gold equivalent from 1.9 metres downhole (consisting of 1.19 g/t gold, 43 g/t silver and 0.41% copper) including; 34.05 metres @ 5.16 g/t gold equivalent from 56.95 metres downhole; and 25.80 metres @ 3.76 g/t gold equivalent from 157 metres downhole which includes 0.75% copper. APC-53 was drilled from Pad 10 to a final downhole depth of 602.45 metres and was designed to test the high-grade Contact Zone at depth to the northeast of previously announced Contact Zone holes APC-41, APC-42 and APC45. Surprisingly, the hole intercepted a robustly enriched zone of north-west and east-west trending overprinting sheeted CBM veins from surface to 145 metres depth. This new discovery is located above the Apollo porphyry system and has potential to be traced in all directions while adhering to a north-west to south-east trend. The mineralization in this new zone relates to sheeted and stockwork carbonate and base metal veinlets and veins with the principal sulphides consisting of sphalerite (0.3%-1%), galena (0.3%-1%), pyrite (0.3%-1.5%) and pyrrhotite (0.2%-0.6%). Further downhole at 232.95 metres depth (225 metres vertical) below this new discovery, the Contact Zone was intercepted over 329.75 metres and consisted of mineralized angular breccia with abundant chalcopyrite (up to 2.5%), pyrite (1%-7%) and 1% pyrrhotite as well as CBM vein system sulphides such as sphalerite (0.2% to 3%) and galena (0.1% to 3%). An extremely high-grade subzone of 56.60 metres was encountered at 277.65 metres downhole with an abundance of CBM vein sulphides flooding the matrix. Assay results for APC-53 are as follows: 145.0 metres @ 2.11 g/t gold equivalent commencing from surface in the newly discovered vein system, and 329.75 metres @ 3.10 g/t gold equivalent from 233 metres downhole (consisting of 2.30 g/t gold, 42 g/t silver and 0.16% copper) in the Contact Zone including; 56.60 metres @ 10.05 g/t gold equivalent.

Faiz karşılama oranı	n/a
Nakit	US$113.33m
Eşitlik	US$134.35m
Toplam yükümlülükler	US$52.58m
Toplam varlıklar	US$186.92m

Veri	Son Güncelleme (UTC saati)
Şirket Analizi	2026/05/27 03:33
Gün Sonu Hisse Fiyatı	2026/05/27 00:00
Kazançlar	2026/03/31
Yıllık Kazançlar	2025/12/31

Paket	Veri	Zaman Çerçevesi	Örnek ABD Kaynağı ^*
Şirket Finansalları	10 yıl	Gelir tablosu Nakit akış tablosu Bilanço	SEC Form 10-K SEC Form 10-Q
Analist Konsensüs Tahminleri	+3 yıl	Finansal tahminler Analist fiyat hedefleri	Analist Araştırma Raporları Blue Matrix
Piyasa Fiyatları	30 yıl	Hisse senedi fiyatları Temettüler, Bölünmeler ve Eylemler	ICE Piyasa Verileri SEC Form S-1
Sahiplik	10 yıl	En büyük hissedarlar İçeriden öğrenenlerin ticareti	SEC Form 4 SEC Form 13D
Yönetim	10 yıl	Liderlik ekibi Yönetim Kurulu	SEC Form 10-K SEC Form DEF 14A
Önemli Gelişmeler	10 yıl	Şirket duyuruları	SEC Form 8-K

Analist	Kurum
Matthew Murphy	BMO Capital Markets Equity Research
Brian Quast	BMO Capital Markets Equity Research
Andrew Mikitchook	BMO Capital Markets Equity Research

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