{"id":2062,"date":"2020-02-11T17:52:27","date_gmt":"2020-02-11T22:52:27","guid":{"rendered":"https:\/\/www.diosexplo.com\/?p=2062"},"modified":"2020-02-17T01:34:52","modified_gmt":"2020-02-17T06:34:52","slug":"2062","status":"publish","type":"post","link":"https:\/\/www.diosexplo.com\/fr\/2020\/02\/11\/2062\/","title":{"rendered":"DIOS fore les anomalies de sols de WTS et frappe des valeurs en or tr\u00e8s int\u00e9ressantes dans ce secteur vierge du projet AU33, atteignant 18 g\/t en or sur 1 m"},"content":{"rendered":"

Le 6 f\u00e9vrier 2020
\nDIOS fore les anomalies de sols de WTS et frappe des valeurs en or tr\u00e8s int\u00e9ressantes dans ce secteur vierge du projet AU33, atteignant 18 g\/t en or sur 1 m<\/h4>\n

Montr\u00e9al (Qu\u00e9bec) \u2013DIOS EXPLORATION<\/strong> publie les r\u00e9sultats significatifs des forages de la cible WTS<\/strong> sur sa propri\u00e9t\u00e9 AU33<\/strong>, atteigant 18 g\/t Au sur 1 m (6.08 g\/t Au \/ 3 m) et 4.41 g\/t en or sur 1 m dans un autre sondage \u00e0 100 m de distance. DIOS<\/strong> a fore dix sondages exploratoires de 100-150 m de longueur, souvent distants de 200 m, en amont glaciaire de valeurs \u00e9lev\u00e9es en or dans le till glaciaire: voir tableau et carte.<\/p>\n

\"\"<\/a>\"\"<\/a>\"\"<\/a>\"\"<\/a><\/p>\n

L\u2019horizon magn\u00e9tique WTS<\/strong> affleure peu mais des sols analys\u00e9s en 2018-2019 ont men\u00e9 \u00e0 la d\u00e9couverte d\u2019essaims anomaux en or (8 \u00e0 269 ppb Au) pr\u00e8s de 2 structures d\u00e9magn\u00e9tis\u00e9es recoupant l\u2019horizon magn\u00e9tique WTS<\/strong> de 300-350 m de large. Aucun affleurement aurif\u00e8re n\u2019y a \u00e9t\u00e9 d\u00e9couvert, \u00e0 8 km au NE des zones aurif\u00e8res d\u2019HEBERTO.<\/p>\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n
No.\u00a0: 2019<\/em><\/p>\n

WTS <\/em><\/strong><\/th>\n

de<\/th>\n\u00e0<\/th>\nlargeur (m)<\/em><\/th>\ng\/t Au<\/em><\/th>\ndescription<\/em><\/th>\n<\/tr>\n<\/thead>\n
43A<\/strong><\/td>\n140<\/strong><\/td>\n141<\/strong><\/td>\n1m<\/strong><\/td>\n18.0<\/strong><\/td>\nQuartz-carbonates-chalcopyrite-pyrite en veinules dans<\/strong><\/p>\n

Basalte foli\u00e9 magn\u00e9tique<\/strong><\/td>\n<\/tr>\n

<\/td>\n139<\/td>\n142:<\/td>\n3m<\/td>\n6.08<\/td>\n<\/td>\n<\/tr>\n
43<\/strong><\/td>\n17<\/strong><\/td>\n18<\/strong><\/td>\n1m<\/strong><\/td>\n4.41<\/strong><\/td>\nBasalte foli\u00e9 magn\u00e9tique<\/strong>, traces pyrite<\/td>\n<\/tr>\n
<\/td>\n16<\/td>\n25<\/td>\n9m<\/td>\n0.547<\/td>\nBasalte foli\u00e9 magn\u00e9tique<\/strong> & granodiorite, traces-1% pyrite<\/td>\n<\/tr>\n
43<\/td>\n90<\/td>\n92<\/td>\n2m<\/td>\n0.503<\/td>\nQuartz carbonates en veinules dans basalte foli\u00e9 magn\u00e9tique<\/strong><\/td>\n<\/tr>\n
49<\/strong><\/td>\n31<\/strong><\/td>\n32<\/strong><\/td>\n1m<\/strong><\/td>\n1.51<\/strong><\/td>\nMagn\u00e9tique granodiorite<\/strong><\/p>\n

0.5% pyrite<\/strong><\/td>\n<\/tr>\n

49<\/strong><\/td>\n115<\/strong><\/td>\n116<\/strong><\/td>\n1m<\/strong><\/td>\n2.48<\/strong><\/td>\nMagn\u00e9tique Granodiorite: dyke 1% pyrite<\/strong><\/td>\n<\/tr>\n
45<\/strong><\/td>\n37<\/strong><\/td>\n38<\/strong><\/td>\n1m<\/strong><\/td>\n1.68<\/strong><\/td>\nBasalte foli\u00e9 <\/strong>\u00a0<\/strong><\/p>\n

1-2% pyrite <\/strong><\/td>\n<\/tr>\n

45<\/strong><\/td>\n46<\/strong><\/td>\n47<\/strong><\/td>\n1m<\/strong><\/td>\n0.891<\/strong><\/td>\nBasalte foli\u00e9 <\/strong>1%pyrite<\/strong><\/td>\n<\/tr>\n
45<\/strong><\/td>\n87<\/strong><\/td>\n88<\/strong><\/td>\n1m<\/strong><\/td>\n1.0<\/strong><\/td>\nBasalte foli\u00e9 <\/strong>1% pyrite <\/strong><\/td>\n<\/tr>\n
51<\/td>\n7<\/td>\n8<\/td>\n1m<\/td>\n0.628<\/td>\nQz-cb-cpy-py.en veinules dans granodiorite<\/td>\n<\/tr>\n
50<\/td>\n54<\/td>\n56<\/td>\n2m<\/td>\n0.17<\/td>\nBasalte foli\u00e9: <\/strong>dyke,<\/p>\n

5% qz-cb en veinules<\/td>\n<\/tr>\n

50<\/td>\n64.5<\/td>\n66.5<\/td>\n2m<\/td>\n0.2<\/td>\nMagn\u00e9tique Granodiorite\u00a0: dyke, 1%py<\/td>\n<\/tr>\n
50<\/td>\n76.5<\/td>\n79.5<\/td>\n3m<\/td>\n0.274<\/td>\nMagn\u00e9tique Granodiorite\u00a0: dyke, 0.5%py<\/td>\n<\/tr>\n
50<\/p>\n

50<\/td>\n

88.5<\/p>\n

123.5<\/td>\n

90.5<\/p>\n

125.5<\/td>\n

2m<\/p>\n

2m<\/td>\n

0.44<\/p>\n

0.4<\/td>\n

Basalte foli\u00e9: <\/strong>dyke, 0.5%py +qz-cb en veinules<\/p>\n

Basalte foli\u00e9<\/strong>, 2%py<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

De nombreuses structures aurif\u00e8res \u00e9troites (1- m) donnant de 0.5 \u00e018 g\/t Au) associ\u00e9es \u00e0 des veinules centim\u00e9triques de quartz (pyrite-chalcopyrite) et\/ou \u00e0 de la pyrite diss\u00e9min\u00e9e (1-4%) ont \u00e9t\u00e9 rcoup\u00e9e par les forages de fin 2019 pr\u00e8s des anomalies en or dans les sols de WTS<\/strong>.<\/p>\n

ROBINO<\/strong> (in English)<\/em>
\nGold mineralization associated with Robino breccia is controlled by NNW to NS structures, including fractures, quartz stringers\/veinlets, and shear zones, recalling geological context of Heberto. Channel sampling across breccia indicates that clasts are barren and mineralization occurs in altered breccia matrix. Mineralized breccias are often associated with intense hydrothermal activity in cupolas and apophysis above porphyry intrusions. Source of gold could be located in root zone of Robino breccia or could have migrated in nearby structure. This also suggests possible occurrence of magmatic-hydrothermal breccias near Heberto showing 3.5 km to the south.<\/em><\/p>\n

Flat tension high-grade quartz-pyrite veins (up to 94 g\/t gold) associated with foliated eastern margin of NNW Robino breccia are reminiscent of flat quartz-pyrite-magnetite veins associated with NNW shears observed at Heberto. They were observed on a surface of 2-3m x 20m along a N-S foliated basic dyke, but not in hole 39, though two one-meter long channel samples had returned 5 g\/t Au \/ 1 m each.<\/em><\/p>\n

Hole 40 tested a NE chargeable induced polarization anomaly adjacent to Robino breccia. It intercepted fractured tonalite with 1-2%pyrite between 53-85m and sericitic magmatic-hydrothermal Robino breccia with 2-3% disseminated pyrite between 85-155 m (0.01g\/t Au) . Robino breccia is locally injected by minor metric feldspar-phyric diorite dykes with 2-4% pyrite. An adjacent sericitic foliated\/fractured zone with 1%pyrite assayed 2.26 g\/t Au over 1 m (0.404 g\/t gold over 6 m).<\/strong><\/em><\/p>\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n
Holes 2019 <\/em><\/p>\n

WTS area <\/em><\/span><\/th>\n

From<\/th>\nTo<\/th>\nLength (m)<\/em><\/th>\ng\/t gold<\/em><\/th>\nComment<\/em><\/th>\n<\/tr>\n<\/thead>\n
39<\/td>\n3<\/td>\n6<\/td>\n3m<\/td>\n0.085<\/td>\nTonalite breccia, lightly sericitized, 2-3% pyrite<\/td>\n<\/tr>\n
40<\/td>\n85<\/td>\n136<\/td>\n51<\/td>\n0.01<\/td>\nTonalite breccia, strongly sericitized<\/td>\n<\/tr>\n
40<\/td>\n155<\/td>\n159.5<\/td>\n4.5<\/td>\n0.5206<\/td>\nFoliate tonalite, very strongly sericitized 1% pyrite<\/td>\n<\/tr>\n
40<\/strong><\/td>\n158.5<\/strong><\/td>\n159.5<\/strong><\/td>\n1m<\/strong><\/td>\n2.26<\/strong><\/td>\n\u00a0Pyrite-rich stringers in foliated tonalite, very strongly sericitized<\/strong><\/td>\n<\/tr>\n
40A<\/td>\n160<\/td>\n269<\/td>\n109m<\/td>\n0.015<\/td>\nTonalite breccia, strongly sericitized, 2-3% pyrite<\/td>\n<\/tr>\n
40A<\/td>\n287<\/td>\n294.5<\/td>\n7.5m<\/td>\n0.077<\/td>\nTonalite strongly sericitized & albitized 1-2% pyrite<\/td>\n<\/tr>\n
42<\/td>\n306<\/td>\n310<\/td>\n4m<\/td>\n0.061<\/td>\nTonalite breccia lightly sericitized 1% py<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n
<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

Hole 40A tested SW extension of Robino breccia<\/strong>. It intersected fractured tonalite with 1-2% pyrite between 85-160m and sericitic magmatic-hydrothermal Robino breccia with 1-2% disseminated pyrite between 160-269 m (0.015g\/t Au). Robino breccia is injected by numerous metric feldspar-phyric diorite dykes with 2-4% pyrite<\/strong>. These are known as favorable gold metallotect in the region. An adjacent sericitic-albite fractured zone with 1-2% pyrite yielded 0.077g\/t Au\/7.5m (287-294.5m). This hole confirms N230 strike, dip 25-35 degree to the SW of the Robino breccia.<\/strong><\/em><\/p>\n

Hole 42 tried to test the N290\/30 Robino breccia and adjacent circular low magnetic & resistive anomaly<\/strong>. It intersected poorly fractured tonalite with pyrite traces between 160-303m and sericitic magmatic-hydrothermal Robino breccia with 1% disseminated pyrite between 303-310m (0.061g\/t Au) at the bottom. This hole was stopped due to bad ground conditions. Robino breccia is usually injected by metric feldspar-phyric diorite dykes with 2-4% pyrite, so this hole did not reach it.<\/em><\/p>\n

Similarities of Robino geochemistry with Heberto diorite suggest they may both represent apophysis of deep gold-bearing intrusions injected along favorable NNW structures. Both Robino & Heberto magmatic phases are distinctive of Mistumis pluton.<\/em><\/p>\n

Favorable area where NE-SW Robino breccia cuts NNW Heberto shears should be checked (systematically resampled for magnetite or pyrite-rich quartz vein\/veinlet) at surface.<\/em><\/p>\n

Road accessible wholly-owned (no royalties) AU33 gold property covers a prospective 20 km strike of Lower Eastmain greenstone belt, a few km west of Eastmain-1 hydropower facilities, James Bay Eeyou Istchee. It is underlain by large Mistumis intrusion which DIOS proved to be gold-bearing through a large series of gold showing and prospect discoveries, often in association with smaller intrusions.<\/em><\/p>\n

Core was logged under supervision of Harold Desbiens Geo M.Sc., Qualified Person, and split in two for sampling following standard industry procedures including quality controls and duplicates and assayed for gold at ALS Global laboratory in Val d\u2019Or by fire assay with atomic absorption or gravimetric finish.<\/em><\/p>\n

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.<\/em><\/h5>\n

Marie-Jos\u00e9 Girard Geo M.Sc. 43-101 QP<\/strong>
\nPresident & CEO<\/strong>
\nmjgirard@diosexplo.com<\/strong>
\nTel.: (514) 923-9123<\/strong>
\nwww.diosexplo.com<\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"

Le 6 f\u00e9vrier 2020 DIOS fore les anomalies de sols de WTS et frappe des valeurs en or tr\u00e8s int\u00e9ressantes dans ce secteur vierge du projet AU33, atteignant 18 g\/t en or sur 1 m Montr\u00e9al (Qu\u00e9bec) \u2013DIOS EXPLORATION publie les r\u00e9sultats significatifs des forages de la cible WTS sur sa propri\u00e9t\u00e9 AU33, atteigant 18 […]<\/p>\n","protected":false},"author":10,"featured_media":2184,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-2062","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-non-classifiee"],"yoast_head":"\nNouveaux r\u00e9sultats int\u00e9ressants sur le projet AU33 - Dios Exploration<\/title>\n<meta name=\"description\" content=\"DIOS fore les anomalies de sols de WTS et frappe des valeurs en or tr\u00e8s int\u00e9ressantes dans ce secteur vierge du projet AU33, atteignant 18 g\/t en or sur 1 m.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.diosexplo.com\/fr\/2020\/02\/11\/2062\/\" \/>\n<meta property=\"og:locale\" content=\"fr_FR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Nouveaux r\u00e9sultats int\u00e9ressants sur le projet AU33 - 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