{"id":83813,"date":"2026-06-29T12:30:55","date_gmt":"2026-06-29T12:30:55","guid":{"rendered":"https:\/\/qimaterials.com\/?p=83813"},"modified":"2026-06-29T12:30:56","modified_gmt":"2026-06-29T12:30:56","slug":"qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or","status":"publish","type":"post","link":"https:\/\/qimaterials.com\/fr\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\/","title":{"rendered":"QIMC signale plusieurs niveaux \u00e9lev\u00e9s de gaz de boue d&#039;hydrog\u00e8ne sur un intervalle de 100 \u00e0 250 m du forage DDH-26-04, dont un pic de 16,01 TP3T, deux relev\u00e9s de 13,51 TP3T et neuf relev\u00e9s \u00e9gaux ou sup\u00e9rieurs \u00e0 51 TP3T."},"content":{"rendered":"<p class=\"wp-block-paragraph\"><strong><em>L&#039;analyseur EAGLE II \u00e0 plage de mesure sup\u00e9rieure enregistre des lectures r\u00e9p\u00e9t\u00e9es du pourcentage d&#039;hydrog\u00e8ne, 35 des 60 \u00e9chantillons IsoJar d\u00e9passant 1% H\u2082 tandis que le m\u00e9thane est rest\u00e9 proche de 0% et le dioxyde de carbone \u00e0 0,2% ou moins sur tout l&#039;intervalle<\/em><\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Montr\u00e9al (Qu\u00e9bec) \u2014 le 29 juin 2026 \u2014 <strong>Soci\u00e9t\u00e9 des mat\u00e9riaux innovants du Qu\u00e9bec.<\/strong> (CSE : QIMC) (OTCQB : QIMCF) (FSE : 7FJ) (\u201c QIMC \u201d ou la \u201c Soci\u00e9t\u00e9 \u201d) est heureuse d\u2019annoncer de nouveaux r\u00e9sultats g\u00e9ochimiques pr\u00e9liminaires sur les gaz de boue provenant de l\u2019intervalle de 100 \u00e0 250 m\u00e8tres du forage au diamant DDH-26-04 \u00e0 Bennett Hill, en Nouvelle-\u00c9cosse, y compris une lecture maximale d\u2019hydrog\u00e8ne de 16,0% H\u2082 \u00e0 236 m\u00e8tres, deux lectures de 13,5% H\u2082, neuf lectures \u00e9gales ou sup\u00e9rieures \u00e0 5% H\u2082 et 35 des 60 \u00e9chantillons IsoJar donnant des lectures \u00e9gales ou sup\u00e9rieures \u00e0 1% H\u2082.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">La Soci\u00e9t\u00e9 consid\u00e8re que les relev\u00e9s r\u00e9p\u00e9t\u00e9s de concentrations \u00e9lev\u00e9es d&#039;hydrog\u00e8ne entre 100 et 250 m\u00e8tres sont significatifs, car ils indiquent une augmentation g\u00e9n\u00e9ralis\u00e9e de la concentration de gaz de forage plut\u00f4t qu&#039;un relev\u00e9 isol\u00e9. Ces r\u00e9sultats ont \u00e9t\u00e9 obtenus \u00e0 l&#039;aide d&#039;un analyseur EAGLE II \u00e0 plus grande capacit\u00e9, d\u00e9ploy\u00e9 apr\u00e8s la saturation du premier analyseur dans les 100 premiers m\u00e8tres, comme indiqu\u00e9 dans le communiqu\u00e9 de presse de la Soci\u00e9t\u00e9 du 18 juin 2026.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Points saillants \u2014 DDH-26-04 (Intervalle 100 m\u2013250 m)<\/strong>.<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li><strong>Mesures de pic et mesures r\u00e9p\u00e9t\u00e9es de l&#039;hydrog\u00e8ne \u00e0 haute valeur.<\/strong> La soci\u00e9t\u00e9 a enregistr\u00e9 une lecture maximale de 16,0% H\u2082 \u00e0 236 m\u00e8tres, ainsi que deux lectures de 13,5% H\u2082 \u00e0 125 m\u00e8tres et 152 m\u00e8tres, et neuf lectures \u00e9gales ou sup\u00e9rieures \u00e0 5% H\u2082 sur l&#039;intervalle signal\u00e9.<\/li>\n\n\n\n<li><strong>R\u00e9ponse \u00e0 l&#039;hydrog\u00e8ne globalement \u00e9lev\u00e9e.<\/strong> <strong>Parmi les 60 \u00e9chantillons de boues et de gaz IsoJar collect\u00e9s simultan\u00e9ment<\/strong> Sur l&#039;intervalle de 100 \u00e0 250 m, 35 \u00e9chantillons ont donn\u00e9 des valeurs \u00e9gales ou sup\u00e9rieures \u00e0 la valeur mesur\u00e9e. <strong>1% H\u2082<\/strong>, ce que la soci\u00e9t\u00e9 interpr\u00e8te comme indiquant des lectures d&#039;hydrog\u00e8ne \u00e9lev\u00e9es et r\u00e9p\u00e9t\u00e9es sur l&#039;intervalle \u00e9chantillonn\u00e9 plut\u00f4t qu&#039;une seule lecture isol\u00e9e.<\/li>\n\n\n\n<li><strong>Mod\u00e8le d&#039;exploration \u00e0 l&#039;\u00e9chelle du district.<\/strong> La r\u00e9ponse \u00e9lev\u00e9e en hydrog\u00e8ne \u00e0 Bennett Hill, situ\u00e9 \u00e0 environ 15 kilom\u00e8tres des forages DDH-26-01 et DDH-26-02 de Eatonville Road, fournit des donn\u00e9es suppl\u00e9mentaires soutenant le mod\u00e8le g\u00e9ologique \u00e9volutif de QIMC d&#039;un syst\u00e8me d&#039;hydrog\u00e8ne naturel potentiellement \u00e9tendu dans la r\u00e9gion d&#039;Advocate.<\/li>\n\n\n\n<li><strong>\u00c9v\u00e9nement superficiel.<\/strong> Les relev\u00e9s de niveau de pourcentage se produisent dans les 250 premiers m\u00e8tres du forage DDH-26-04, \u00e0 une profondeur inf\u00e9rieure \u00e0 celle des intervalles de niveau de pourcentage plus profonds pr\u00e9c\u00e9demment signal\u00e9s dans les forages d&#039;Eatonville Road (West-Advocate), y compris le relev\u00e9 de 10,77% H\u2082 signal\u00e9 pr\u00e8s de 848 m dans le forage DDH-26-03, tel que divulgu\u00e9 le 20 mai 2026. Les comparaisons de profondeur refl\u00e8tent les mesures effectu\u00e9es dans chaque forage et ne sont pas des valeurs calibr\u00e9es \u00e9quivalentes.<\/li>\n\n\n\n<li><strong>Analyseur de gamme sup\u00e9rieure d\u00e9ploy\u00e9.<\/strong> Les lectures ont \u00e9t\u00e9 obtenues \u00e0 l&#039;aide d&#039;un analyseur EAGLE II \u00e0 plus grande port\u00e9e d\u00e9ploy\u00e9 apr\u00e8s que le premier analyseur ait atteint sa limite sup\u00e9rieure de mesure de 4,03% H\u2082 dans les 100 premiers m\u00e8tres, comme indiqu\u00e9 le 18 juin 2026.<\/li>\n\n\n\n<li><strong>Signature gazeuse \u00e0 faible teneur en m\u00e9thane et en dioxyde de carbone.<\/strong> Du m\u00e9thane (CH\u2084) a \u00e9t\u00e9 enregistr\u00e9 \u00e0 environ 0% et du dioxyde de carbone (CO\u2082) \u00e0 ou en dessous de 0,2% sur l&#039;intervalle, ce que la Soci\u00e9t\u00e9 interpr\u00e8te pr\u00e9liminairement comme potentiellement coh\u00e9rent avec une signature de gaz hydrog\u00e8ne naturel.<\/li>\n\n\n\n<li><strong>Association structurale.<\/strong> Les relev\u00e9s les plus importants co\u00efncident avec les zones fractur\u00e9es et br\u00e9chifi\u00e9es enregistr\u00e9es dans les lithologies felsiques d\u00e9form\u00e9es et affect\u00e9es par des failles du forage, y compris un intervalle de br\u00e8che de faille enregistr\u00e9 entre environ 132 m et 149 m, que la Soci\u00e9t\u00e9 interpr\u00e8te comme \u00e9tant coh\u00e9rent avec son hypoth\u00e8se de travail selon laquelle les structures locales peuvent influencer la migration du gaz.<\/li>\n\n\n\n<li><strong>Mod\u00e8le d&#039;exploration r\u00e9gionale.<\/strong> Bennett Hill se situe \u00e0 environ 15 kilom\u00e8tres de la zone de forage d&#039;Eatonville. La soci\u00e9t\u00e9 consid\u00e8re la faible profondeur d&#039;\u00e9l\u00e9vation observ\u00e9e \u00e0 Bennett Hill comme une donn\u00e9e suppl\u00e9mentaire appuyant son mod\u00e8le d&#039;exploration r\u00e9gionale dans la zone d&#039;Advocate.<\/li>\n\n\n\n<li><strong>Forage et validation en cours.<\/strong> L\u2019\u00e9chantillonnage \u00e0 plus de 250 m\u00e8tres de profondeur est en cours et d\u2019autres r\u00e9sultats seront communiqu\u00e9s d\u00e8s qu\u2019ils seront disponibles et valid\u00e9s.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Construction sur les 100 m\u00e8tres sup\u00e9rieurs<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Comme indiqu\u00e9 le 18 juin 2026, les 100 premiers m\u00e8tres du puits DDH-26-04 pr\u00e9sentaient des concentrations d&#039;hydrog\u00e8ne \u00e9lev\u00e9es, notamment une zone de 9 m\u00e8tres avec quatre relev\u00e9s \u00e9gaux ou sup\u00e9rieurs \u00e0 4,03% H\u2082 \u2014 la limite sup\u00e9rieure de mesure (point de saturation) du premier analyseur EAGLE II utilis\u00e9 sur cet intervalle. Cet instrument \u00e9tant satur\u00e9, la soci\u00e9t\u00e9 a d\u00e9ploy\u00e9 un second analyseur EAGLE II dot\u00e9 d&#039;une plage de mesure plus \u00e9tendue afin de quantifier l&#039;hydrog\u00e8ne pr\u00e9sent \u00e0 plus de 100 m\u00e8tres de profondeur.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les r\u00e9sultats pr\u00e9sent\u00e9s aujourd&#039;hui sont issus de cet \u00e9chantillonnage \u00e0 plus grande \u00e9chelle. Soixante \u00e9chantillons d&#039;espace de t\u00eate IsoJar ont \u00e9t\u00e9 pr\u00e9lev\u00e9s simultan\u00e9ment \u00e0 intervalles d&#039;environ 3 m\u00e8tres sur l&#039;intervalle de 100 \u00e0 250 m\u00e8tres.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Contexte g\u00e9ologique et interpr\u00e9tation<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">La soci\u00e9t\u00e9 interpr\u00e8te les taux \u00e9lev\u00e9s d&#039;hydrog\u00e8ne relev\u00e9s \u00e0 plusieurs reprises \u00e0 des profondeurs relativement faibles comme pouvant indiquer des zones de perm\u00e9abilit\u00e9 accrue susceptibles de permettre la migration de gaz, sous r\u00e9serve d&#039;\u00e9talonnages en laboratoire, de v\u00e9rifications ind\u00e9pendantes et d&#039;une interpr\u00e9tation g\u00e9ologique plus pouss\u00e9e. Les taux n\u00e9gligeables de m\u00e9thane et les tr\u00e8s faibles taux de dioxyde de carbone relev\u00e9s simultan\u00e9ment ne sont pas, \u00e0 titre pr\u00e9liminaire, fortement \u00e9vocateurs d&#039;une signature de gaz d&#039;hydrocarbures conventionnelle.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les relev\u00e9s les plus importants sont spatialement associ\u00e9s \u00e0 des roches d\u00e9form\u00e9es et fractur\u00e9es identifi\u00e9es dans le forage, notamment une s\u00e9quence felsique d\u00e9form\u00e9e s&#039;\u00e9tendant d&#039;environ 43 m \u00e0 162 m et un intervalle de br\u00e8che de faille identifi\u00e9 entre environ 132 m et 149 m. La Soci\u00e9t\u00e9 consid\u00e8re cette association comme pertinente pour son hypoth\u00e8se de travail selon laquelle les structures locales peuvent influencer la migration du gaz.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Ces r\u00e9sultats sont en cours d&#039;int\u00e9gration dans le syst\u00e8me propri\u00e9taire de QIMC. <strong>R2G2\u2122 (G\u00e9ostructure de rift et de graben r\u00e9activ\u00e9e)<\/strong> cadre d&#039;exploration.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Commentaire de la direction<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>\u201c\u00a0Pour QIMC, la reproductibilit\u00e9 est essentielle\u00a0\u201d, a d\u00e9clar\u00e9 John Karagiannidis, pr\u00e9sident-directeur g\u00e9n\u00e9ral de QIMC. \u201c\u00a0Sur l\u2019intervalle de 100 \u00e0 250\u00a0m\u00e8tres du forage DDH-26-04, nous avons enregistr\u00e9 une concentration pr\u00e9liminaire maximale de gaz de forage de 16,01\u00a0TP3T H\u2082 \u00e0 236\u00a0m\u00e8tres, deux concentrations de 13,51\u00a0TP3T H\u2082, neuf concentrations \u00e9gales ou sup\u00e9rieures \u00e0 51\u00a0TP3T H\u2082 et 35 des 60\u00a0\u00e9chantillons IsoJar pr\u00e9sentant des concentrations \u00e9gales ou sup\u00e9rieures \u00e0 11\u00a0TP3T H\u2082. \u00c0 notre avis, il s\u2019agit d\u2019un r\u00e9sultat technique important car il d\u00e9montre des concentrations d\u2019hydrog\u00e8ne \u00e9lev\u00e9es et r\u00e9p\u00e9t\u00e9es sur l\u2019ensemble de l\u2019intervalle, et non une seule concentration isol\u00e9e.\u00a0\u201d<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>\u201c\u00a0Ce qui est \u00e9galement significatif, c\u2019est la combinaison de l\u2019ampleur du ph\u00e9nom\u00e8ne, de sa faible profondeur et d\u2019une signature gazeuse caract\u00e9ris\u00e9e par de faibles concentrations de m\u00e9thane et de dioxyde de carbone. Le m\u00e9thane a \u00e9t\u00e9 d\u00e9tect\u00e9 \u00e0 environ 0% et le dioxyde de carbone \u00e0 une concentration \u00e9gale ou inf\u00e9rieure \u00e0 0,2% sur l\u2019ensemble de l\u2019intervalle.\u00a0\u00bb.<\/em> <em>Ces r\u00e9sultats constituent une \u00e9tape importante vers l&#039;\u00e9valuation de l&#039;ampleur et de la continuit\u00e9 potentielles du syst\u00e8me d&#039;hydrog\u00e8ne naturel d&#039;Advocate. Il est \u00e0 noter que Bennett Hill se situe \u00e0 environ 15 kilom\u00e8tres des forages DDH-26-01 et DDH-26-02 de Eatonville Road, o\u00f9 QIMC avait pr\u00e9c\u00e9demment signal\u00e9 des concentrations \u00e9lev\u00e9es d&#039;hydrog\u00e8ne. La pr\u00e9sence de concentrations \u00e9lev\u00e9es d&#039;hydrog\u00e8ne aux deux endroits confirme notre mod\u00e8le de travail d&#039;un syst\u00e8me d&#039;hydrog\u00e8ne naturel potentiellement \u00e9tendu dans la r\u00e9gion d&#039;Advocate.\u201d<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>\u201c La nouvelle interpr\u00e9tation g\u00e9ologique fournit \u00e0 QIMC un cadre g\u00e9ologique et structural de plus en plus convaincant pour la poursuite de l&#039;exploration. Les concentrations d&#039;hydrog\u00e8ne les plus \u00e9lev\u00e9es se situent au sein ou \u00e0 proximit\u00e9 imm\u00e9diate de zones \u00e9paisses de br\u00e8ches de faille et d&#039;intervalles intens\u00e9ment fractur\u00e9s associ\u00e9s au pluton d&#039;Apple River, confortant notre hypoth\u00e8se de travail selon laquelle le syst\u00e8me de failles de Cobequid pourrait avoir constitu\u00e9 une voie de migration durable pour l&#039;hydrog\u00e8ne naturel. Cette corr\u00e9lation entre les concentrations \u00e9lev\u00e9es d&#039;hydrog\u00e8ne, le pluton d&#039;Apple River et les principaux corridors structuraux offre une base technique solide pour la poursuite des forages, la validation et l&#039;\u00e9valuation g\u00e9ologique \u00e0 Bennett Hill. \u201d<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Commentaire scientifique du professeur Marc Richer-LaFl\u00e8che<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>Les nouvelles donn\u00e9es du forage DDH-26-04 sont tr\u00e8s instructives, car elles r\u00e9v\u00e8lent un net enrichissement en H\u2082, de l&#039;ordre de 400%, vers le nord, dans un contexte structural de plus en plus profond. Les concentrations d&#039;hydrog\u00e8ne les plus \u00e9lev\u00e9es dans la boue de forage se trouvent au sein, ou imm\u00e9diatement \u00e0 proximit\u00e9, de zones de br\u00e8ches de faille relativement \u00e9paisses associ\u00e9es \u00e0 une fracturation intense (RQD%) de l&#039;intrusion d&#039;Apple River (Fig. 1). Cette intrusion se situe entre les failles de Cobequid Sud et Nord, qui forment ensemble un corridor de cisaillement composite de 6,2 km de large dans la r\u00e9gion de Bennett Hill.<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>La g\u00e9ologie observ\u00e9e dans le forage met en \u00e9vidence l&#039;influence dominante de la zone de faille nord, qui dans cette r\u00e9gion est typiquement caract\u00e9ris\u00e9e par une plus grande abondance de br\u00e8ches et de gouge de faille, contrairement \u00e0 la zone sud, o\u00f9 la d\u00e9formation s&#039;exprime plus fortement par la mylonitisation et le cisaillement ductile.<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>\u00c9tant donn\u00e9 l&#039;\u00e2ge carbonif\u00e8re de la mise en place du pluton, la forte d\u00e9formation observ\u00e9e dans le granito\u00efde potassique est n\u00e9cessairement li\u00e9e aux importants mouvements de d\u00e9crochement associ\u00e9s au syst\u00e8me de failles de Cobequid. Cette g\u00e9ostructure semble avoir exerc\u00e9 une influence profonde sur les roches des hauts plateaux de Cobequid.<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>Le nombre et la diversit\u00e9 des zones de roches cataclastiques, des zones de failles et des gouges de failles sont remarquables, d\u00e9montrant que le syst\u00e8me de failles de Cobequid a fonctionn\u00e9 comme un corridor de d\u00e9formation tr\u00e8s dynamique sur une longue p\u00e9riode g\u00e9ologique.<\/em><\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img fetchpriority=\"high\" decoding=\"async\" width=\"749\" height=\"457\" src=\"https:\/\/qimaterials.com\/wp-content\/uploads\/2026\/06\/image.png\" alt=\"\" class=\"wp-image-83814\" srcset=\"https:\/\/qimaterials.com\/wp-content\/uploads\/2026\/06\/image.png 749w, https:\/\/qimaterials.com\/wp-content\/uploads\/2026\/06\/image-300x183.png 300w, https:\/\/qimaterials.com\/wp-content\/uploads\/2026\/06\/image-18x12.png 18w\" sizes=\"(max-width: 749px) 100vw, 749px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><em>Figure 1. Diagrammes r\u00e9capitulant la g\u00e9ologie observ\u00e9e dans le forage DDH-26-04 entre 0 m et 250 m de profondeur (mesur\u00e9e le long du forage).<sub>2<\/sub> Les concentrations (ppmV) issues de l&#039;analyse des boues de forage (technique Isojar) soulignent l&#039;importance de l&#039;H<sub>2 <\/sub>concentrations observ\u00e9es ainsi que la relation spatiale avec les zones de br\u00e8che tectonique et la fracturation du noyau (RQD%).<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>\u00c0 propos de la Soci\u00e9t\u00e9 des mat\u00e9riaux innovants du Qu\u00e9bec (SMIQ)<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Soci\u00e9t\u00e9 des mat\u00e9riaux innovants du Qu\u00e9bec.<\/strong> (CSE\u00a0: QIMC) (OTCQB\u00a0: QIMCF) (FSE\u00a0: 7FJ) est une soci\u00e9t\u00e9 nord-am\u00e9ricaine d\u2019exploration et de d\u00e9veloppement qui fait progresser un portefeuille de projets d\u2019hydrog\u00e8ne naturel et de min\u00e9raux critiques. La soci\u00e9t\u00e9 d\u00e9ploie son mod\u00e8le d\u2019exploration au Qu\u00e9bec, en Ontario, en Nouvelle-\u00c9cosse et au Minnesota gr\u00e2ce \u00e0 l\u2019application de son cadre exclusif R2G2\u2122.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">QIMC privil\u00e9gie l&#039;exploration responsable, l&#039;innovation technique et le d\u00e9veloppement des ressources en hydrog\u00e8ne naturel susceptibles de contribuer aux futures initiatives de d\u00e9veloppement des \u00e9nergies propres. Les activit\u00e9s d&#039;exploration de la soci\u00e9t\u00e9 dans la zone d&#039;Advocate n&#039;impliquent ni fracturation hydraulique ni stimulation du r\u00e9servoir.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Pour plus d&#039;informations<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>QU\u00c9BEC MAT\u00c9RIAUX INNOVANTS CORP.<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">&nbsp;John Karagiannidis Pr\u00e9sident et chef de la direction<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">E-mail: <a href=\"mailto:info@qimaterials.com\">info@qimaterials.com<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">T\u00e9l. : +1 514-726-7058<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>\u00c9chantillonnage, m\u00e9thodologie et v\u00e9rification des donn\u00e9es<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les mesures de gaz de forage pr\u00e9sent\u00e9es dans ce communiqu\u00e9 sont pr\u00e9liminaires et bas\u00e9es sur des \u00e9chantillons d&#039;espace de t\u00eate pr\u00e9lev\u00e9s simultan\u00e9ment \u00e0 l&#039;aide d&#039;un IsoJar, \u00e0 intervalles d&#039;environ 3 m\u00e8tres, lors du forage du puits DDH-26-04. Les mesures sur l&#039;intervalle de 100 \u00e0 250 m\u00e8tres ont \u00e9t\u00e9 obtenues \u00e0 l&#039;aide d&#039;un analyseur de gaz portable EAGLE II, dot\u00e9 d&#039;une plage de mesure sup\u00e9rieure \u00e0 celle de l&#039;appareil utilis\u00e9 dans les 100 premiers m\u00e8tres, ce dernier ayant atteint sa limite sup\u00e9rieure de mesure de 4,031 TP3T (point de saturation) pour le H\u2082. Le m\u00e9thane (CH\u2084) a \u00e9t\u00e9 mesur\u00e9 \u00e0 environ 0,1 TP3T et le dioxyde de carbone (CO\u2082) \u00e0 une concentration inf\u00e9rieure ou \u00e9gale \u00e0 0,21 TP3T sur l&#039;ensemble de l&#039;intervalle consid\u00e9r\u00e9, soit \u00e0 la limite de d\u00e9tection de l&#039;analyseur.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les mesures effectu\u00e9es sur l&#039;intervalle 100 m\u2013250 m ont \u00e9t\u00e9 r\u00e9alis\u00e9es dans la plage de mesure de l&#039;analyseur EAGLE II \u00e0 haute r\u00e9solution. Toutes les mesures restent soumises \u00e0 un \u00e9talonnage en laboratoire et \u00e0 une v\u00e9rification ind\u00e9pendante.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Toutes les valeurs rapport\u00e9es sont soumises \u00e0 une v\u00e9rification ind\u00e9pendante par rapport \u00e0 des \u00e9chantillons de bouteilles de gaz certifi\u00e9es analys\u00e9s par un instrument de r\u00e9f\u00e9rence de laboratoire de plus haute pr\u00e9cision, sous la supervision du Prof. Marc Richer-LaFl\u00e8che, P.Geo., de l&#039;INRS.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Mise en garde concernant les relev\u00e9s de gaz de boue<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les investisseurs sont avertis que les mesures de gaz de boue et de gaz d&#039;espace de t\u00eate ne sont que des indicateurs g\u00e9ochimiques pr\u00e9liminaires, propres \u00e0 la phase d&#039;exploration. Il s&#039;agit de mesures pr\u00e9liminaires effectu\u00e9es en laboratoire \u00e0 partir d&#039;\u00e9chantillons d&#039;espace de t\u00eate pr\u00e9lev\u00e9s avec IsoJar. Elles ne constituent ni des ressources ni des r\u00e9serves min\u00e9rales, et ne sont pas indicatives de la pr\u00e9sence, du volume, de la concentration, du d\u00e9bit, de la capacit\u00e9 de livraison ou de la rentabilit\u00e9 commerciale d&#039;une quelconque accumulation d&#039;hydrog\u00e8ne naturel. Elles ne doivent donc pas \u00eatre consid\u00e9r\u00e9es comme telles. Rien ne garantit que des taux d&#039;hydrog\u00e8ne \u00e9lev\u00e9s seront v\u00e9rifi\u00e9s, calibr\u00e9s ou traduits en une ressource \u00e9conomiquement exploitable par un organisme ind\u00e9pendant. Les termes \u201c record \u201d, \u201c plus haut \u201d, \u201c plus fort \u201d ou autres expressions similaires refl\u00e8tent l&#039;analyse que la Soci\u00e9t\u00e9 fait de ses propres donn\u00e9es et ne constituent pas des affirmations de faits v\u00e9rifi\u00e9s de mani\u00e8re ind\u00e9pendante.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><em>Ni la Bourse canadienne des valeurs mobili\u00e8res ni son fournisseur de services de r\u00e9glementation (tel que ce terme est d\u00e9fini dans les politiques de la Bourse canadienne des valeurs mobili\u00e8res) n\u2019acceptent la responsabilit\u00e9 de l\u2019ad\u00e9quation ou de l\u2019exactitude du pr\u00e9sent communiqu\u00e9.<\/em><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>D\u00e9clarations prospectives<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Ce communiqu\u00e9 de presse contient des \u201c informations prospectives \u201d et des \u201c \u00e9nonc\u00e9s prospectifs \u201d au sens des lois canadiennes sur les valeurs mobili\u00e8res applicables. Les \u00e9nonc\u00e9s prospectifs comprennent, sans s\u2019y limiter, des \u00e9nonc\u00e9s concernant l\u2019interpr\u00e9tation et la signification des mesures d\u2019hydrog\u00e8ne au forage DDH-26-04 et dans d\u2019autres forages; l\u2019existence, l\u2019\u00e9tendue, la continuit\u00e9 ou la possibilit\u00e9 d\u2019expansion de tout corridor ou syst\u00e8me d\u2019hydrog\u00e8ne; la relation entre Bennett Hill et la zone de forage d\u2019Eatonville; les r\u00e9sultats attendus de l\u2019\u00e9chantillonnage continu et de l\u2019\u00e9talonnage en laboratoire; les activit\u00e9s d\u2019exploration, de forage et de d\u00e9veloppement planifi\u00e9es, en cours ou futures; et les occasions strat\u00e9giques potentielles, l\u2019\u00e9valuation technique, les partenariats de d\u00e9veloppement ou d\u2019autres occasions commerciales futures. Ces \u00e9nonc\u00e9s sont fond\u00e9s sur des hypoth\u00e8ses et sont assujettis \u00e0 des risques et incertitudes connus et inconnus \u2014 y compris le fait que les mesures pourraient ne pas \u00eatre confirm\u00e9es par une analyse en laboratoire, que les indicateurs g\u00e9ochimiques pourraient ne pas refl\u00e9ter une ressource r\u00e9cup\u00e9rable et les risques li\u00e9s au financement, \u00e0 l\u2019obtention des permis, aux conditions m\u00e9t\u00e9orologiques, aux march\u00e9s et \u00e0 la conjoncture \u00e9conomique g\u00e9n\u00e9rale \u2014 qui pourraient faire en sorte que les r\u00e9sultats r\u00e9els diff\u00e8rent sensiblement de ceux exprim\u00e9s ou sous-entendus. Les lecteurs sont pri\u00e9s de ne pas se fier ind\u00fbment aux \u00e9nonc\u00e9s prospectifs. Sauf en cas d&#039;obligation l\u00e9gale, la Soci\u00e9t\u00e9 d\u00e9cline toute obligation de mettre \u00e0 jour ou de r\u00e9viser les d\u00e9clarations prospectives.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Informations scientifiques et techniques<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Les informations scientifiques et techniques contenues dans ce communiqu\u00e9 de presse ont \u00e9t\u00e9 examin\u00e9es et approuv\u00e9es par le professeur Marc Richer-LaFl\u00e8che, P.Geo., de l\u2019Institut national de la recherche scientifique (INRS), consultant technique de la Soci\u00e9t\u00e9.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">L\u2019hydrog\u00e8ne naturel est une substance gazeuse et ne constitue ni une \u201c ressource min\u00e9rale \u201d ni une \u201c r\u00e9serve min\u00e9rale \u201d au sens du R\u00e8glement 43-101 \u2013 Normes de divulgation pour les projets miniers (\u201c R\u00e8glement 43-101 \u201d) et des Normes de d\u00e9finition de l\u2019ICM. Les teneurs en hydrog\u00e8ne pr\u00e9sent\u00e9es dans ce communiqu\u00e9 sont fournies \u00e0 titre de renseignements g\u00e9ochimiques relatifs \u00e0 l\u2019exploration et d\u2019information g\u00e9n\u00e9rale de l\u2019entreprise. Les d\u00e9finitions et classifications des ressources min\u00e9rales et des r\u00e9serves min\u00e9rales du R\u00e8glement 43-101 ne s\u2019appliquent pas aux teneurs en hydrog\u00e8ne rapport\u00e9es ici.<\/p>","protected":false},"excerpt":{"rendered":"<p>Higher-range EAGLE II analyzer records repeated percent-level hydrogen readings, with 35 of 60 IsoJar samples exceeding 1% H\u2082 while methane remained near 0% and carbon dioxide at or below 0.2% across the interval Montr\u00e9al, Qu\u00e9bec \u2014 June 29, 2026 \u2014 Qu\u00e9bec Innovative Materials Corp. (CSE: QIMC) (OTCQB: QIMCF) (FSE: 7FJ) (\u201cQIMC\u201d or the \u201cCompany\u201d) is [&hellip;]<\/p>\n","protected":false},"author":5,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_eb_attr":"","iawp_total_views":68,"footnotes":""},"categories":[10,11],"tags":[],"class_list":["post-83813","post","type-post","status-publish","format-standard","hentry","category-industry-news","category-press-releases"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.9 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>QIMC Reports Multiple Elevated Hydrogen Mud-Gas Readings Over 100m\u2013250m Interval of DDH-26-04, Including a Peak Hydrogen Reading of 16.0%, Two Hydrogen Readings of 13.5%, and Nine Readings at or Above 5% Hydrogen - QIMC<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/qimaterials.com\/fr\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\/\" \/>\n<meta property=\"og:locale\" content=\"fr_CA\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"QIMC Reports Multiple Elevated Hydrogen Mud-Gas Readings Over 100m\u2013250m Interval of DDH-26-04, Including a Peak Hydrogen Reading of 16.0%, Two Hydrogen Readings of 13.5%, and Nine Readings at or Above 5% Hydrogen - QIMC\" \/>\n<meta property=\"og:description\" content=\"Higher-range EAGLE II analyzer records repeated percent-level hydrogen readings, with 35 of 60 IsoJar samples exceeding 1% H\u2082 while methane remained near 0% and carbon dioxide at or below 0.2% across the interval Montr\u00e9al, Qu\u00e9bec \u2014 June 29, 2026 \u2014 Qu\u00e9bec Innovative Materials Corp. (CSE: QIMC) (OTCQB: QIMCF) (FSE: 7FJ) (\u201cQIMC\u201d or the \u201cCompany\u201d) is [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/qimaterials.com\/fr\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\/\" \/>\n<meta property=\"og:site_name\" content=\"QIMC\" \/>\n<meta property=\"article:published_time\" content=\"2026-06-29T12:30:55+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2026-06-29T12:30:56+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/qimaterials.com\/wp-content\/uploads\/2026\/06\/image.png\" \/>\n\t<meta property=\"og:image:width\" content=\"749\" \/>\n\t<meta property=\"og:image:height\" content=\"457\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/png\" \/>\n<meta name=\"author\" content=\"OPS OPS\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"\u00c9crit par\" \/>\n\t<meta name=\"twitter:data1\" content=\"OPS OPS\" \/>\n\t<meta name=\"twitter:label2\" content=\"Estimation du temps de lecture\" \/>\n\t<meta name=\"twitter:data2\" content=\"10 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\\\/\\\/qimaterials.com\\\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\\\/#article\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/qimaterials.com\\\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\\\/\"},\"author\":{\"name\":\"OPS OPS\",\"@id\":\"https:\\\/\\\/qimaterials.com\\\/#\\\/schema\\\/person\\\/4b0b8cdace5e0ece1df885772763f8f1\"},\"headline\":\"QIMC Reports Multiple Elevated Hydrogen Mud-Gas Readings Over 100m\u2013250m Interval of DDH-26-04, Including a Peak Hydrogen Reading of 16.0%, Two Hydrogen Readings of 13.5%, and Nine Readings at or Above 5% Hydrogen\",\"datePublished\":\"2026-06-29T12:30:55+00:00\",\"dateModified\":\"2026-06-29T12:30:56+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\\\/\\\/qimaterials.com\\\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\\\/\"},\"wordCount\":2052,\"image\":{\"@id\":\"https:\\\/\\\/qimaterials.com\\\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\\\/#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/qimaterials.com\\\/wp-content\\\/uploads\\\/2026\\\/06\\\/image.png\",\"articleSection\":[\"Industry News\",\"Press Releases\"],\"inLanguage\":\"fr-CA\"},{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/qimaterials.com\\\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\\\/\",\"url\":\"https:\\\/\\\/qimaterials.com\\\/qimc-reports-multiple-elevated-hydrogen-mud-gas-readings-over-100m-250m-interval-of-ddh-26-04-including-a-peak-hydrogen-reading-of-16-0-two-hydrogen-readings-of-13-5-and-nine-readings-at-or\\\/\",\"name\":\"QIMC Reports Multiple Elevated Hydrogen Mud-Gas Readings Over 100m\u2013250m Interval of DDH-26-04, Including a Peak Hydrogen Reading of 16.0%, Two Hydrogen Readings of 13.5%, and Nine Readings at or Above 5% Hydrogen - 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