{"id":83502,"date":"2026-05-06T11:26:42","date_gmt":"2026-05-06T11:26:42","guid":{"rendered":"https:\/\/qimaterials.com\/?st-import=3e2d0c6d4e73f4c31e54d3fa8e736725"},"modified":"2026-05-14T15:27:41","modified_gmt":"2026-05-14T15:27:41","slug":"qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date","status":"publish","type":"post","link":"https:\/\/qimaterials.com\/fr\/qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\/","title":{"rendered":"QIMC traverse une zone d&#039;hydrog\u00e8ne naturel de 243 m, dont un intervalle sur\u00e9lev\u00e9 continu de 163 m \u00e0 West Advocate (DDH-26-03) \u2013 R\u00e9ponse la plus forte \u00e0 ce jour"},"content":{"rendered":"<h5>\u2013<\/h5>\n<p><strong><em>Plusieurs mesures de H2 dans l&#039;espace de t\u00eate d\u00e9passent la plage de mesure de l&#039;instrument, avec des valeurs de v\u00e9rification crois\u00e9e atteignant 8\u00a0961 ppmV\u00a0; le syst\u00e8me reste ouvert \u00e0 une profondeur d&#039;environ 900 m.<\/em><\/strong><\/p>\n<p><b>Points cl\u00e9s \u2013 DDH-26-03 (intervalle de 300 \u00e0 543 m)<\/b><\/p>\n<ul>\n<li><b>163 m\u00e8tres de g\u00e9ochimie continue de l&#039;espace de t\u00eate d&#039;hydrog\u00e8ne naturel \u00e9lev\u00e9<\/b>\u00a0d&#039;environ 380 m \u00e0 543 m de profondeur de puits<\/li>\n<li><b>Zone anormale contenant de l&#039;hydrog\u00e8ne de 243 m\u00e8tres<\/b>\u00a0identifi\u00e9 entre 300 m et 543 m, repr\u00e9sentant l&#039;intervalle le plus \u00e9tendu rencontr\u00e9 \u00e0 ce jour<\/li>\n<li><b>Plusieurs mesures de H\u2082 dans l&#039;espace de t\u00eate ont d\u00e9pass\u00e9 la plage de mesure de 1\u00a0000 ppm de l&#039;instrument.<\/b>, avec des valeurs de contr\u00f4le crois\u00e9 secondaires s\u00e9lectionn\u00e9es jusqu&#039;\u00e0\u00a0<b>8\u00a0961 ppmV<\/b><\/li>\n<li><b>R\u00e9ponse \u00e0 l&#039;hydrog\u00e8ne la plus forte et la plus continue jamais observ\u00e9e \u00e0 ce jour<\/b>\u00a0dans le cadre du programme de forage West Advocate 2026 de QIMC<\/li>\n<li><b>Min\u00e9ralisation contenue dans un corridor de br\u00e8che de faille \u00e0 structure complexe.<\/b>, notamment les dykes intrusifs, la silicification et les r\u00e9seaux de fractures<\/li>\n<li><b>Le syst\u00e8me reste ouvert en profondeur<\/b>, les forages se poursuivant jusqu&#039;\u00e0 une profondeur totale pr\u00e9vue d&#039;environ 900 m<\/li>\n<\/ul>\n<p>Montr\u00e9al, Qu\u00e9bec \u2013 (Newsfile Corp. \u2013 6 mai 2026) \u2013\u00a0<b>Qu\u00e9bec Mat\u00e9riaux Innovatifs Corp. (CSE : QIMC) (OTCQB : QIMCF) (FSE : 7FJ) (\u201d QIMC \u201d ou la \u201d Soci\u00e9t\u00e9 \u201d)<\/b>\u00a0la soci\u00e9t\u00e9 a le plaisir d&#039;annoncer qu&#039;elle a rencontr\u00e9 un\u00a0<b>Intervalle anormal contenant de l&#039;hydrog\u00e8ne de 243 m\u00e8tres (300-543 m)<\/b>, y compris un\u00a0<b>zone d&#039;hydrog\u00e8ne continue en altitude de 163 m\u00e8tres (380-543 m)<\/b>, repr\u00e9sentant la r\u00e9ponse g\u00e9ochimique de terrain la plus forte et la plus continue observ\u00e9e \u00e0 ce jour dans le cadre de ce projet.<\/p>\n<p>L&#039;intervalle plus profond de DDH-26-03 est caract\u00e9ris\u00e9 par des lectures d&#039;hydrog\u00e8ne \u00e9lev\u00e9es et r\u00e9p\u00e9t\u00e9es, y compris de multiples mesures d\u00e9passant la limite de d\u00e9tection sup\u00e9rieure de l&#039;instrument de terrain principal GA5000, avec des valeurs de v\u00e9rification crois\u00e9e s\u00e9lectionn\u00e9es allant jusqu&#039;\u00e0\u00a0<b>8\u00a0961 ppmV<\/b>\u00a0Confirm\u00e9s \u00e0 l&#039;aide d&#039;un analyseur secondaire Eagle II, ces r\u00e9sultats \u00e9tendent l&#039;\u00e9tendue verticale et l&#039;intensit\u00e9 connues de la min\u00e9ralisation d&#039;hydrog\u00e8ne \u00e0 West Advocate et concordent avec l&#039;interpr\u00e9tation de la Soci\u00e9t\u00e9 d&#039;un syst\u00e8me \u00e0 contr\u00f4le structural qui demeure ouvert en profondeur, tandis que le forage se poursuit jusqu&#039;\u00e0 une profondeur totale pr\u00e9vue d&#039;environ\u00a0<b>900 m<\/b>. Parall\u00e8lement, les \u00e9chantillons de gaz de boue ISOJAR pr\u00e9lev\u00e9s \u00e0 intervalles de 3 m\u00e8tres dans le puits DDH-26-03 sont trait\u00e9s et interpr\u00e9t\u00e9s par le professeur Marc Richer-Lafl\u00e8che de l&#039;INRS, ajoutant ainsi une couche scientifique ind\u00e9pendante au programme int\u00e9gr\u00e9 de la soci\u00e9t\u00e9.<\/p>\n<p><b>Commentaire du PDG<\/b><\/p>\n<p>\u201d\u00a0DDH-26-03 a produit la r\u00e9ponse g\u00e9ochimique naturelle \u00e0 l\u2019hydrog\u00e8ne la plus forte et la plus continue observ\u00e9e \u00e0 ce jour \u00e0 West Advocate, faisant progresser de mani\u00e8re significative notre compr\u00e9hension du syst\u00e8me.\u00a0\u00bb.<\/p>\n<p>Le forage a recoup\u00e9 plus de 163 m\u00e8tres de g\u00e9ochimie de l&#039;espace de t\u00eate \u00e0 teneur \u00e9lev\u00e9e en hydrog\u00e8ne, au sein d&#039;un intervalle anomal plus large de 243 m\u00e8tres, avec des valeurs de contr\u00f4le crois\u00e9e atteignant jusqu&#039;\u00e0 8\u00a0961 ppmV. Ces r\u00e9sultats se situent dans une zone structuralement complexe caract\u00e9ris\u00e9e par une br\u00e9chification de failles, des dykes intrusifs, une silicification et des r\u00e9seaux de fractures, confortant notre interpr\u00e9tation d&#039;un vaste syst\u00e8me d&#039;hydrog\u00e8ne contr\u00f4l\u00e9 par la structure.<\/p>\n<p>Cet intervalle repr\u00e9sente une avanc\u00e9e significative par rapport aux forages pr\u00e9c\u00e9dents, avec une continuit\u00e9, une intensit\u00e9 et une coh\u00e9rence g\u00e9ologique accrues observ\u00e9es en profondeur. L&#039;\u00e9chantillonnage continu des gaz de forage ISOJAR et l&#039;analyse g\u00e9ologique int\u00e9gr\u00e9e avec l&#039;INRS contribuent \u00e0 affiner notre compr\u00e9hension du syst\u00e8me.<\/p>\n<p>Les r\u00e9sultats actuels confirment l&#039;existence d&#039;un syst\u00e8me d&#039;hydrog\u00e8ne qui reste ouvert en profondeur, et nous continuerons d&#039;\u00e9valuer sa continuit\u00e9 et son ampleur \u00e0 mesure que le forage progresse vers l&#039;objectif pr\u00e9vu de 900 m\u00e8tres.\u201d<\/p>\n<p>\u2013 John Karagiannidis, pr\u00e9sident et chef de la direction, Soci\u00e9t\u00e9 Mat\u00e9riaux Innovants Qu\u00e9bec.<\/p>\n<p><b>R\u00e9sultats \u2013 DDH-26-03<\/b><\/p>\n<p>La nouvelle zone identifi\u00e9e dans DDH-26-03 \u00e0 partir d&#039;environ\u00a0<b>300 m \u00e0 543 m de profondeur de puits<\/b>\u00a0est caract\u00e9ris\u00e9e par des r\u00e9ponses r\u00e9p\u00e9t\u00e9es \u00e0 l&#039;hydrog\u00e8ne dans l&#039;espace de t\u00eate \u00e0 champ \u00e9lev\u00e9, y compris plusieurs intervalles o\u00f9 l&#039;instrument GA5000 principal a d\u00e9pass\u00e9 sa plage de mesure H\u2082 sup\u00e9rieure.<\/p>\n<p><b>COMMENTAIRE SCIENTIFIQUE DU PROFESSEUR MARC RICHER-LAFLECHE<\/b><\/p>\n<p>Entre 300 et 540 m, les donn\u00e9es du forage DDH-26-03 montrent une nette augmentation de l&#039;intensit\u00e9 du fond d&#039;hydrog\u00e8ne approchant 1000 ppmV (<b>Fig. 1<\/b>Des valeurs sup\u00e9rieures \u00e0 3000 ppmV ont \u00e9t\u00e9 observ\u00e9es \u00e0 380 m (<b>3239 ppmV<\/b>), 476 m (<b>8961 ppmV<\/b>) et 521 m (<b>3537 ppmV<\/b>Cette tendance indique un potentiel d&#039;hydrog\u00e8ne naturel qui augmente avec la profondeur et se d\u00e9place vers le nord. Notamment, les concentrations m\u00e9dianes d&#039;hydrog\u00e8ne augmentent de\u00a0<b>357 ppmV (3-300 m)<\/b>\u00a0\u00e0\u00a0<b>820 ppmV (300-540 m)<\/b>, ce qui indique une augmentation statistiquement significative de l&#039;intensit\u00e9 de l&#039;hydrog\u00e8ne avec la profondeur.<\/p>\n<p><a href=\"\/fr\/\"https:><img class=\"\\\"releaseimage\\\"\" src=\"\\\"https:><\/a><\/p>\n<p><i><b>Figure 1<\/b>. Distribution comparative des concentrations d&#039;hydrog\u00e8ne (H\u2082 ppmV) dans des \u00e9chantillons d&#039;eau pr\u00e9lev\u00e9s dans le forage DDH-26-03 entre 3 m et 299 m et entre 300 m et 540 m (fraction d&#039;espace de t\u00eate). Les donn\u00e9es ont \u00e9t\u00e9 mesur\u00e9es \u00e0 pression atmosph\u00e9rique et normalis\u00e9es \u00e0 une temp\u00e9rature de r\u00e9f\u00e9rence de 22 \u00b0C.<\/i><\/p>\n<p>Pour consulter une version am\u00e9lior\u00e9e de ce graphique, veuillez visiter\u00a0:<br \/>\n<a href=\"\/fr\/\"https:>https:\/\/images.newsfilecorp.com\/files\/7968\/296156_62987d9b34881b41_001full.jpg<\/a><\/p>\n<p>Chiffre\u00a0<b>2<\/b>\u00a0L&#039;importance de l&#039;augmentation des concentrations en H\u2082 (ppmV) avec la profondeur, mesur\u00e9e le long du forage DDH-26-03, est mise en \u00e9vidence. Un examen rapide de la figure montre que, malgr\u00e9 son importance reconnue, le RQD n&#039;explique pas enti\u00e8rement la variabilit\u00e9 de l&#039;hydrog\u00e8ne observ\u00e9e dans le forage. Par exemple, les valeurs les plus \u00e9lev\u00e9es du forage DDH-26-03 sont observ\u00e9es dans des zones de RQD mod\u00e9r\u00e9, et les valeurs les plus faibles dans une zone de faible concentration en H\u2082. Cette observation est importante car elle souligne le r\u00f4le d&#039;autres param\u00e8tres, tels que la br\u00e9chification tectonique des roches, clairement visible sur la section comprise entre 400 et 510 m. Ce processus semble \u00eatre le m\u00e9canisme \u00e0 l&#039;origine de la perm\u00e9abilit\u00e9 n\u00e9cessaire au transport de l&#039;hydrog\u00e8ne dans les roches d\u00e9voniennes de la r\u00e9gion.<\/p>\n<p><a href=\"\/fr\/\"https:><img class=\"\\\"releaseimage\\\"\" src=\"\\\"https:><\/a><\/p>\n<p><i><b>Figure 2.<\/b>\u00a0Diagramme montrant la variabilit\u00e9 des concentrations de H2 (ppmV) et du RQD (%) en fonction de la profondeur mesur\u00e9e le long du trou DDH-26-03 situ\u00e9 dans la zone de Reid Farm (West Advocate).<\/i><\/p>\n<p>Pour consulter une version am\u00e9lior\u00e9e de ce graphique, veuillez visiter\u00a0:<br \/>\n<a href=\"\/fr\/\"https:>https:\/\/images.newsfilecorp.com\/files\/7968\/296156_62987d9b34881b41_002full.jpg<\/a><\/p>\n<p><b>Importance g\u00e9ologique de la zone 300-543 m<\/b><\/p>\n<p>L&#039;architecture g\u00e9ologique de l&#039;intervalle 300-543 m diff\u00e8re des zones pr\u00e9c\u00e9demment d\u00e9crites dans DDH-26-01, DDH-26-02 et la partie sup\u00e9rieure de DDH-26-03. Ce nouvel intervalle plus profond est caract\u00e9ris\u00e9 par une d\u00e9formation structurale, une alt\u00e9ration et des fracturations plus intenses, que la Soci\u00e9t\u00e9 interpr\u00e8te comme des facteurs potentiellement importants influen\u00e7ant la migration et l&#039;accumulation d&#039;hydrog\u00e8ne.<\/p>\n<p>L&#039;intervalle 300-543 m est d\u00e9fini par une zone de structure intensifi\u00e9e caract\u00e9ris\u00e9e par\u00a0:<\/p>\n<ol>\n<li><b>Br\u00e8che de faille cisaill\u00e9e majeure entre 478 et 509 m environ.<br \/>\n<\/b><br \/>\nUn intervalle de 31 m\u00e8tres de br\u00e8che de faille noire, \u00e0 foliation mod\u00e9r\u00e9e \u00e0 forte, a \u00e9t\u00e9 observ\u00e9. Il contient des fragments anguleux de veines de quartz broy\u00e9es et de siltite, inclus dans une matrice \u00e0 grain fin. Cet intervalle est interpr\u00e9t\u00e9 comme une zone structurale majeure et une voie potentielle de migration des fluides.<\/li>\n<li><b>Dykes felsiques intrusifs \u00e0 proximit\u00e9 du pic de r\u00e9ponse \u00e0 l&#039;hydrog\u00e8ne<br \/>\n<\/b><br \/>\nDes dykes felsiques de quartz rose-orang\u00e9 et de feldspath potassique ont \u00e9t\u00e9 observ\u00e9s \u00e0 l&#039;int\u00e9rieur ou \u00e0 proximit\u00e9 de l&#039;intervalle de br\u00e8che de faille plus large. Leur association spatiale avec des teneurs \u00e9lev\u00e9es en hydrog\u00e8ne est g\u00e9ologiquement notable et sera \u00e9valu\u00e9e dans le cadre de l&#039;interpr\u00e9tation structurale et g\u00e9ochimique en cours de la Soci\u00e9t\u00e9.<\/li>\n<li><b>alt\u00e9ration de l&#039;h\u00e9matite et de la s\u00e9ricite<br \/>\n<\/b><br \/>\nCet intervalle pr\u00e9sente des surimpressions d&#039;h\u00e9matite brun-rouge\u00e2tre, une br\u00e8che alt\u00e9r\u00e9e \u00e0 la s\u00e9ricite et des veines de quartz s\u00e9riciteuses. Ces caract\u00e9ristiques d&#039;alt\u00e9ration sont compatibles avec un syst\u00e8me structural chimiquement r\u00e9actif.<\/li>\n<li><b>Silicification et pyrite diss\u00e9min\u00e9e en faible quantit\u00e9<br \/>\n<\/b><br \/>\nUne siltite fortement br\u00e9chifi\u00e9e et silicifi\u00e9e, contenant environ 1 \u00e0 21 TP3T de pyrite finement diss\u00e9min\u00e9e, a \u00e9t\u00e9 observ\u00e9e pr\u00e8s de la partie inf\u00e9rieure de l&#039;intervalle \u00e9tudi\u00e9. La Soci\u00e9t\u00e9 consid\u00e8re cette caract\u00e9ristique comme pertinente pour son \u00e9valuation continue des conditions redox et du potentiel de pr\u00e9servation de l&#039;hydrog\u00e8ne.<\/li>\n<li><b>horizons de conglom\u00e9rat \u00e0 galets de quartz<br \/>\n<\/b><br \/>\nDes conglom\u00e9rats \u00e0 galets de quartz ont \u00e9t\u00e9 observ\u00e9s pr\u00e8s de la partie inf\u00e9rieure de l&#039;intervalle. Ces horizons lithologiques pourraient avoir une incidence sur la perm\u00e9abilit\u00e9, le stockage ou les voies d&#039;\u00e9coulement des fluides et seront \u00e9valu\u00e9s dans le cadre de l&#039;interpr\u00e9tation g\u00e9ologique en cours.<\/li>\n<li><b>stockwerk de calcite \u00e0 remplissage de fracture<br \/>\n<\/b><br \/>\nUne zone de fractures et de veinules remplies de calcite a \u00e9t\u00e9 observ\u00e9e dans la partie inf\u00e9rieure de l&#039;intervalle, indiquant un r\u00e9seau de fractures d\u00e9velopp\u00e9 et un mouvement de fluide ant\u00e9rieur.<\/li>\n<\/ol>\n<p><b>Comparaison avec les r\u00e9sultats pr\u00e9c\u00e9demment publi\u00e9s des \u00e9tudes DDH-26-01, DDH-26-02 et Upper DDH-26-03<\/b><\/p>\n<p>R\u00e9sultats pr\u00e9c\u00e9demment annonc\u00e9s de\u00a0<b>DDH-26-01<\/b>,\u00a0<b>DDH-26-02<\/b>\u00a0et le\u00a0<b>partie sup\u00e9rieure de DDH-26-03<\/b>\u00a0Des lectures anormales de l&#039;espace de t\u00eate du champ d&#039;hydrog\u00e8ne naturel ont \u00e9t\u00e9 identifi\u00e9es dans des zones moins profondes et contr\u00f4l\u00e9es par la structure.<\/p>\n<p>Le rapport r\u00e9cemment publi\u00e9\u00a0<b>Intervalle de 380 \u00e0 543 m dans DDH-26-03<\/b>\u00a0repr\u00e9sente une augmentation notable de :<\/p>\n<ul>\n<li>longueur de l&#039;intervalle\u00a0;<\/li>\n<li>fr\u00e9quence des lectures \u00e9lev\u00e9es\u00a0;<\/li>\n<li>nombre de r\u00e9ponses instrumentales primaires hors plage\u00a0;<\/li>\n<li>valeurs de v\u00e9rification crois\u00e9e secondaires s\u00e9lectionn\u00e9es ; et<\/li>\n<li>Complexit\u00e9 structurelle de l&#039;intervalle h\u00f4te.<\/li>\n<\/ul>\n<p><b>Mod\u00e8le R2G2\u2122 et interpr\u00e9tation structurelle<\/b><\/p>\n<p>L&#039;interpr\u00e9tation en cours de QIMC chez West Advocate est en cours d&#039;int\u00e9gration avec le syst\u00e8me propri\u00e9taire de la soci\u00e9t\u00e9.\u00a0<b>R2G2\u2122 \u2014 G\u00e9ostructure de rift et de graben r\u00e9activ\u00e9e \u2014 cadre<\/b>, D\u00e9velopp\u00e9 en collaboration avec l&#039;INRS, le mod\u00e8le R2G2\u2122 est utilis\u00e9 pour \u00e9valuer les corridors structuraux profonds, la r\u00e9activation des failles, les contrastes lithologiques et les anomalies g\u00e9ochimiques susceptibles d&#039;influencer la production, la migration et la pr\u00e9servation de l&#039;hydrog\u00e8ne naturel.<\/p>\n<p>L&#039;intervalle DDH-26-03 (380-543 m) est interpr\u00e9t\u00e9 par la Soci\u00e9t\u00e9 comme \u00e9tant compatible avec le type de contexte structural complexe cibl\u00e9 par le cadre R2G2\u2122. Cet intervalle repr\u00e9sente une augmentation significative de l&#039;\u00e9paisseur et de l&#039;intensit\u00e9 des zones hydrog\u00e9n\u00e9es observ\u00e9es \u00e0 ce jour et conforte le mod\u00e8le \u00e9volutif de la Soci\u00e9t\u00e9 concernant les syst\u00e8mes hydrog\u00e9n\u00e9s contr\u00f4l\u00e9s par la profondeur.<\/p>\n<p><b>PROCHAINES \u00c9TAPES<\/b><\/p>\n<p>Les priorit\u00e9s techniques imm\u00e9diates de QIMC comprennent la v\u00e9rification et la compilation compl\u00e8tes de toutes les donn\u00e9es de boue ISOJAR DDH-26-03, l&#039;int\u00e9gration des r\u00e9sultats sur l&#039;hydrog\u00e8ne avec une description lithologique et structurale d\u00e9taill\u00e9e, la corr\u00e9lation de l&#039;intervalle 380-543 m avec les donn\u00e9es g\u00e9ophysiques et structurales de fond de puits, et la mise \u00e0 jour du mod\u00e8le g\u00e9ologique de la Soci\u00e9t\u00e9 pour le syst\u00e8me d&#039;hydrog\u00e8ne naturel de West Advocate \u00e0 mesure que le forage se poursuit vers la profondeur de 900 m.<\/p>\n<p><b>\u00c0 propos de la Soci\u00e9t\u00e9 des mat\u00e9riaux innovants du Qu\u00e9bec.<\/b><\/p>\n<p>Qu\u00e9bec Mat\u00e9riaux Innovatifs Corp. est une soci\u00e9t\u00e9 nord-am\u00e9ricaine d&#039;exploration et de d\u00e9veloppement qui fait progresser un portefeuille de projets d&#039;hydrog\u00e8ne naturel et de min\u00e9raux critiques. La soci\u00e9t\u00e9 d\u00e9ploie son mod\u00e8le d&#039;exploration d&#039;hydrog\u00e8ne \u00e0 l&#039;\u00e9chelle d&#039;un district au Qu\u00e9bec, en Ontario, en Nouvelle-\u00c9cosse et au Minnesota, en tirant parti de son cadre exclusif R2G2\u2122.<\/p>\n<p>QIMC s&#039;engage en faveur d&#039;une exploration responsable, d&#039;une innovation technique et d&#039;un d\u00e9veloppement durable, dans le but de soutenir les initiatives en mati\u00e8re d&#039;\u00e9nergie propre et de d\u00e9carbonation.<\/p>\n<div id=\"\\\"contactinfo\\\"\">\n<p><b>Pour plus d&#039;informations\u00a0:<\/b><br \/>\n<b>QU\u00c9BEC MAT\u00c9RIAUX INNOVANTS CORP.<\/b><br \/>\nJohn Karagiannidis<br \/>\nPr\u00e9sident et chef de la direction<br \/>\nE-mail:\u00a0<a href=\"\/fr\/\"mailto:info@qimaterials.com\\\"\" rel=\"\\\"nofollow\\\"\">info@qimaterials.com<\/a><br \/>\nT\u00e9l. : +1 514-726-7058<\/p>\n<\/div>\n<p><i><b>Clause de non-responsabilit\u00e9<\/b><\/i><\/p>\n<p><i>Ni la Bourse canadienne des valeurs mobili\u00e8res ni son fournisseur de services de r\u00e9glementation n&#039;assument la responsabilit\u00e9 de l&#039;exactitude ou de l&#039;exhaustivit\u00e9 du pr\u00e9sent communiqu\u00e9.<\/i><\/p>\n<p><i><b>Mise en garde concernant les \u00e9nonc\u00e9s prospectifs<\/b><\/i><\/p>\n<p><i>Ce communiqu\u00e9 de presse contient des \u00e9nonc\u00e9s prospectifs au sens de la l\u00e9gislation canadienne applicable en mati\u00e8re de valeurs mobili\u00e8res, y compris des \u00e9nonc\u00e9s concernant les plans d&#039;exploration, l&#039;interpr\u00e9tation des observations g\u00e9ologiques, les r\u00e9sultats anticip\u00e9s de la g\u00e9ochimie du gaz, le mod\u00e8le d&#039;exploration R2G2\u2122 de la Soci\u00e9t\u00e9, les activit\u00e9s de forage pr\u00e9vues, les analyses de laboratoire, les essais de fond de puits et l&#039;importance potentielle des occurrences d&#039;hydrog\u00e8ne naturel \u00e0 West Advocate.<\/i><\/p>\n<p><i>Les \u00e9nonc\u00e9s prospectifs reposent sur les hypoth\u00e8ses et les jugements de la direction de la Soci\u00e9t\u00e9 et comportent des risques et des incertitudes connus et inconnus. Les r\u00e9sultats r\u00e9els peuvent diff\u00e9rer sensiblement de ceux pr\u00e9vus.<\/i><\/p>\n<p><i>Les mesures de gaz de l&#039;espace de t\u00eate sur le terrain constituent des indicateurs g\u00e9ochimiques pr\u00e9liminaires et ne doivent pas \u00eatre interpr\u00e9t\u00e9es comme une preuve de production commerciale, de ressources r\u00e9cup\u00e9rables ou de r\u00e9serves. Rien ne garantit que les r\u00e9sultats d&#039;exploration d\u00e9crits ici se traduiront par la d\u00e9couverte de quantit\u00e9s commercialisables d&#039;hydrog\u00e8ne naturel.<\/i><\/p>\n<p><i>Bien que la Soci\u00e9t\u00e9 estime que les informations prospectives contenues dans le pr\u00e9sent communiqu\u00e9 soient raisonnables \u00e0 la date de sa publication, ces informations sont susceptibles d&#039;\u00e9voluer et aucune garantie ne peut \u00eatre donn\u00e9e quant \u00e0 la r\u00e9alisation des r\u00e9sultats futurs. La Soci\u00e9t\u00e9 ne s&#039;engage \u00e0 aucune obligation de mise \u00e0 jour des \u00e9nonc\u00e9s prospectifs, sauf si la l\u00e9gislation en valeurs mobili\u00e8res applicable l&#039;exige. Les valeurs d&#039;hydrog\u00e8ne rapport\u00e9es dans ce communiqu\u00e9 sont des mesures g\u00e9ochimiques de gaz de l&#039;espace de t\u00eate effectu\u00e9es sur le terrain. Elles ne repr\u00e9sentent pas les concentrations in situ, les concentrations \u00e0 l&#039;\u00e9chelle du r\u00e9servoir, les d\u00e9bits, les donn\u00e9es de pression, les volumes r\u00e9cup\u00e9rables, les ressources ou les r\u00e9serves. Aucune fracturation hydraulique ni stimulation de r\u00e9servoir n&#039;a \u00e9t\u00e9 utilis\u00e9e dans les forages du programme de forage 2026 de West Advocate. Les lectures \u201d\u00a0hors plage\u00a0\u201d indiquent que l&#039;instrument de terrain principal GA5000 a d\u00e9pass\u00e9 sa limite sup\u00e9rieure de mesure de H\u2082 de 1\u00a0000\u00a0ppm. Ces valeurs ont \u00e9t\u00e9 v\u00e9rifi\u00e9es dans certains cas \u00e0 l&#039;aide d&#039;un instrument secondaire Eagle II. Les mesures de l&#039;espace de t\u00eate sont uniquement des indicateurs g\u00e9ochimiques effectu\u00e9s sur le terrain et ne repr\u00e9sentent pas les concentrations de gaz in situ, les d\u00e9bits \u00e0 l&#039;\u00e9chelle du r\u00e9servoir, les volumes r\u00e9cup\u00e9rables, les ressources ou les r\u00e9serves. L&#039;analyse formelle en laboratoire d&#039;\u00e9chantillons de gaz s\u00e9lectionn\u00e9s, pr\u00e9lev\u00e9s dans des sacs d&#039;\u00e9chantillonnage composites en feuille d&#039;aluminium, est en cours.<\/i><\/p>","protected":false},"excerpt":{"rendered":"<p>&#8211; Multiple headspace H2 readings exceed instrument range with cross-check values up to 8,961 ppmV; system remains open at depth toward 900 m Key Highlights &#8211; DDH-26-03 (300-543 m Interval) 163 metres of continuous elevated natural hydrogen headspace geochemistry\u00a0from approximately 380 m to 543 m downhole 243-metre anomalous hydrogen-bearing zone\u00a0identified between 300 m and 543 [&hellip;]<\/p>\n","protected":false},"author":4,"featured_media":978,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_eb_attr":"","iawp_total_views":22,"footnotes":""},"categories":[10,11],"tags":[],"class_list":["post-83502","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-industry-news","category-press-releases"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.7 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>QIMC Intersects 243 m Natural Hydrogen Zone Including 163 m Continuous Elevated Interval at West Advocate (DDH-26-03) - Strongest Response to Date - 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-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\/\" \/>\n<meta property=\"og:locale\" content=\"fr_CA\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"QIMC Intersects 243 m Natural Hydrogen Zone Including 163 m Continuous Elevated Interval at West Advocate (DDH-26-03) - Strongest Response to Date - QIMC\" \/>\n<meta property=\"og:description\" content=\"&#8211; Multiple headspace H2 readings exceed instrument range with cross-check values up to 8,961 ppmV; system remains open at depth toward 900 m Key Highlights &#8211; DDH-26-03 (300-543 m Interval) 163 metres of continuous elevated natural hydrogen headspace geochemistry\u00a0from approximately 380 m to 543 m downhole 243-metre anomalous hydrogen-bearing zone\u00a0identified between 300 m and 543 [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/qimaterials.com\/fr\/qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\/\" \/>\n<meta property=\"og:site_name\" content=\"QIMC\" \/>\n<meta property=\"article:published_time\" content=\"2026-05-06T11:26:42+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2026-05-14T15:27:41+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/qimaterials.com\/wp-content\/uploads\/2024\/07\/newpos2-min.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"1200\" \/>\n\t<meta property=\"og:image:height\" content=\"675\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"author\" content=\"QIMC\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"QIMC\" \/>\n\t<meta name=\"twitter:label2\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"9 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\\\/\\\/qimaterials.com\\\/qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\\\/#article\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/qimaterials.com\\\/qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\\\/\"},\"author\":{\"name\":\"QIMC\",\"@id\":\"https:\\\/\\\/qimaterials.com\\\/#\\\/schema\\\/person\\\/39435340349b65729b1463189bf3d52e\"},\"headline\":\"QIMC Intersects 243 m Natural Hydrogen Zone Including 163 m Continuous Elevated Interval at West Advocate (DDH-26-03) &#8211; 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Multiple headspace H2 readings exceed instrument range with cross-check values up to 8,961 ppmV; system remains open at depth toward 900 m Key Highlights &#8211; DDH-26-03 (300-543 m Interval) 163 metres of continuous elevated natural hydrogen headspace geochemistry\u00a0from approximately 380 m to 543 m downhole 243-metre anomalous hydrogen-bearing zone\u00a0identified between 300 m and 543 [&hellip;]","og_url":"https:\/\/qimaterials.com\/fr\/qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\/","og_site_name":"QIMC","article_published_time":"2026-05-06T11:26:42+00:00","article_modified_time":"2026-05-14T15:27:41+00:00","og_image":[{"width":1200,"height":675,"url":"https:\/\/qimaterials.com\/wp-content\/uploads\/2024\/07\/newpos2-min.jpg","type":"image\/jpeg"}],"author":"QIMC","twitter_card":"summary_large_image","twitter_misc":{"Written by":"QIMC","Est. reading time":"9 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"Article","@id":"https:\/\/qimaterials.com\/qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\/#article","isPartOf":{"@id":"https:\/\/qimaterials.com\/qimc-intersects-243-m-natural-hydrogen-zone-including-163-m-continuous-elevated-interval-at-west-advocate-ddh-26-03-strongest-response-to-date\/"},"author":{"name":"QIMC","@id":"https:\/\/qimaterials.com\/#\/schema\/person\/39435340349b65729b1463189bf3d52e"},"headline":"QIMC Intersects 243 m Natural Hydrogen Zone Including 163 m Continuous Elevated Interval at West Advocate (DDH-26-03) &#8211; 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