{"id":18180,"date":"2026-04-24T14:34:56","date_gmt":"2026-04-24T14:34:56","guid":{"rendered":"https:\/\/quantecgeo.com\/?page_id=18180"},"modified":"2026-04-24T14:46:34","modified_gmt":"2026-04-24T14:46:34","slug":"titan-case-passiflora","status":"publish","type":"page","link":"https:\/\/quantecgeo.com\/es\/titan-case-passiflora\/","title":{"rendered":"TITAN-case-Passiflora"},"content":{"rendered":"
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Viscount Mining’s Passiflora Discovery Drill Hole TITAN MT<\/h2>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n
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\n \n \n Challenges<\/span>\n
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The exploration target at Passiflora presented a typical deep-target challenge: the conductive porphyry signature began well below surface, starting around ~400 m depth and extending to at least ~1,500 m, and spanned over 2\n km laterally. Conventional geophysical methods (e.g., shallow IP, CSAMT) often lack the resolution and depth penetration needed to accurately image such a deep, extensive system. Precisely delineating the anomaly\u2019s volume\n and depth extent without excessive drilling is both technically and economically demanding<\/p>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n

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Quantec deployed its TITAN system; a deep 2D imaging method combining DC-IP during the day with MT surveying at night. TITAN MT provides high lateral resolution and depth penetration (MT resistivity to ~1,500 m+; DCIP to ~750\n m), enabling efficient multi-parameter characterization from a single line setup. For Passiflora, this allowed Quantec to define a massive low-resistivity body that begins around ~400 m, extends downward to at least 1.5 km,\n spans nearly 2.4 km in strike, and is roughly 700 m wide, representing a subsurface volume exceeding ~665 million m\u00b3<\/p>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n

\n \n \n Highlights<\/span>\n
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The TITAN MT survey successfully imaged a deeply seated, highly conductive zone, defining a robust, large-scale drill target. Guided by this imagery, Viscount confidently positioned hole PF-03A, which intersected the conductor\n at ~400 m depth and returned 843.9 m of continuous copper-gold mineralization averaging 0.214 % CuEq, including higher-grade zones of 189 m at 0.326 % CuEq and 45 m at 0.417 % CuEq\u2014well above early porphyry thresholds. The\n system remains open in all directions and at depth, with sulfide mineralization observed from surface to ~300 m and gold present in every assayed interval, underscoring both its vertical continuity and multi-metallic potential.<\/p>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n

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Title:<\/strong> Deep discovery<\/span>\n
Geology:<\/strong> Passiflora porphyry<\/span>\n
Client:<\/strong> Newmont Mining<\/span>\n
Technology:<\/strong> TITAN MT<\/span>\n
Location:<\/strong> Nevada, USA<\/span>\n
Sector:<\/strong> Mining<\/span><\/p>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n

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< Back<\/span><\/a>\n <\/span>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n <\/div>\n<\/div>","protected":false},"excerpt":{"rendered":"

Viscount Mining’s Passiflora Discovery Drill Hole TITAN MT Challenges The exploration target at Passiflora presented a typical deep-target challenge: the conductive porphyry signature began well below surface, starting around ~400 m depth and extending to at least ~1,500 m, and spanned over 2 km laterally. Conventional geophysical methods (e.g., shallow IP, CSAMT) often lack the […]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-templates\/full-width-page.php","meta":{"footnotes":""},"class_list":["post-18180","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/pages\/18180","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/comments?post=18180"}],"version-history":[{"count":2,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/pages\/18180\/revisions"}],"predecessor-version":[{"id":18189,"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/pages\/18180\/revisions\/18189"}],"wp:attachment":[{"href":"https:\/\/quantecgeo.com\/es\/wp-json\/wp\/v2\/media?parent=18180"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}