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PDAC 2020 ppp hand out 2020 [autosaved]

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PowerPoint Presentation prepared for the PDAC 202mining convention as an explainer tool for Major Mining companies, with a view to joint venture the Pecors Nickel, Copper, Platinum, Palladium, Gold project at Pecors lake, Ontario, Canada

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PDAC 2020 ppp hand out 2020 [autosaved]

  1. 1. International Montoro Resources Inc. Pecors Anomaly (2007-2020) Nickel, Copper, Platinum, Palladium and Gold massive sulphide exploration project Elliot Lake, Ontario, Canada IMT – TSXV (Canada) IMTFF – OTC/Grey market (USA ) O4T1 – Frankfurt (Germany) ISIN .....CA46004W2076 CUSIP.... 46004W207
  2. 2. 1. Introduction Overview Magmatic sulfide deposits containing nickel i) and copper (Cu), with or without (±) platinum-group elements (PGE), account for approximately 60 percent of the Worlds Nickel Production.” “The sulfide deposits form when the mantle-derived mafic and/or ultramafic magmas become sulfide-saturated and segregate immiscible sulfide liquid, commonly following interaction with continental crustal rocks” “With the exception of the deposits in the Sudbury district, Canada, which are related to a meteorite-impactgenerated melt sheet, these deposits are associated with smallto medium-sized differentiated mafic and/or ultramafic dikes and sills related mostly to tholeiitic basalt magmas emplaced in continental settings. In addition, most of the major Ni deposits in this subgroup, including the three largest producing Ni-Cu sulfide camps after Sudbury (Noril’sk-Talnakh, Russia; Jinchuan, China; and Voisey’s Bay, Canada; Eckstrand and Hulbert, 2007) are related to dynamic magmatic systems and occur in intrusions that served as magma conduits “ “ Brief Deposit Description : These magmatic sulfide deposits are significant producers of Ni and Cu resources, primarily from deposits in Russia (Noril’sk-Talnakh, Pechenga), Canada (Voisey’s Bay), and China (Jinchuan). In addition, the Noril’sk-Talnakh deposits are the world’s largest producer of palladium. These sulfide deposits form when mantle-derived, sulfur- undersaturated picrite or tholeiitic basalt magma becomes sulfide-saturated, commonly following interaction with continental crustal rocks. Sulfur saturation results in formation of an immiscible sulfide liquid. The sulfide liquid tends to segregate into physical depressions or other areas in the lower parts of dike- and/ or sill-like intrusions because of changes in the magma flow dynamics. Economic deposits appear to be associated almost 4 Occurrence Model for Magmatic Sulfide-Rich Nickel-Copper Deposits exclusively with dynamic magmatic systems that experience repeated surges of magma. Such dynamic systems appear to promote the interaction of sulfide liquid with a sufficiently large amount of silicate magma to concentrate chalcophile elements to economic levels.
  3. 3. LE. Reid, Geophysics 3D inversion of 2007 VTEM airborne survey Pecors magnetic Anomaly USGS Report 2010-5070-I pg17 Geophysical Signature - Magnetic Signaturewell- suited for mafic-ultramafic dike-sill complexes “The magnetic method is particularly well-suited for reconnaissance-scale investigations for mafic- ultramafic dike-sill complexes that might host Ni- Cu±PGE sulfide deposits” Magnetic Signaturewell-suited for mafic-ultramafic dike-sill complexes that might deposits
  4. 4. Pecors Magnetic Anomaly 57,700 nTeslas
  5. 5. Sudbury 58,962 nT Pecors (magnetic portion) 57,700 nT Record: Kursk Iron mine, Russia 60,000 nT
  6. 6. Speaking in Sudbury, 2019 Ontario’s Minister of mines stated that between ore mined and reserves in the ground the value of Sudbury is over $1Trillion. FYI mining generates $10 billion per/year to Ontario’s economy.
  7. 7. USGS Report 2010- 5070-I (pg 19) Geophysical Signatures Gravity Signature Bouguer anomalies typically range from less than one milligal to several tens of milligals. In comparison, the total gravity field of the Earth is approximately 980,000 milligals. Similar to magnetic data, gravity anomaly data can be effective for investigating the geology of the igneous and metamorphic terranes where mineral deposits may occur. Pecors Gravity Anomaly 22 MGAL
  8. 8. Gravity Comparison chart of the largest and richest Massive Sulphide Mines in the World and Pecors Anomoly.
  9. 9. Geotech ZTEM (2D) inversion airborne survey data for Pecors Anomaly viewed Mira Geoscience - Geoscience Analyst (3D) Conductive portion of Pecors Anomaly 33 ohms Magnetic Portion of Pecors Anomaly 57,700 nanoTeslas PECORS Anomaly Width: 2288 meters 1.42 miles Height: 4255 meters 2.64 miles Length:5700 meters 3.45 miles PpppppP-15_ P-15-23 (1m) Palladium .08 ppm Platinum .12 ppm Gold .09 ppm Copper 1,410 ppm Nickel 147 ppm P-15-22 (17m) Palladium .0898 ppm Platinum .02634 ppm Gold .09 ppm Copper 1,374.4 ppm Nickel 449 ppm USGS 2010 5070-I -The size and shape of deposits and ore zones depend on the form and orientation of the host unit, generally an intrusive body and adjacent footwall rocks, on any ore- localizing feature (for example, footwall embayments), and on the nature and distribution of the sulfides (table 5–1). Host intrusions typically range from tens to a few hundreds of meters in thickness, about 100 to 2,000 meters wide, and hundreds of meters to several kilometers in length, to plug-like intrusions generally
  10. 10. Pecors Conductive Anomaly, Geotech ZTEM (2D) Conductive/ (EM) data in Geoscience analyst (3D)Drill hole location and depth > P-15-23 and location P-15-22 (1000m)- Crone 2015 P-15-23 P-15-22 RioTinto Drill hole(s) Crone down hole probe 2015 Electromagnetic (EM) Signature USGS Report 2010-5070-I pg33 “Sulfide minerals associated with suplfide-rich Ni,Cu+PGE deposits are highly conductive, and massive to semi-massive present highly favorable EM targets…Particularly helpful with the Voisey Bay Deposits” ciated with sulfide-rich Ni- Cu±PGE deposits Data Showing total area of 3 Ohm Resistivity
  11. 11. Geotec ZTEM 2D Synthetic Modeling Pecors/Serpent River Project, Elliot Lake Ontario Canada Buried Magmatic Massive Sulphide Target
  12. 12. Geotech ZTEM surveys Inversion model Montoro -Pecors (left panel) Vale - Voisey Bay Eastern Deeps (below) Mineral Explora tion Using Natural EM Fields Jansen, J.C. [1] , Cristall, J.A. [1] ~1-5 Ωm(ohms) Voisey Bay/Eastern Deeps Source: Mineral Exploration Using Natural EM Fields Jansen, J.C. [1] , Cristall, J.A. [1]
  13. 13. USGS Report 2010 – 5070 pg.23 Resistivity (EM) Data - Vale, Voisey Bay, (Ovoid deposit) Labrador, Canada) USGS Report 2010 – 5070 pg.23
  14. 14. Pecors Anomaly 2015 Drill program:Assays and Sulphides with core descriptions by Geologist's
  15. 15. New Insights into the geology of the basal Huronian Supergroup in the Elliot Lake area: Implications for Mineral Exploration R.M. Easton Precambrian Geoscience Section, Ontario Geological Survey, Sudbury 2010 https://www.slideshare.net/slidesho w/embed_code/46092921 OGS Geochemical Survey Sulphur - Pecors Lake “Brief Deposit Description These magmatic sulfide deposits are significant producers of Ni and Cu resources, primarily from deposits in Russia (Noril’sk-Talnakh, Pechenga), Canada (Voisey’s Bay), and China (Jinchuan). In addition, the Noril’sk-Talnakh deposits are the world’s largest producer of palladium. These sulfide deposits form when mantle-derived, sulfur- undersaturated picrite or tholeiitic basalt magma becomes sulfide-saturated, commonly following interaction with continental crustal rocks. Sulfur saturation results in formation of an immiscible sulfide liquid. The sulfide liquid tends to segregate into physical depressions or other areas in the lower parts of dike- and/ or sill-like intrusions because of changes in the magma flow dynamics. Economic deposits appear to be associated almost 4 Occurrence Model for Magmatic Sulfide-Rich Nickel-Copper Deposits exclusively with dynamic magmatic systems that experience repeated surges of magma. Such dynamic systems appear to promote the interaction of sulfide liquid with a sufficiently large amount of silicate magma to concentrate chalcophile elements to economic levels.” USGS Report 2010-5070-I (04.2014)
  16. 16. P-15-23 (full depth 1317 meters) *Note the red square area (Crone Geophysics down hole probe data) • P-15-23 interacts with the Pecors Conductive Anomaly • @ 880.7 meters – 881.70 (1) meter Assayed for Nickel, Copper, Platinum, Platinum, Gold Pecors Geoscience Analyst Exploration project Data Graphic. The coloured balls are OGS Geochem 2010 survey indicated anomalous lake/River mineral/sediments. The lines are the flight route of the Geotech ZTEM survey Rio-Tinto drill holes Pecors Anomaly (Conductive) Geotech ZTEM indicated data, viewed in Geoscience Analyst
  17. 17. ~3ohms Conductive Portion 4.3km x1.2km X 1.2km >57,700 nanoTeslas 4km x 1.3 km X1.1km
  18. 18. www.Montororesources.com Vancouver,B.C., Canada Suite 600-625 Howe St. 604-683-6648

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