Report on the Gradient IP Survey

We are committed to providing accessible customer service. If you need accessible formats or communications supports, please contact us. <a href="mailto:[email protected]?subject=Probleme%20Accessibilite" target="_blank">Nous tenons à </a>améliorer l’accessibilité des services à la clientèle. Si vous avez besoin de formats accessibles ou d’aide à la communication, veuillez nous contacter. 1REPORT ON THE GRADIENT IP SURVEY MELBA AND BERNHARDT TOWNSHIPS DISTRICTS OF COCHRANE AND TIMISKAMING ONTARIO FOR JONATHAN CAMILLERI TABLE of CONTENTS Introduction 1. <ul style="display: flex;"><li style="flex:1">Property </li><li style="flex:1">2. </li></ul>3. 4. 5. Location and Access Regional and Property Geology Previous work in the Area Gradient IP Survey Program and Results Summarry and Recommendations Expenditure 6. 7. 8. References 9. Certificate of Qualification Appendices 10. 11. LIST of TABLES <ul style="display: flex;"><li style="flex:1">Camilleri Melba Property </li><li style="flex:1">MLAS Claims/cells </li><li style="flex:1">Ta ble 1 </li></ul><ul style="display: flex;"><li style="flex:1">Melba and Bisley Twps </li><li style="flex:1">Table 2 Table of Lithologic Units </li></ul>LIST of FIGURES Figure 1 Property Location Camilleri Melba Property and MLAS Claims/cells Figure 2 <ul style="display: flex;"><li style="flex:1">Figure 3 </li><li style="flex:1">Location and Access </li></ul><ul style="display: flex;"><li style="flex:1">Field Survey Map, Melba Twp. </li><li style="flex:1">Figure 4 Airborne Residual Magnetic </li></ul>Gradient IP Survey Lines-- Location Map Gradient IP survey Line 71 E Gradient IP Survey Line 72 E Figure 5 Figure 6 Figure 7 <ul style="display: flex;"><li style="flex:1">·</li><li style="flex:1">1. Introduction </li></ul>Melba Property (the Property) was aqulr�d <ul style="display: flex;"><li style="flex:1">Camilleri </li><li style="flex:1">for </li><li style="flex:1">The </li></ul>ꢀꢁꢂ The eto host gold and copper mineralization of 1 conomic t<ul style="display: flex;"><li style="flex:1">'</li><li style="flex:1">potential </li></ul>t<ul style="display: flex;"><li style="flex:1">in </li><li style="flex:1">ere </li></ul>ꢄgroup of cl,aimꢄ iꢄ located in the noꢃheaꢄt quadrant of Melba townꢄihip, approxiꢅꢆꢇꢈly 15 km north of Kirkland Lake, Diꢄtrict of Timiꢄkaming, Larder Lake Mining Diviꢄion, Ontario. Between November 14 and 20, 2018, 2 lineꢄ of Gradient Induced Polarization (IP) ꢄurveying totaling <ul style="display: flex;"><li style="flex:1">km were completed. The ꢄurvey waꢄ carried out by Dan Patrie </li><li style="flex:1">8</li></ul>Exploration Ltd, with C. Brent Patrie, an experienced geophyꢄical contactor The following report preꢄentꢄ a brief review of the regional and <ul style="display: flex;"><li style="flex:1">geology aꢄ well aꢄ a ꢄummary of previouꢄ work in the area and </li><li style="flex:1">property </li></ul><ul style="display: flex;"><li style="flex:1">deꢄcription of the work done and the reꢄultꢄ obtained. </li><li style="flex:1">a</li></ul><ul style="display: flex;"><li style="flex:1">2. </li><li style="flex:1">Property </li></ul>The Claim Group being reported on conꢄiꢄtꢄ of MLAS active mining claimꢄ/cellꢄ aꢄ ꢄhown in Figure 2 and aꢄ liꢄted in Table i They cover an area of approximately 800 ha. <ul style="display: flex;"><li style="flex:1">3. </li><li style="flex:1">Location and Acceꢄꢄ </li></ul>The Claim Group. iꢄ located in the northeaꢄtern quadrant of Melba townꢄhip, adjacent to the north-ꢄouth townꢄhip boundary line with Biꢄley twp to the eaꢄt, and iꢄ centred at UTM co-ordinateꢄ, NAO 83, Zone 17, 571 500mE, 5351 OOOmN. The Claim Group iꢄ approximately 1 5 km north of Kirkland Lake and can be acceꢄꢄed by gravel/dirt roadꢄ aꢄ ꢄhown in Figure 3. TABLE 1 CAMILLERI MELBA PROPERTY MLAS CLAIMS/CELLS MLAS Legacy Number Claim Number Claim 4265069 MELBA 30634 i 239056 203120 203119 190943 182995 158438 143819 143818 239057 210414 108025 343700 312210 305459 292789 292787 256240 237584 226169 226168 192344 345129 313141 308287 308286 305459 260521 248507 240451 240450 226168 203120 193800 192343 182702 174277 174276 159798 143819 139731 108025 335921 239057 143817 345129 325830 313141 BISLEYMELBA ,04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 04265070 4265069 4265069 4265069 4265069 4265069 4265069 4265069 4265069 4265069 4265069 4265069 4265071 4265071 4265071 MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA BISLEY,MELBA BISLEY,MELBA MELBA MELBA MELBA 4265071 4265071 4265071 MELBA MELBA MELBA 4265071 4265071 4265071 4265071 4265071 4265071 4265071 4265071 4265071 MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA MELBA 219352 201620 189467 182703 182702 BISLEYMELBA ,BISLEY,MELBA BISLEY,MELBA MELBA 4265069 4265069 MELBA MELBA 4265069 <ul style="display: flex;"><li style="flex:1">Regional and Property Geology </li><li style="flex:1">4. </li></ul>Melba and Bisley townships are underlain by Archean-age metavolcanic rocks of the Blake River Group which extends from Timmins in the west to and beyond, Noranda, Quebec in the east in the form of a large synclinorium. The geological sequence is summarized in Table 2, Table of Lithologic Units. The Archean assemblage is a volcanic sequence with interbedded metasediments in the upper part. Intermediate metavolcanics are predominant, however, mafic metavolcanics occur in the upper part of the sequence while the lower part is mainly felsic metavolcanics. Regional alteration in general is of a very low grade. Late mafic intrusive rocks of Matachewan age occur in Melba township as part of a swarm of north-trending diabase dykes extending east from Benoit township Major faults in the area trend north to north-northwest (Ontario Geological Survey, Map 2252) Pleistocene deposits consist of sand, gravel and clay deposited on the Archean basement during the Wisconsin glacial retreat ( Jensen, 1972) -Figure 4 is a copy of the OGS airborne survey map of Melba township which shows very well the regional lithological trends. The Melba claims in the southeast part of the township lie in an area of Intermediate metavolcanic rocks while the claims along the Melba-Bernhardt township area cover an area of mafic metavolcanic units (OGS prel. Map P. 519, Melba Township) Table 2 TABLE OF LITHOLOGIC UNITS MELBA AND EISLEY TOWNSII- IPS CENOZOIC RECENT Peat, alluvium PLEISTOCENE Gravel, sand, silt, varved clay Unco1 1 formity PRECAMBRIAN ARCHEAN LATE MAFIC IN'fRUSIVE ROCKS Quartz diabase (dikes) Int r usive Conta c t FELSIC INTRUSIVE ROCKS Hornblende diotite, monzonite porphyry Int ru siv e Cont a c t EARLY MAFIC INTRUSIVE ROCKS Gabbro, quartz gabbro, ho1·nblende gabbro I nt r usiv e Cont ac t FELSIC VOLCANIC ROCKS Pillow lava, flow brcccia, pyroclastic rocks INTERMEDIATE VOLCANIC AND SEDIMENTARY ROCKS Massive lava, pillow lava, flow breccia, pyroclastic rocks, argillite MAFIC VOLCANIC ROCKS Basalt, andesite, massive lava, pillow lava, flow breccia 5. Previous Work in the Area At some time following the discoveꢂy of gold in the Kiꢂkland Lake aꢂea in 1906 based on the pꢂesence of old pits in Melba township, however, the fiꢂst <ul style="display: flex;"><li style="flex:1">woꢂk dates fꢂom 1934. At this time in the noꢂthwesteꢂn quadꢂant </li><li style="flex:1">ꢂecoꢂded </li></ul>of Melba township, north of the Black River gold mineralization was discovered followed by extensive suꢀace woꢂk, undeꢂgꢂound exploꢂation and diamond dꢂilling. The opeꢂation was shut down due to the onset of Woꢂld Waꢂ II in 1939. The next woꢂk was in 1959 by Pitchvein Mines Limited thꢂough to 1963 and consisted of stꢂipping, dewateꢂing of the shaft and woꢂkings, UG mapping and sampling and surface and UG diamond drilling. The Property was shut down <ul style="display: flex;"><li style="flex:1">1963. This pꢂopeꢂty is cuꢂꢂently ꢂepꢂesented by the patented claims in this </li><li style="flex:1">in </li></ul><ul style="display: flex;"><li style="flex:1">aꢂea. </li><li style="flex:1">A bulk sample taken fꢂom UG ꢂetuꢂned 0.210 oz gold peꢂ ton acꢂoss a </li></ul>vein width of 4.5 ft. In 1962 chalcopyrite mineralization was discovered in the northeastern <ul style="display: flex;"><li style="flex:1">of Melba township and oveꢂ the next 3 yeaꢂs seveꢂal pits weꢂe put down.. </li><li style="flex:1">paꢂt </li></ul><ul style="display: flex;"><li style="flex:1">1965 Midꢂim Mining Company Limited optioned the pꢂopeꢂty, caꢂꢂied out an </li><li style="flex:1">In </li></ul>aiꢂboꢂne suꢂvey and dꢂilled 7 holes ꢁꢂ a total of 2932 ft..The main vein is 1 foot wide and 500 ft long and contains small specks of chalcopyꢂite and gold. In the last 20 yeaꢂs oꢂ so the eskeꢂ tꢂending south thꢂough the centꢂal paꢂt of the pꢂoperty has been sampled and the pꢂopeꢂty has been coveꢂed by aiꢂboꢂne suꢂveys as part of the OGS Discoveꢂ Abitibi project. 6. Gradient IP Survey Program and Results <ul style="display: flex;"><li style="flex:1">Novembeꢂ 14 and 20 inclusive, C. Bꢂent Patꢂie, at the </li><li style="flex:1">Between </li></ul>ꢂequest of Mꢂ. Camilleꢂi caꢂꢂied out a Gꢂadient IP Survey on the Camilleꢂi Melba Pꢂopeꢂty...The pꢂogꢂam consisted of line cutting and surveying along 2 north-south lines as shown in Figure 5. Two lines aꢂe in the noꢂtheasteꢂn paꢂt of Melba township immediately east of <ul style="display: flex;"><li style="flex:1">block of patented claims in this aꢂea. These claims contain the </li><li style="flex:1">the </li></ul>1 ft wide vein caꢂꢂying gold and coppeꢂ values. <ul style="display: flex;"><li style="flex:1">Gradient IP Survey Program and Results </li><li style="flex:1">6. </li></ul>Beꢃweeꢌ November 14 aꢌd 20 ꢋꢌclusꢋve, C. ꢀꢁeꢂꢃ Patꢁꢋe, at the ꢁequesꢃ ꢅf Mr. Camꢋlleꢁi carrꢋed ꢅuꢃ a Gꢁadieꢌt IP Surveꢇ ꢅn ꢃhe Cammeri Melba ꢄꢁꢅpeꢆꢇ...Tꢙe program cꢅꢌsꢋsted of liꢌe ꢈꢉꢊꢋꢌꢍ and <ul style="display: flex;"><li style="flex:1">as showꢎ in Fiꢍure 5. </li><li style="flex:1">eyinꢍ alꢓꢎꢍ 2.ꢎꢏꢐꢑ-ꢒꢓꢔꢕꢖ lines </li></ul>Two iines suꢁv are in tꢙe ꢌꢅrtꢙeasteꢁꢌ parꢃ ꢅf Melba ꢃꢏꢗꢘsꢙꢚꢛ ꢋmmedꢋaꢃelꢇ east of the block ꢅf pateꢌted claims nꢌ this aꢁea. These claꢚms cꢅꢌtaꢋꢌ the 1 ﬅ wide veiꢌ carꢁꢇꢚꢌꢍ ꢍꢅld aꢌd cꢅppeꢁ values. The two surveyed lines, 71E and 72E aꢁe both 4 km long, tꢁend noꢁth-south, aꢁe paꢁallel (Figuꢁe 5) and weꢁe coveꢁed by a Gꢁadient IP survey oveꢁ a 3 day peꢁiod, 14 - 16 Novembeꢁ 2018. The Gꢁadient IP <ul style="display: flex;"><li style="flex:1">is of a ꢁeconnaissance natuꢁe and was executed as follows. </li><li style="flex:1">appꢁoach </li></ul>Staꢁting on the 14 Novembeꢁ 2018, two cuꢁꢁent electꢁodes connected by an electꢁic cable weꢁe laid out in a north-south diꢁection and centꢁed on the aꢁea of inteꢁest. (Figuꢁe 4). The southeꢁn cuꢁꢁent electꢁode was put in place at UTM co-oꢁdinates 571700mE, 5349000mN, 500 metꢁes south of the pꢁoposed suꢁvey aꢁea. The geneꢁatoꢁ and tꢁansmitteꢁ weꢁe alsb located at this site. The noꢁtheꢁn cuꢁꢁent electꢁode was placed at UTM co-oꢁdinates, 571700mE, 5354000mN ; ie, 5000 m north of the south <ul style="display: flex;"><li style="flex:1">and 500 m noꢁth of the noꢁth ends of the two suꢁvey lines. </li><li style="flex:1">electꢁode </li></ul>Following the emplacement of the cuꢁꢁent electꢁodes, Line 71E was suꢁveyed staꢁting appꢁoximately 400 metꢁes west of the cuꢁꢁent electꢁode line at UTM co-ordinates 571300mE, 5349000mN ( L71 0+00 N) The survey line was pꢁevi9usly ut and GPS ꢁeadings and IP ꢁeadings weꢁe ctaken at 50 metꢁe inteꢁvals, a = 50 metꢁes. The fiꢁst ꢁeading was taken starting at the south end of the line with consecutive ꢁeadings at 50 metꢁe inteꢁvals to the noꢁth end of the line foꢁ a total of 80 ꢁeadings (4000 m). A similaꢁ appꢁoach was used foꢁ Line 72E. On 14 Novembeꢁ 2 line-km weꢁe coveꢁed on Line 71E and on 15 Novembeꢁ the noꢁtheꢁn 2 km weꢁe surveyed plus 1 line-km on Line· 72E. The ꢁemaining 3 line-km on Line 72E weꢁe suꢁveyed on 16 Novembeꢁ ꢀꢁ a total of 8 line-km. <ul style="display: flex;"><li style="flex:1">culates </li><li style="flex:1">cal </li></ul>Receiver <ul style="display: flex;"><li style="flex:1">IPR-12 </li><li style="flex:1">the </li><li style="flex:1">field, </li><li style="flex:1">the </li></ul>in taken <ul style="display: flex;"><li style="flex:1">reading </li><li style="flex:1">each </li><li style="flex:1">For </li></ul>,<ul style="display: flex;"><li style="flex:1">taken </li><li style="flex:1">readings </li><li style="flex:1">the </li><li style="flex:1">to </li></ul>dition ad In <ul style="display: flex;"><li style="flex:1">site. </li><li style="flex:1">r the </li></ul>fo <ul style="display: flex;"><li style="flex:1">resistivity </li><li style="flex:1">and </li><li style="flex:1">iity </li></ul>chargeabi electrode the nt <ul style="display: flex;"><li style="flex:1">re </li><li style="flex:1">cu </li><li style="flex:1">. The </li></ul><ul style="display: flex;"><li style="flex:1">erator </li><li style="flex:1">o</li><li style="flex:1">the </li><li style="flex:1">by </li></ul><ul style="display: flex;"><li style="flex:1">noted </li><li style="flex:1">also </li><li style="flex:1">are </li></ul>is locations reading and �array time �the <ul style="display: flex;"><li style="flex:1">lo .of </li><li style="flex:1">plet </li></ul>mco eth ina llow Fo ded. cor re also �<ul style="display: flex;"><li style="flex:1">the </li><li style="flex:1">of </li></ul><ul style="display: flex;"><li style="flex:1">the </li><li style="flex:1">at </li><li style="flex:1">ge </li></ul>volta _ ·yt<ul style="display: flex;"><li style="flex:1">ivi </li><li style="flex:1">ist </li></ul>res ꢀli bi ea arg <ul style="display: flex;"><li style="flex:1">ch </li><li style="flex:1">the </li></ul>vey, sur mre fro thꢁ m and <ul style="display: flex;"><li style="flex:1">ra </li><li style="flex:1">prog </li></ul><ul style="display: flex;"><li style="flex:1">Geosoﬅ </li><li style="flex:1">a</li></ul>be with can uter mp <ul style="display: flex;"><li style="flex:1">co </li><li style="flex:1">a</li></ul><ul style="display: flex;"><li style="flex:1">to </li><li style="flex:1">2 Receiver </li></ul>IPR-1 eth mfro nd i te en es cpr ps as <ul style="display: flex;"><li style="flex:1">ma </li><li style="flex:1">as </li><li style="flex:1">plotted </li></ul><ul style="display: flex;"><li style="flex:1">ues </li><li style="flex:1">val </li></ul>esistivity d r an Mr <ul style="display: flex;"><li style="flex:1">lity </li><li style="flex:1">abi </li><li style="flex:1">rge </li><li style="flex:1">cha </li></ul>the

Report on the Gradient IP Survey

Details

Download

Copyright

We respect the copyrights and intellectual property rights of all users. All uploaded documents are either original works of the uploader or authorized works of the rightful owners.

Support