Brian J. Groves Geophysicist REPORT ON AN AIRBORNE ELECTROMAGNETIC AND MAGNETIC SURVEY CARMAN TOWNSHIP, ONTARIO DELORO CLAIMS PROJECT ION
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1 - -,,-.... IVM* w mi m 42A06NE0284 S,5267 CARMAN 010 REPRT N AN AIRBRNE ELECTRMAGNETIC AND MAGNETIC SURVEY CARMAN TWNSHIP, NTARI DELR CLAIMS PRJECT IN NTS: 42-A-6/7 AMAX MINERALS EXPLRATIN Timmins, ntario November 1982 Brian J. Groves Geophysicist
2 SUMMARY An airborne electromagnetic and magnetometer survey was flown over 4 claims in Carman township. Magnetic data suggest the presence of a northerly trending diabase dyke cutting felsic vol canics or sediments. ne electromagnetic response was recorded over the pro perty. The source of the response is doubtful and limited ground geophysical surveying is suggested to resolve the causative source of the conductor.
3 42A86NE8284 2,5267 C ARMAN TABLE F CNTENTS 010C SUMMARY I. INTRDUCTIN II. LCATIN AND ACCESS III. EXPLRATIN HISTRY AND GENERAL GELGY Previous Work Regional Geology Property Geology IV. SURVEY EQUIPMENT AND PRCEDURES V. DATA PRESENTATIN VI. DISCUSSIN F RESULTS Magnetic Survey Electromagnetic Survey VII. CNCLUSINS VIII. LIST F REFERENCES l l l APPENDIX A LIST F APPENDICES SCHEDULE F CLAIMS After Page 6 FIGURE l FIGURE 2 LIST F FIGURES LCATIN F SURVEY AREA CLAIM SKETCH After Page l After Page l MAP l MAP 2 LIST F MAPS AIRBRNE MAGNETMETER DATA AIRBRNE ELECTRMAGNETIC DATA After Page 4 After Page 4
4 I. INTRDUCTIN A combined helicopter-borne electromagnetic and magnetic sur vey was performed by Aerodat Limited over a group of 4 claims within Carman township on May l, The purpose of the survey was to define possible areas of base metal and gold mineralization and as an aid to geological map ping within this part of the Archean greenstone belt. II. LCATIN AND ACCESS The survey area is located in the northwest corner of Carman township in the District of Cochrane, ntario. Figure l shows the survey location. Access to the property is possible by boat from Nighthawk Lake into the Redstone River. The claims are located south of the Redstone River about 1.6 kilometres up-stream from Nighthawk Lake. Figure 2 presents a claim location map. III. EXPLRATIN HISTRY AND GENERAL GELGY Previous Work: No work on the present Amax claims was found in the assess ment files nor was there any evidence of previous field work. The Nighthawk Lake area was mapped in by E. J. Leahy of the.d.m. (Map 2222). n this map, the Amax claims area geology is unknown. Regional Geology: The volcanic rocks of the Timmins area consist of the older Deloro Group and the younger overlying Tisdale Group.
5 Scale: l" = A miles LCATIN MAP Project CARMAN-l l" = 4 miles on of FIGURE l
6 \ J M CLAIM MAP Project CARMAN-l Carman Township l"-k mile FIGURE 2
7 2 - The Deloro Group is confined to a large domal structure centred in Shaw township. It grades from andesite and basalt flows in the lower portion to dacite and rhyolite pyroclastics near the top. A major change in volcanism marks the beginning of the Tisdale Group, the Lower Volcanic Formation of which is marked by serpentinized ultramafic flows. The Destor-Porcupine Fault is the major structural feature in the area, along with the Porcupine Syncline to the north and the Shaw Dome to the south. Property Geology: Geological surveys were performed by Amax (Lickley, 1981) in No outcrop was found in or around the claim area in this sur vey, therefore the geology of the area is not known. IV. SURVEY EQUIPMENT AND PRCEDURES Survey equipment consisted of a dual frequency Aerodat/Perle electromagnetic system operating at 940 Hz and 4250 Hz, a Barringer AM-1Q4 proton precession magnetometer, an Aerodat/Perle data acqui sition system, a Hoffman radar altimeter, a Geocam 35 mm flight path camera and a Barringer 8-channel analogue recorder. This system was installed in a Bell Jet-Ranger helicopter. The survey was flown at a line spacing of 150 metres. Survey airspeed averaged about 120 kilometres per hour and the electromagne tic sensor was maintained at an average terrain clearance of 40 metres and the magnetometer sensor at a clearance of 55 metres. Survey navigation was based on photo-mosaics at a scale of 1:15,000. Survey lines were visually navigated and fiducial points manually recorded corresponding to recognisable terrain features. Flight paths were finally verified by comparison of the 35 mm tracking film with the mosaic.
8 - 3 Personnel involved with the survey were: P. Moisson - operator/navigator D. Poole - field assistant B. Mealy - pilot B. Groves - Amax geophysicist V. DATA PRESENTATIN The airborne magnetic and electromagnetic results are presented in Maps l and 2 at a scale of 1:15,000. Recovered flight lines are shown, together with principal topo graphic features and claim boundaries. In-phase and quadrature electromagnetic readings (at the 940 Hz frequency) are plotted as profiles along each flight line, using an amplitude scale of l ppm of the primary field equal to l mm. The zero level for each trace is set using the background observed at the end of each line. The locations of significant anomalous responses are shown as a circle with the in-phase amplitude displayed in ppm and the computed apparent conductivity-thickness (et) shown by a graphic representation. For ease of comparison, the derived e-t value is divided into 10 ranges (as shown on the inset) and the range and not the actual value is indicated on the map. While high ot values are generally associated with good bedrock conductors such as graphite or massive sulphides and low values with overburden sources, anomaly amplitude, shape, persist ence and magnetic association are equally important in the subsequent evaluation of the A.E.M. anomalies. Individual zones of interest have been outlined and numbered. The interpreted axis of a conductor is indicated by a dash line. Aeromagnetic data are presented in Map l in computer contoured plan form. A nominal contour interval of 20 gammas has been employed. No filtering has been carried out on the magnetic data.
9 VI. DISCUSSIN F RESULTS Magnetic Survey: The magnetic data are dominated by a narrow, northerly trending dyke-like response which displays the greatest local magnetic relief of up to 200 nt. It is believed that this response is due to a dia base dyke. verburden depth appears to be uniform (of the order of 50 metres) across the property. The magnetic gradient associated with the diabase dyke effect ively masks more subtle magnetic expressions over the property. The relatively subdued magnetic pattern over the remainder of the property may suggest felsic volcanics or sediments. Electromagnetic Survey: Within the area of the claim group, only one conductive res ponse was recorded. The one-line (line 35) conductor is weak and poorly conductive, displaying a broad quadrature response. This broad response suggests the presence of an overburden component with in the electromagnetic data which leaves doubt as to the causative source of the response. n the basis of limited strike extent and anomaly shape, the conductor is interpreted to have an overburden source. A weak, two-line (lines 29 and 30) conductor exists in the vicinity of the northeastern claim post of the group and extends off the property to the east.
10 VII. CNCLUSINS In an area of poorly known geology, the magnetometer data have defined the presence of a northerly trending diabase dyke within sediments or felsic volcanic rocks. The one line electromagnetic response recorded during the survey is considered a doubtful bedrock conductor. A limited amount of ground geophysical surveying (magne tometer and horizontal loop electromagnetics) in the vicinity of the airborne electromagnetic response is suggested to ascertain the source of this feature. Respectfully submitted, Timmins, ntario Brian J.SJr'bve-s' November 1982 Geophysicist
11 6 - VIII. LIST F REFERENCES Lickley, P. (1981) Report on a Geological Survey, Carman-1, ; Amax Minerals Exploration Assessment Report, September 1981
12 APPENDIX A SCHEDULE F CLAIMS PRJECT Claim Group Township Number Claim Numbers Recording Date Carman-l Carman 4 P February 6, 1980 P February 6, 1980 P February 6, 1980 P February 6, 1980
13 Ministry of Nal ntario GEPHYSICAL - GEL( TECHNICAL 42A06NE CARMAN 300 T BE ATTACHED AS AN APPENDIX T TECHNICAL REPRT FACTS SHWN HERE NEED NT BE REPEATED IN REPRT TECHNICAL REPRT MUST CNTAIN INTERPRETATIN, CNCLUSINS ETC. Type of Survey(s) Airhnrne Magnetometer and Electromagnetic Township or Area Carman Township^ ^.^.^^ ^- -. Claim HnlHer(s) Amax of Canada Limited ^^^^ ^^ MINING CLAIMS TRAVERSED List numerically Survey impany Aerodat ltd..^ ^ - ^^ Author of Report Brian J. Groves ^ Address of Author 255 Algonquin Blvd.M.. Timmins. nt. P4N DD Covering Dates of Survey May l, 1981 (linecutting to office) Total Miles of Line Cut. (Prefix)...J?... (number) SPECIAL PRVISINS CREDITS REQUESTED Geophysical DAYS per claim ENTER 40 days (includes line cutting) for first survey. ENTER 20 days for each additional survey using same grid. Electromagnetic. Magnetometer - Radiometric ther. -. Geological. GeochemicaL LANDS Sfc l AIRBRNE CREDITS (Special provision credits do not apply to airborne lurveyi) Magnetometer 20 Electromagnetic 2fJ Radiometric (enter days per claim) Report or Agent Res. Geo!...Qualifications. Q. Previous Surveys File No. Type Date Claim Holder : TTAL CLAIMS. 837 (5/79)
14 GEPHYSICAL TECHNICAL DATA GRUND SURVEYS - If more than one survey, specify data for each type of survey Number of Stations Number of Readings Station interval Line spacing. Profile scale^- -^^^ ^ ^^ Contour interval. Instrument - ^. Accuracy Scale constant, W Diurnal correction method Base Station check-in interval (hours). Base Station location and value U Z S s 5 Instrument Coil configuration Coil separation - - ^^ ^^^^^^.. ^ ^. ^..^....,.. ^... Accuracy. Method: CD Fixed transmitter CD Shoot back CD In line CD Parallel line 6 W Frequency (specify V.L.F. station) W Parameters measured. b l Instrument Scale constant Corrections made. Base station value and location Elevation accuracy. Instrument. 2; Method D Time Domain D Frequency Domain Parameters - n time Frequency - ff time Range e Delay time Integration time. Q Power. Electrode array Electrode spacing. Type of electrode
15 SELF PTENTIAL Instrument. - ^^ ^.^. ^^.^.^. Range. Survey Method Corrections made. RADIMETRIC Instrument. Values measured Energy windows (levels) - - ^ - ^. -. Height of instrument - ^ ^^-...^-^. Background Count. Size of detector. ^. -. ^ -^.-...^ - verburden ^ ^^ -^^ ^ ^^. ^.^.^. (type, depth - include outcrop map) THERS (SEISMIC, DRILL WELL LGGING ETC.) ype of survey Instrument ^. - ^^ ^ Accuracy ^ ^^- ^ -^^ ^^- Parameters measured. Additional information (for understanding results). AIRBRNE SURVEYS Typenf~giirvpy(l)'~ Magnetometer and Electromagnetic Instrument(s) Mag : Barringer AM-104 Proton Precession; E.M. (specify for each type of survey) Amirary Mag ; l nt E.M. ; 2 ppm (specify for each type of survey) Aircraft mph Bell Jet-Ranger Helicopter ^ Sensor aitih.hp Mag : 55 metres E.M. ; 40 metres ^ Navigation and flight path recovery method Visual navigation based on 1:15000 photomosaics f manual fiducial recording; Flight lines verified by comparison with 35 mm r tracking film Aircraft altitude 75 metres Line Sparing 150 metres f^^^. Miles flown over total area 165 line kilometres ver claims only 3.8S line kilometres
16 GECHEMICAL SURVEY - PRCEDURE RECRD Numbers of claims from which samples taken. Total Number of Samples. Type of Sample. (Nature of Material) Average Sample Weight Method of Collection ANALYTICAL METHDS Values expressed in: per cent p. p. m. p.p. b. Cu, Pb, D D D Zn, Ni, Co, Ag, Mo, As.-(circle) Soil Horizon Sampled. Horizon Development. Sample Depth Terrain Drainage Development Estimated Range of verburden Thickness. SAMPLE PREPARATIN (Includes drying, screening, crushing, ashing) Mesh size of fraction used for analysis thers Field Analysis (- Extraction Method. Analytical Method- Reagents Used Field Laboratory Analysis No. ^ Extraction Method Analytical Method Reagents Used. Commercial Laboratory (- Name of Laboratory Extraction Method Analytical Method Reagents Used -.tests).tests).tests) GeneraL General.
17 nt Ministry of Natural [esources Type of Survey(s) Claim Holder(s) Report of Work (Geophysical, Geological, Geochemical and Expenditures) he Mining Act Airborne Magnetometer and Electromagnetic Amax of Canada Limited Survey Company Survey Dates (III Aerodat Ltd. ^, S? Name and Address of Author (of Qeo-Technlcal report) Brian Groves, 255 Algonquin Blvd. West, Timmins, Special Provisions Credits Requested Instructions Geophysical For first survey: Enter 40 days. (This Includes line cutting) - Electromagnetic - Magnetometer Days per Claim Please type or print. If number of mining claims traversej exceeds space on this form, attach a list. Note: - nly days credits calculated in the "Expenditures 1 ' section may bs entered in the "Expend. Days Cr." columns. Do not use shaded areas below. Township or Area eci rttlng to office) 1 Day Mo. Yr. ntario. P4N 2R8 Mining Claims Traversed (List in numerical sequence) Carman Township A Total Miles of line Cut For each additional survey: using the same grid: Enter 20 days (for each) Man Days Instructions Complete reverse side and enter total(s) here - Radiometric - ther Geological Geochemical Geophysical - Electromagnetic - Magnetometer - Radiometric - ther Geological Days per Claim. Airborne Credits Note: Special provisions credits do not apply to Airborne Surveys, Qeochemlcal Electromagnetic Magnetometer Redlometrlc Expenditures (excludes power stripping) Type of Work Performed Days per Claim Performed on Clnlm(n) Calculation of Expenditure Days Credits Total Expenditures S 4-15 m Total Days Credits Instructions Total Days Credits may be apportioned (t the claim holder's oholet, Enter number of days credits per claim selected In columns at right, Report Completed [ato of Report Nov. 30, 1982 Recorded Holder or Agent (Signature) ''""'"'M'l'.'iriiiojjii- / "'i; it i f. ~.., J Total number of mining claims covered by this report of work, Certification Vorlfylnci Report of Work hereby csrtlfy that 1 have a personal end intimate knowledge of the facts set forth In the Report of Work annexed rieeto, having performed the work or witnessed snmo during and/or after Its completion and the annexed report Is true, Name and Postal Address of Person Certifying Brian Groves 255 Algonquin Blvd. W., Timmins, nt. P4N 2R8 Datt Certified Certlf!ed,Wtelgna)ur uro) VJ; /J-tt-/^,.
18 Ministryof Geotechnical XL'L ""-o", omario Approval Mining Lands Comments To: Geophysics Comments Approved l l Wish to see again with corrections To: Geology - Expenditures Comments D j Approved [~ Wish to see again with corrections To: Geochemistry Comments L L Signature Approved f i Wish to see again with corrections Date Signature l [To: Mining Lands Section, Room 6462, Whitney Block. {Tel: ) 1593(81/10)
19 Mining Recorder Ministry of Natural Resources 60 Wilson Avenue Timmins, ntario P4N 2S7 Dear Sir: We have received reports and maps for an Airborne (Electromagnetic and Magnetometer) Survey submitted on Mining Claims P et al In the Township of Carman. This material will be examined and assessed and a statement of assessment work credits will be Issued. Yours very truly E.F. Anderson Director Land Management Branch Whitney Block, Room 6450 Queen's Park Toronto, ntario M7A 1W3 Phone: 416/ DU: se cc: Amex of Caaada Limited Timmins, ntario Attn: Brian Grove.
20 December 7, 1982 MINERALS EXPLRATIN (A Division of AMAX F CANADA LIMITED) 255 Algonquin Blvd. West Timmins, ntario P4N 2R8 Telephone: (705) ur File RECEIVED ir D j ^ Mr. F. W. Matthews, ntario Ministry of Natural Resources, W1617, Whitney Block, Queen's Park, TRNT, ntario. M7A 1W3 DEC l". E. ANDERSN J. R.I/IRTN G. SMKKMAN Dear Sir: Re: Mining Claims P et Carman Township J. M. f; tt At.;. T K', Please find enclosed herewith two (2) copies of a report and plans concerning an airborne electromagnetic and magnetometer survey which was carried out over the below listed four (4) mining claims located in Carman township. P P P P A Report of Work concerning this survey has been filed with Mr. William Good, Mining Recorder for the Porcupine Mining Division. Thank you. Yours truly, AMAX F CANADA LIMITED Qov tsr Rosemary Tntley (Mrs.) Land Recorder Encs. c.c. K. Clemiss/E. Barclay, Toronto W. Good, Mining Recorder, Porcupine Mining Division
21 3 W o fi) H) 3 G D 0) o ^m ^ D I- > SHAW TWP. " * S J Q. s s o o w -i M s * o a W X o. -i A -t. a.. o y -t A *" r -n o zr 'l 1 V I J - "H f ~n? "^ o A J rt 2 o o 3 o - f o? '~ ^ * - A " 3 a (D 3 c o. ; - ^15 (D - ^ c A o c 5" ^ * ^ TJ o o o ra w CD ~ ^ c ^ "" -1" i i -: l T, n s o * 3! ^ l z i ^ c? W* -^ 3 L. B ^.'-- i T - 3 *- sa g ^s- m? * o " 3 o 3J i W -e 71 3) J " -* r o T 4- ± f n l Z} o a -o? A > TJ (/l K 2 D o -c /--4-- ~. T~ ~~ L.f -~"~nt~ -Z"r 7*' *~ -_t-- -'4_-1-4 \ -D. 2 -D T o* ^T * " m l i r -l l 4- ' THMAS TWP. l o C z m ) {D - w ^ d. h W 05 w Branch Managemen ~0 and 0 = 05-1 m m W ^ ^ ^ x o o-"n f ^* C CH m W o o o > T, -0 -v*'* "' T C o" > -5.2 g m > " 0 o 0 I X H SPS 3D 00 z " J j) C ^ ^ m p m m ~^ 3) m ^ m H 0 0 m r C/) m m en X -t m o m
22 ^ x T Q r- '"' vt -i r -f K Q. C r*
23 LEGEND W~ Claim Boundary Magnetic intensity contours Township Boundary Flight Line and fiducial 4SA06NE CARMAN 210 MA P l ~ MAGNETMETER DATA MAP AM AX MINERALS EXPLRATIN Scale 1:15,000 Veluro Project'
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