l l l l l l l for MAR 1 6 MAMNG AERODAT LIMITED December, 1983

Transcription

1 RPRT N MIN LIPTR-RN MGNTI N LTRMGNTI SURVY GRLTN, NTRI.655 LTR g fr LLR IN, RT LIMIT eceber, 98 MR 6 MMNG

2 {Scae: LIST F MPS :,) Maps. Interpretatin Map. irbrne ectragnetic Survey Prfies (95 z (axia). Tta Fied Magnetic Map. Tta Fied VLF-M s prvided but nt incuded with the reprt 5. tw-cur aster veray f the cpanar (7 z) and caxia (57 z)respnse prfies.

3 , i. INTRUTIN. SURVY R Ii (I NM5e.655 LTR TL F IRRFT, QUIPMNT N PRSNNL. ircraft. quipent.. ectragnetic Syste.. VLF-M Syste.. Magneteter.. Magnetic ase Statin..5 Radar tieter..6 Tracking aera..7 nag Recrder..8 igita Recrder. Persnne. T PRSNTTIN. ase Map and Fight Path. ectragnetic Prfie Maps. Magnetic ntur Maps. VLF-M ntur Maps 5. INTRPRTTIN 6. RMMNTINS PPNIX I - Genera Interpretive nsideratins PPNIX II - nay List Page N

4 LIST F MPS - (Scae: /,) Map irbrne ectragnetic Survey I nterpretatin Map I Map ectragnetic Prfie Map (95 z caxia cnfiguratin) Map Tta Fied Magnetic Map Map VLF-M Tta Fied nturs Map prvided but nt incuded in reprt; - aster ap ( cur) f caxia and cpanar prfies with fight path

5 . INTRUTIN This reprt describes an airbrne gephysica survey c arried ut n behaf f care Resurces Inc. by erdat Liited. quipent perated incuded a - frequency eectragnetic syste, a VLF-M syste and a agneteter. The survey area near Geradtn, ntari was fwn n eceber 8th and 9th, 98 fr an peratins base at Geradtn. tta f ine k { ine ies) were M fwn, at a nina ine spacing f eters. f this tta quantity, 7 ine k (9 ine ies) fe within the cai bcks.

6 -. SURVY R The survey cnsisted f three areas,, and, which are utined bew. The fight ine directin was nrth/suth at a nina ine spacing f eters. e5' 87 ' i;.,;, t JK

7 M. IRRFT, QUIPMNT N PRSNNL. ircraft The heicpter used fr the survey was an erspatiae star 5 wned and perated by Mape Leaf eicpters. Instaatin f the gephysica and anciary equipent was carried ut by erdat at Geradtn. The heicpter. quipent was perated at a ean terrain cearance f 6 eters... ectragnetic Syste The eectragnetic syste was an erdat/ Genics frequency syste. Tw vertica caxia ci pairs were perated at 95 and 57 z and a hriznta cpanar ci pair at 7 z. The transitter-receiver separ- atin was 7 eters. In-phase and quadrature j signas were easured siutaneusy fr the frequencies with a tie-cnstant f. secnds. The eectragnetic bird was twed eters bew the heicpter.

8 .. VLF-M Syste - The VLF-M Syste was a erz. This i nstruent easures the tta fied and vertica quadrature cpnent f the signa fr N (uter, Maine, 7.8 kz). The sensr was twed in a bird 5 eters bew the heicpter... Magneteter The agneteter was a Geetrics G-8 prtn precessin type. The sensitivity f the instruent was gaa at a.5 secnd sape 8 rate. The sensr was twed in a bird 5 eters bew the heicpter... Magnetic ase Statin n IFG prtn precessin type agneteter was perated at the base f peratins t recrd diurna variatins f the earth's agnetic fied. The cck f the base statin was synchrnized with that f the airbrne syste t faciitate ater crreatin...5 Radar tieter ffan R- radar atieter was used t recrd terrain cearance. The utput fr the

9 - instruent is a inear functin f atitude fr axiu accuracy...6 Tracking aera Geca tracking caera was used t recrd " fight path n 5 fi. The caera was perated in frae de and the fiducia nubers fr crss-reference t" the anag and digita g data were iprinted n the argin f the fi...7 nag Recrder J RMS dt-atrix recrder was used t dispay the data during the survey. In additin t anua and tie fiducias, the fwing data was recrded: hanne Input Scae 7 atieter (5 ft. at ft. / tp f chart) high freq. quadrature pp/ high freq. in-phase pp/ 5 id freq. quadrature pp/ id freq. in-phase pp/ w freq. quadrature pp/ w freq. in-phase pp/

10 hanne Input Scae agneteter 5 gaa/ M agneteter.5 gaa/ 8 VLF-M Tta Fied.5%/ J 9 VLF-M Quadrature.5%/..8 igita Recrder f Sntek SS data syste recrded the survey data n agnetic tape. Infratin recrded was as fws: quipent M VLF-M agneteter atieter fiducia (tie) fiducia (anua). Persnne Interva. secnd.5 secnd.5 secnd. secnd. secnd. secnd Persnne directy invved with the survey peratin were as fws: Pit: Rger Mrrw quipent peratr/technician: Mike ndin

11 ' T PRSNTTIN. ase Map and Fight Path Pht ap bases at /, scae were prepared by enargeent f aeria phtgraphs f the areas. They were used during the curse f the survey fr * visua navigatin as we as fr fina fight path recvery and ap presentatin. p. ectragnetic Prfie Maps The eectragnetic data was recrded digitay at a high sape rate f /secnd with a sa tie cnstant f. secnd. tw stage digita fiter- M ing prcess was carried ut t reject ajr sferic events, and t reduce syste nise. Lca sferic activity can prduce sharp, arge apitude events that cannt be reved by cnven tina fitering prcedures. Sthing r stacking wi reduce their apitude but eave a brader M residua respnse that can be cnfused with a gegica phenenn. T avid this pssibiity, a cputer agrith searches ut and rejects the ajr sferic events. The signa t nise rati was further enhanced by the appicatin f a w pass digita fiter. It

12 - j has zer phase shift which prevents any ag r peak dispaceent fr ccurring, and it suppresses ny variatins with a waveength ess than abut.5 g secnds. This w effective tie cnstant perits axiu prfie shape resutin. Fwing the fitering prcesses, a base eve crrectin was ade. The crrectin appied is a j I inear functin f tie that ensures that the crrected apitude f the varius in-phase and quadrature cpnents is zer when n cnductive r pereabe surce is present. - The fitered and eveed data were then presented in prfie ap fr. I The in-phase and quadrature respnses f the caxia 57 z and the cpanar 7 z cnfiguratin were ptted with fight path and presented as a tw cur veray. The in-phase and quad- rature respnses f the caxia 95 z cnfigur- atin were ptted with eectragnetic anay infratin.

13 -. Magnetic ntur Maps The aeragnetic data was crrected fr diurna variatins by subtractin f the digitay recrded base statin agnetic prfie. N crrectin fr regina variatin was appied.. The crrected prfie data was interpated nt a reguar grid at a.5 interva using a cubic spine technique. The grid prvided the basis fr threading the presented cnturs at a gaa g interva. The aeragnetic data was presented with eectr agnetic anay infratin.. VLF-M ntur Maps The VLF-M signa fr N, uter, Maine was cpied in ap fr. The ean respnse eve f the tta fied signa was reved and the data was gridded and cntured at an interva f %. M The VLF-M data was presented with eectragnetic anay infratin.

14 5-5. INTRPRTTIN The eectragnetic prfie aps were anaysed t identify thse respnses typica f bedrck cnductrs. s discussed in ppendix I, the prfie shape can indicate the genera geetry f the cnductive surce. naies that exhibited the characteristics f a hriznta cnducting ayer were attributed t cnductive verburden. Thse with character- j I cnductive verburden surce the cnductr axis was indie g istics f a thin, steepy dipping sheet were interpreted t be f bedrck rigin. Where the respnse shape was insuff- incienty diagnstic t rue ut the pssibiity f a ated as a pssibe bedrck cnductr. The prcess f cnductr identificatin ephasized prfie shape rather than the estiated cnductance. wever, this paraeter was cacuated by appicatin f the high frequency caxia in-phase and quadrature respnse t the phasr diagra fr the vertica haf-pane de. This was carried ut by g cputer and the resuts are tabuated in ppendix II and presented n the interpretatin ap in sybized fr. The estiated cnductance is a easure f the cnductive prperties f the surce. w cnductance f say, hs r ess is indicative f eectrytic cnductin in fauts r shears r pssibe inr disseinated ineraizatin.

15 5- M igher cnductances generay indicate that a significant fractin f the eectrica cnductin ay be due t suphide r graphite ineraizatin. eve f hs r greater is a very psitive indicatin f such ineraizatin. stiated cnductance can be a usefu paraeter in the identificatin f base eta targets; hwever, in the case f gd expratin it is f iited significance.

16 rea 5- The ntari epartent f Mines Gegica Map indicates that the suthern and eastern part f the area cnsists f etasedientary rcks. T the nrth and nrthwest bth etavcanics and basic t utrabasic igneus rcks are apped. This descriptin is generay cpatibe with the aeragnetic data. th the eta g rphsed and igneus vcanic rcks are expected t have assciated agnetic anaies and a distinctin between the tw rigins n the basis f the aeragnetics is nt bvius. Many cnductive axes have been interpreted, st f which g are csey assciated with the vcanic rcks. nductance eves, particuary at catins indicated as,,, and 5 are sufficienty high t suggest significant suphide r graphite ineraizatin. Severa pssibe bedrck cnductrs f w cnductance are indicated in the suthern part f the area. Thse at catins 6 and 7 are fet st ikey t be f bedrck rigin and due t inr suphide r graphite ineraizatin r eectrytic effects in a faut r shear zne.

17 5- rea The ntari epartent f Mines Gegica Map indicates that the survey area ay be argey f etasedientary rigin. n irn fratin is nted in Partridge Lake. The aeragnetic ap generay supprts j this descriptin. reativey quiet backgrund with the intense agnetic anay extending ang the ake typica f an irn fratin. nuber f anaies f ptentia bedrck rigin have been identified by the survey. Thse extending ang the ake in assciatin with r in prxiity t the irn fratin are ikey due t suphide r graphite ineraizatin. The anaies nted as, and fa utside this centra zne and ay be f different rigin r nature. The strike interpreted fr axis is in cntrast t the genera trend f the area athugh it is rughy aigned with a perturb- j atin in the irn fratin that ay be indicative f a faut.

18 I rea 5-5 The ntari epartent f Mines Gegica Map indicates that st f this area ay be cvered by rcks f etasedientary rigin. crss the suthern part f the area a band f etavcanic rcks is indicated. The aeragnetic ap is cpatibe with this descriptin: the higher apitude agnetic znes crrespnding with the etavcanic rcks. Within this suthern zne are nuerus cnductrs with cnductance eves ften abve hs and suphide r. graphite ineraizatin is expected. T the nrth are severa axes f w cnductance but with attributes characteristic f bedrck rigin. The surce j f the anaies ay be inr suphide r graphite ineraizatin r sipy eectrytic effects within a faut r shear zne. s indicated axes, and are beieved st ikey t be f bedrck rigin. The rigin f the ther axes is nt certain but st ikey due t cnductive verburden. The nuerus respnses ver ter Lake with n axes interpreted are interpreted as due t cnductive ake btt sedients.

19 j 6-6. RMMNTINS Nuerus cnductr axes f interpreted bedrck rigin have been identified by the survey. f these any have cnductance eves that are nray indicative f suphide r graphite ineraizatin. Thse anaies with higher cnductance, categry r ay deserve fw-up as base eta prspects if the ca gegy is deeed favurabe. Gd ineraizatin, disseinated in the rck, cannt be expected t prduce a easureabe eectragnetic anay. The assciated gegica fratin ay bece easureaby cnductive due t accessry suphide r graphite inera izatin r even eectrytic cnductin within fauts r shears. The interpreted bedrck cnductr axes indicate znes ptentiay favurabe t gd ineraizatin and deserve " f fw-up investigatin. Thse st faiiar with the detaied gegy f the area can best evauate the ptentia significance f the cnductrs and agnetic features and assign reative fw-up pririty. Respectfuy subitted, RT LIMIT February, 98 R. L. Sctt g^,

20 PPNIX I GNRL INTRPRTIV NSIRTINS ectragnetic The erdat frequency syste utiizes different transitter-receiver ci geetries. The traditina caxia ci cnfiguratin is perated at widey separated frequencies and the hriznta cpanar ci pair is perated at a frequency apprxiatey aigned with ne f the caxia frequencies. The eectragnetic respnse easured by the heicpter syste is a functin f the "eectrica" and "geetrica" p prperties f the cnductr. The "eectrica" prperty f a cnductr is deterined argey by its cnductivity and its size and shape; the "geetrica" prperty f the respnse is argey a functin f the cnductrs shape and rientatin with respect t the easuring transitter and receiver. ectrica nsideratins Fr a given cnductive bdy the easure f its cnductivity r cnductance is csey reated t the easured phase shift between the received and transitted eectragnetic M fied. sa phase shift indicates a reativey high cnductance, a arge phase shift wer cnductance. sa phase shift resuts in a arge in-phase t quadrature

21 Q - - PPNIX I rati and a arge phase shift a w rati. This reatin- I ship is shwn quantitativey fr a vertica haf-pane de n the accpanying phasr diagra. ther physica des wi shw the sae trend but different quantitative reatinships. The phasr diagra fr the vertica haf-pane de, as presented, is fr the caxia ci cnfiguratin with the apitudes in pp as easured at the respnse peak ver the cnductr. T assist the interpretatin f the survey resuts the cputer is used t identify the apparent cnductance and depth at seected anaies. The resuts f this cacuatin are presented in tabe fr in ppendix II and the cnductance and in-phase apitude are presented in sybized fr n the ap presentatin. The cnductance and depth vaues as presented are crrect ny as far as the de apprxiates the rea gegica M ' situatin. The actua gegica surce ay be f iited ength, have significant dip, its cnductivity and thickness ay vary with depth and/r strike and adjacent bdies and verburden ay have dified the respnse. In genera the cnductance estiate is ess affected by these iitatins than is the depth estiate, but bth shud be cnsidered as reative rather than absute guides t the anay's prperties.

22 - - PPNIX I nductance in hs is the reciprca f resistance in M hs and in the case f narrw sab-ike bdies is the prduct f eectrica cnductivity and thickness. Mst verburden wi have an indicated cnductance f ess than hs; hwever, re cnductive cays ay have an apparent cnductance f say t hs. s in the w cnductance range wi be eectrytic cnductrs in fauts and shears. The higher ranges f cnductance, greater than hs, indicate that a significant fractin f the eectrica cnductin is eectrnic rather than eectrytic in nature. Materias that cnduct eectrnicay are iited t certain etaic suphides and t graphite. igh cnductance anaies, rughy hs r greater, are generay iited t suphide r graphite bearing rcks. Suphide ineras with the exceptin f sphaerite, cinnabar - and stibnite are gd cnductrs; hwever, they ay ccur in a disseinated anner that inhibits eectrica cnductin thrugh the rck ass. In this case the apparent cnductance can seriusy underrate the quaity f the cnductr in J gegica ters. In a siiar sense the reativey nn- cnducting suphide ineras nted abve ay be present in significant cncentratin in assciatin with inr cnductive

23 ' - - PPNIX I suphides, and the eectragnetic respnse ny reate t is f it t the inr assciated ineraizatin. Indicated cnductance as f itte direct significance fr the identificatin gd ineraizatin. thugh gd is highy cnductive wud nt be expected t exist in sufficient quantity create a recgnizabe anay, but inr accessry suphide ineraizatin cud prvide a usefu indirect indicatin. - In suary, the estiated cnductance f a cnductr can prvide a reativey psitive identificatin f significant suphide r graphite ineraizatin; hwever, a derate t f w cnductance vaue des nt rue ut the pssibiity significant ecnic ineraizatin. Geetrica nsideratins Geetrica infratin abut the gegic cnductr can ften be interpreted fr the prfie shape f the anay. The change in shape is priariy reated t the change in inductive cuping ang the transitter, the target, and the In the the receiver. the case f a thin, steepy dipping, sheet-ike cnductr, caxia ci pair wi yied a near syetric peak ver cnductr. n the ther hand the cpanar ci pair wi pass thrugh a nu cupe reatinship and yied a iniu ver the cnductr, fanked by psitive side bes. s the dip f the cnductr decreases fr vertica, the caxia

24 - 5 - PPNIX I anay shape changes ny sighty, but in the case f the cpanar ci pair the side be n the dwn dip side strengthens reative t that n the up dip side. g s the thickness f the cnductr increases, induced current fw acrss the thickness f the cnductr beces reativey significant and cpete nu cuping with the cpanar cis is n nger pssibe. s a resut, the apparent iniu f the cpanar respnse ver the cnductr diinishes with increasing thickness, and in the iiting. case f a fuy diensina bdy r a hriznta ayer r haf-space, the iniu disappears cpetey. M hriznta cnducting ayer such as verburden wi prduce a respnse in the caxia and cpanar cis that is a functin f atitude (and cnductivity if nt unifr). The prfie shape wi be siiar in bth ci cnfiguratins with an apitude rati (cpanar/caxia) f abut /*. In the case f a spherica cnductr, the induced currents are cnfined t the vue f the sphere, but nt reativey restricted t any arbitrary pane as in the case f a sheetike fr. The respnse f the cpanar ci pair directy ver the sphere ay be up t 8* ties greater than that f the caxia ci pair.

25 - 6 - PPNIX I In suary, a steepy dipping, sheet-ike cnductr wi dispay a decrease in the cpanar respnse cincident with the peak f the caxia respnse. The reative strength f this cpanar nu is reated inversey t the thickness f the cnductr; a'prnunced nu indicates a reativey thin cnductr. The dip f such a cnductr c an be inferred fr the reative apitudes f the side-bes, f Massive cnductrs that cud be apprxiated by a cnducting sphere wi dispay a sipe singe peak prfie fr n bth caxia and cpanar cis, with a rati between the cpanar t caxia respnse apitudes as high as 8.* verburden anaies ften prduce brad pry defined anay prfies. In st cases the respnse f the cpanar cis csey fws that f the caxia cis with a reative apitude rati f.* ccasinay if the edge f an verburden zne is sharpy - defined with se significant depth extent, an edge effect wi ccur in the caxia cis. In the case f a hriznta cnductive ring r ribbn, the caxia respnse wi cnsist f tw peaks, ne ver each edge; whereas the cpanar ci g wi yied a singe peak.

26 - 7 - PPNIX I *It shud be nted at this pint that erdat's definitin f the easured pp unit is reated t the priary fied sensed in the receiving ci withut nraizatin t the axiu cuped (caxia cnfiguratin). If such nraizatin were appied t the erdat units, the apitude f the cpanar ci pair wud be haved.

27 8 - PPNIX Magnetics The Tta Fied Magnetic Map shws cnturs f the tta agnetic fied, uncrrected fr regina varia tin. Whether an M anay with a agnetic crre- I atin is re ikey t be caused by a suphide depsit than ne withut depends n the type f ineraizatin. n apparent cincidence between an M and a agnetic anay ay be caused by a cnductr which is as agnetic, r by a cnductr which ies in cse prxiity t a agnetic bdy. The ajrity f cnductrs which are as agnetic are suphides cntaining pyrrhtite and/r agnetite. nductive j and agnetic bdies in cse assciatin can be, and ften are, graphite and agnetite. It is ften very difficut t distinguish between these cases. If the cnductr is as agnetic, it wi usuay prduce an M anay whse genera pattern resebes ' that f the agnetics. epending n the agnetic pereabiity f the cnducting bdy, the apitude f the inphase M anay wi be weakened, and if the cnductivity is as weak, the inphase M anay ay even be reversed in sign.

28 VLF ectragnetics PPNIX I The VLF-M ethd epys the radiatin fr pwerfu iitary radi transitters as the priary signas. * The agnetic fied assciated with the priary fied is eipticay parized in the vicinity f eectrica cnductrs. The erz Tte uses three cis in the X, Y, Z cnfiguratin t easure the tta fied and vertica quadrature cpnent f the parizatin eipse. The reativey high frequency f VLF 5-5 kz prvides M high respnse factrs fr bdies f w cnductance. Reativey "discnnected" suphide res have been fund t prduce easurabe VLF signas. Fr the sae reasn, pr cnductrs such as sheared cntacts, breccia znes, narrw fauts, ateratin znes and prus fw tps M nray prduce VLF anaies. The ethd can therefre be used effectivey fr gegica apping. The ny reative disadvantage f the ethd ies in its sensitivity t cnductive verburden. In cnductive grund the depth f expratin is severey iited. The effect f strike directin is iprtant in the sense f the reatin f the cnductr axis reative t the energizing eectragnetic fied. cnductr aigned f ang a radius drawn fr a transitting statin wi be

29 - - PPNIX I in a axiu cuped rientatin and thereby prduce a strnger respnse than a siiar cnductr at a different strike ange. Thereticay it wud be pssibe fr a cnductr, riented tangentiay t the transitter t " prduce n signa. The st bvius effect f the strike J ange cnsideratin is that cnductrs favuraby riented with respect t the transitter catin and as near perpendicuar t the fight directin are st ceary rendered and usuay dinate the ap presentatin. The tta fied respnse is an indicatr f the existence and psitin f a cnductivity anay. The respnse wi be a axiu ver the cnductr, withut any specia fitering, and strngy favur the upper edge f the cnductr even in the case f a reativey shaw dip. j The vertica quadrature cpnent ver steepy dipping sheet ike cnductr wi be a crss-ver type respnse with the g crss-ver csey assciated with the upper edge f the ' cnductr. The respnse is a crss-ver type due t the fact that it i s the vertica rather than tta fied quadrature cpnent that is easured. The respnse shape is due argey t geetrica rather than cnductivity cnsideratins and the distance between the axiu and iniu n either side f the crss-ver is reated t target depth. Fr a given target geetry, the arger this distance the greater the

30 - - PPNIX I depth. f The apitude f the quadrature respnse, as ppsed t shape is functin f target cnductance and depth f as we as the cnductivity f the verburden and hst rck. s the priary fied traves dwn t the cnductr thrugh cnductive ateria it is bth attenuated and j phase shifted in a negative sense. The secndary fied prduced by this atered fied at the target as has an g assciated phase shift. This phase shift is psitive and is arger fr reativey pr cnductrs. This secndary ~ fied is attenuated and phase shifted in a negative sense during return trave t the surface. The net effect f these phase shifts deterine the phase f the secndary fied sensed at the receiver. reativey pr cnductr in resistive grund wi yied a net psitive phase shift. reativey gd cnductr in re cnductive grund wi yied a net negative phase shift. cbinatin is pssibe whereby the net phase shift is zer and the respnse is purey in-phase with n quadrature cpnent. net psitive phase shift cbined with the geetrica crss-ver shape wi ead t a psitive quadrature respnse n the side f apprach and a negative n the side f M departure. net negative phase shift wud prduce the reverse. further sign reversa ccurs with a 8 degree

31 - - PPNIX I change in instruent rientatin as ccurs n reciprca ine headings. uring digita prcessing f the quad- I rature data fr ap presentatin this is crrected fr by nraizing the sign t ne f the fight ine headings

32 PPNIX II NMLY LIST

33 9 FLIGT L INF NMLY TGRY L.LR Rt FRQUNY 57 INPS QU, Pftt NUTR IR TP PT IGT MS MTRS TRS ,, 6,9,9 6,,,6, P n h c, 7. 8,,.,8 7,6 8,,6, 7,7 9,,,5 7,6,7,8 9,9 6, 9,8.6.6,5,,6,,,6,, n,,7, 5, 9,6,, 7,7,5,, P r 7,,7 9, 9,9,9 6,6 -, 7,6 7.,, 8,,,,6,, 9,5 Q,.,,,,.,*, F G ,,,5 9,, ,6, 9, 8,,6.,,,,,, ' 5,,6 7,7 8,, 9,,5,9,6 5 stiated der-th nigy be unreiabe because the strnger f the cnd'jctr ay be deerpr r t ne side f the fight inei r becuse f s s haw cip r verburden effects,

34 I 9 : LIGT LIN NMLY LLR R* r nut NUTR FRQUNY 57 TP PT TGRY INPS QU, MS MTRS t. IR IGT MTRS,9,6.9,7,, 5?7 8,8, 6,7,,5,7,,,,,8, , 8,,9, ,,, 7,5. 8,5,,,8,8,,9,, ,7 6,6,9, 6, 9,6 8, 5,,8,,, ,. 8,5,,9 7,6,, , 5,8.7,7 8,5 6,8,6, 6,5 8.,, P,,.6..6,,. 9. 7,., 8.7.5, ,8,5,,6 58,,,,8, ,9,. stiated der-th as; be unreiabe because the strnger part f the cnductr ay be deeper r t ne side f the fi i ah t i ne i r because nf e shaw dip r verburden effect s,

35 LLR Rf PG NUTR FRQUNY 57 GTP PT FLIGT LIN NMLY TGRY INPS QU, MS TRS 7,9,6,7, 5,, 6,,,,6,9, IR IGT MTR FI F 5,9 6,,9 7,6 5,5,9, 6,,8 5,5 7, 6, 7,,7,8,,5,, 6,,9, 7,7 5, 8, 5,7,7.,,,5,,,,,.,8.7,9,, ,6 8,8,,8 5.7, 7, 5,7,,,., ,7, -,,8 7, 5,,, 5, 8,9,,6,,, F G -. 7, 8,,8 6, -,.,7,6,6 6, 5, 58,,8,5,, 5,5 7,.,,,5,7,,,,,, st j eted d P P- t h s y be f the cnductr a.; be ine? r because f unreiabe deeper r ihaw dip becsusp the t ne side f r verburden pert the fight effects, strnger

36 FLIGT LLR RI FRQUNY 57 LIN NMLY TGRY IPS QU, r F G P F F : F G J i F G J ") i.- 9,8 5,.,, 6,5,5 5,, -, -,, 6., 5,5, , 6,,.5,,, 5.9 5,9,, 8.9, 5, 5,8,,,5,9 7,9 7,,, ,8,7 8,, 5,,8 69., ,8,8 5,5.7, 6..7, , ,5 5, 5,, 8,, 6, PG NUTR IR TP PT IGT MS MTRS MTRS,,6, ,,, ,6 7, ,,, ,7.7. dpm,h us y he unreisbe because the strnger F-srt f the cnductr sy be deeper r t ne side f the fight ine* r because nf s ^httw dip r verburden effects,

37 PG FLIGT LLR Rt FRQUNY 57 L INF NMLY TGRY INPS QU, K It F G F G [i F G J i F G J K M P -,, 9,9, 6,6,8 9,,.9 7,7 8,8 9,6 68,8,,, -,8 -,6,,7,7, 8,5,5 57,6 9,5 6, ,9. 6,8 5,, 7, 7,,, 5,6, 5, 9,,6 5,9 6, 6,6 5, ,6,8 6,7 6,7, 7.8,.9,5,,7,5,7.8, 56, 6,8, 67, 5, 9, 5,9,7 7,9 8,6 7, ,6 NUTR IR TP PT IGT MS TRS MTRS,,,9,.8,8,7,5.5,5,9,.5,5.,-,.,,,7 5,,.,8.9,5,,8,,5,9,,9,,8,6,,,, derth niey b e u nreiabe beceuse the strnger pert f the cnductr ay be deeper r t ne side f the fight iner r because f? shaw dip r verburden effects, I

38 FLIGT LIN NMLY TGRY T. 5 n F G J F G i F G : Ḡ F G L.LR Rt FRQUNY 57 INPS QU , 9, 8, 5, -,,5 7,.. 7,9,9,,,6, 7,,6,5 -, -, -,,,8 9, 5,6,,,,6 5,9,,5 -, -,8 -,9,6,, ,5 6. 9, 8,8,,8 6,,5 7,9,7, , ,6,7 6,,,.9,8 PG NUTR IR TP PT IGT MS MTRS TRS,,,9,5,,,..9,,,,,, ,,..,,7,,,,,,,8,,,,.r,, stiated depth ay be unreiabe because the strnger part f the cnductr ay he deeper r t ne side f the fight ine? r because f a shaw dip r verburden effects

39 ^^F- FLIGT p?. LIN NMLY IS' S n f G J P r G P t: F F n TGRY LLR Rt FRQUNY INPS,6 8, -.7 -,6 --, -,. -,5 -, 6,8., , rj,9,7, 7,7,7,,,..6 6, ,,9 8, -,,9 5,5 6,8,7 57 QUIU 7, 7,., 9,6,, 9,5 5,,6 9, 6,8, 8, 5, 7* 7, 6,7,5, 5, 8,9 9,,5,8 7,,,5 5,7 8,5 7, 5,9 9, , 5, PG; NUUTR IR GTP PT IGT MS MTRS MTRS,,5.,,,,,,,,,9,,,,7,,,,.7*,9,8,..,,9,5,7,,.5,.,,9,.7 F stitnsted depth IPW bf unreiabe because the strnger part f the cnductr py be dppper r t ne side f the fight ine? r because f?;hw dip r verburden effects,

40 . LR Ri PG 8 NUTR IR FRQUNY 57 TP PT IGT FLIGT LIN NMLY TGRY INP8 RUU MS MTRS MTRS 'i t*. i / j 7 *- T * r F G : F G F,8,8,5,7,5,9,,,,,,,,5,9,5, 7, 5,,,5,9, 5, 5, 5, 6,7.9.5,,5 6,,.8,,,,,,,,6,,,,..., n 6,7 5,5,9 6, 7,, , 9,.,.6,7.7, stiated depth niey be unreiabe because the strnger par t f the cnductr ey be deeper r t ne side f the fight iner r because f shaw dii* r verburden effects,

41 LLR RI PG ^ NUTR IR FRQUNY 57 TP PT IGT FLIGT LIN NMLY TGRY INPS QU, MS TRS MTRS.8,, 7.,7, ii i i i i i i i i i i i i i i F G F G,, 6,, 5,,7,6,9 5,8,, 8. 6, 9,,5 7,8,8, ,5 6,9 7,6,,, 6, , 5,7 9,5,9 5,5 6,6 5,5 8,8 9,.7.5 6,5 8,9 5, 7. 9,6 9.6, 7, ,,,,,,,,,,,,,,,,,.....i;.i-,,.,,,,,,, stiated def-th rsy be f the cnductr sy i ne j r because f be un re i ab e deeper r shsu dip because the strnger pert t ne side f the fi S h t r verburden effects f

42 LLR RI -'fut ^ NUTR FRQUNY 57 TP PT FLIGT LIN NMLY TGRY INPS QU, S TRS i ii ,,, 9, 7,6,, 8,6 5, 7.5 9,,6.,5,5,, 8., 9, , 8, -, -,6 -,7, ,7., , 7, 5.6.5,.5, , ,. 9,9.,.9,..6, stiated depth ay be unreiabe because the strnger part f the cnductr ay be deeper r t ne side f the fi isht ine? r because f shaw dip r verburden effects. 8,6...,.,,,,,,,5,.6,.,8,.,,,...,.,.,...,... (. 7 IR IGT MTRS

43 LLR RI PG ^ NUTR IR FRQUNY 57 TP PT IGT FLIGT LIN NMLY TGRY INPS QU. MS MTRS MTRS ,6, 7,6,,5, , ,..,,5, 9.5 7, ,5,5,, ,7 9,7 6,..., ,9 9,8 8,7,9, 7,8 6, 9,9 8,6 7,8.5,.,, 8 6 i ii ,, ,6 7,9,,6 5,5,9 8, 7,6,,,,,8,,, 9 5 i i i ,6 8,9 9,,,, 8 5 v, i , , 7,,,9.,5,,,, * 8 stiated depth ay be unreiabe because the strnger part f the cnductr ay be deeper r t ne side f the fi issht ine* r because f shaw dip r verburden effects.

44 J! LLR RI FRQUNY FLIGT LIN NMLY TGRY INPS 7 P 8*9 7, 6 9,9 6 P,6 6 6, 5,8 5 9,5 7, 7,,8, 6, 7, 5,,7 PG NUTR 57 TP PT QU, MS MTRS 6,7,,, 5,7,,,8,,,,,7, 8,,,, 7,9, 9,,,6,,6,,9 8,,, stiated depth ay be unreiabe be cause the strnger part f the cnductr ay be deeper r t ne side f the fi iaht ine* r because f a shaw dip r verburden effect s, IR IGT MTRS hi-

45 LLR R* PG NUTR IR FRQUNY 57 TP PT IGT FLIGT LIN NMLY TGRY INPS QU. MS MTRS MTRS F.9.,9 8. 5,,9 -, 8, ,,... 7 i F G J 8.6 6,8 6., , 6,,8.6,,. 7. 5, ,8 69,9.,5,8,,,* i i P F G F G J n F G stiated depth ay be f the cnductr ay ine? r because f be. 8.5, ,5 7. 8, ,,5,,8 5,.6, , 5, -,7,. unreiabe deeper r shaw dip 6, 59, ,. 6, 7, , 5,, ,, , ,,,,.,6,6.7.5.,,9,.,, ,9.,,, because the t ne side f r verburden strnger part the fight effects,

46 FLIGT i LLR RI FRQUNY 57 LIN NMLY TGRY INPS QU, n F G F G F G,,,7 5,7,,9 6,,8 7,7,9 5, 5, 7,., 6,5,8 5,8. 6,5 8,7,9, 5,5 57,,,9,9,.9,5,,5 5,.9.5,7,7, 6,, 6,7 6,9,8,9,9,9 7,,5.8, 9, ,8 7, 6,,,,6,,9,,,7 8,, 6,6 6,, 8,9 7, 6,5 PG NUTR IR TP PT IGT MS MTRS MTRS,,,,5,,,,7...,,.,,, 8,8.7,.6,7,6, 6,8,,,7,5,8.,7, 8,6.,, 6,,8 stiated depth ay be unreisbe because the strnger part f the cnductr uiey be deeper r t ne side f the fisht ine) r because f shaw dip r verburden effects

47 LLR R* PG W NUTR FRQUNY 57 GTP PT FLIGT LIN NMLY TGRY INPS QU, MS TRS i - i F G F G F G P F G F G 8,, 9,5, 8,,,7 5.,,,,, 5,5,7 8,5,9 8, 8,8,. 5,, -,6,5,.6,5, 8, 6,8 8,5,9,5,6,7,,5 7,5 7,5 7,6 6, 8,5 9,5 9,8 7,8 6,,7,7, ,5 5, 9, 5,8 6,5,.5 5, 7,8..7,,6.6,.9,,5,9,,..,6,6,,,,.9.,9,..,,.9,5,9,, IR IGT MTRS , 6,9 8,7,7, 5,5,,8 8,.5 7,8 5,5 5,,6,,,7, 5,8,, Z.7, stiated depth ay be unreiabe because the strnger part f the cnductr nifty be deeper r t ne side f the fidht ines r because f shaw dip r verburden effects.

48 PG w FLIGT LIN NMLY TGRY LLR R* FRQUNY INPS 57 QU. NUTR IR TP PT IGT MS MTRS MTRS.8 5.8, ,,9, , ,,, ,6, 6,,.8,6, F G 5, ,7.,8 5, 56,,,8,5,8,6, 5, 5.6 9, 9,,9, 5,9 5,,5,,,,9,5,6 5,6,, ,,, 9. 56,7, 78,.,, ,6,,8, 5, 6,, 9,7 7,,7,,8,5 6,8 7,, 8,6 5,5,5,9,5 5, ,,, :, stiated depth ay be unreiabe because the strnger part f the cnductr nisy be deeper r t ne side f the fight ine? r because f a shaw dip r verburden effects,

49 LLR RI r nc. FRQUNY 57 FLIGT LIN NMLY TGRY INPS QU. NUTR TP PT S MTRS IR IGT MTRS n t: F, ,6 9,6,...8*...9, stiated depth nisv be unreisbe because the strnger pert f the cnductr ay be deeper r t ne side f the fight ine* r because f a shaw dip r verburden effects*

50 i. ' ntari Ministry f Natura ^jsui ^surces Type f Survey(s) ai" der (i)""""" ddress Reprt f Wrk (Gephysica, Gegica, Gecheica and xpenditures) care Resurces Inc..^ urvey pany The Minin West radway, Vancuver,.. V6J W ate f Survey (fr ST t) u areas ew. Twnship r rea Per ist ^attached Prspectr's Licence N T55J.. - Tta Mies f ine ut 9 Nae and ddress f uthr (f Ge-Technicai reprt) redits Requested per ach ai in uns at right Specia Prvisins *f* Per Gephysica ai Fr first survey: nter days. (This incudes ine cutting) Fr each additina survey: using the sae grid: nter days (fr each) - ectragnetic i - Magneteter ' - Radietric i - ther Gegica Mining ais Traversed (List in nuerica sequence) Mining ai Prefix Nuber ' Xk^jtt, "! ;"? -*' PLS S TT xpend. ays r. Mining ai Prefix j Nuber -. fj-z'+k,. ^J^ iftiiim xpend. ays r " "~ -~ Man ays pete reverse side and enter tta(s) here Gecheica Gephysica - ectragnetic ' ;.,-'*-.. -*. '\? ^ Wf) *-'*fc±- ^. #jg. : - Magneteter - Radietric ther ^..:.'-.- i'jy:., ';-*t5'' c' --~ - - "-- j Gegica Gecheica irbrne redits Nte: Specia prvisins ectragnetic credits d nt appy t irbrne Surveys Magneteter v/uf -tv ays per ai ' - ' ~ ^ j-f-* -.'- T.."J. *'.')V-'- ' ' * '' '-.' iv'i^' ^:^i W^^" ~ ' -.' ' i WN 98 TT" T ' enditures (excudes pwer stripping) f Wrk Perfred MININ Z i-'"-*-.. ^^; ' ' V. ' Perfred n iai(s) - \ acuatin f xpenditure ays redits Tta xpenditures Tta ays redit -, Ttf nuiriht'f f IfirnS Vf t'd t iy t! i.'i t i')* W Mf f. a t ec. 9, 9'p-j ertificatin Venfying Reprt f Wrk hw eby c* ' ii y t tint J in w ;s (XM's.i ant i in, j! r k ( n,v!t-n.-. '! he s.srr- s* n.*t i f; ;f' r h' Mcjit i ; -t W f witness t si iml 'j F IM:I ;*"d 'i a f ei its i)mu*'i'! K: c ;int i i tn.i c x i '. J i cpi i i- tt utrjrn** ) F'stfi ei.ire^ Mrs. G.T. arke, 95 '.Ve:-t, 5th venue, Vancuver,.. V5Z S a\f ertified eit'fieti by (Signature) 6? 8/9)

51 ,.* v care Inc West radway -'. ' Vancuver,.. V6J W6 Teephne (6) 7-8 I x a i n e La k e Mining ais., L. e c! LI c:: T w n h i p, Thunder ay Mining ivisin, ntari. TTL... NUMR F Lft I MS 8 ai Nubers T 67587, 67588, 6759, 6759, 6759, 6759, 6759, 6759,, 67595,, 67596, 67597, 67598, 67599, 675, 675, 675, 675, 675, 6755, 6756, 6757, 675,, 6759,, 675., 675:!., 675, 675, 675, 6755, 6756, , 6758, 6759, 675, 675, 675, 675, 675. Partridge Lake Mining ais,, Legaut and ter Twnships, Thunder ay Mining ivisin, ntari. TTL NUMR F LIMS ^ ai Nubers T 6755, 6756, 6757, 6758, 6759, 67, 675, 675, 675, 675, 6755, 6756, 6757, 6758, 6759, 675-, 675!, ; 675,; 675, 675, 6755, 6756,, 6757., ter Lake Mining ais, ter and Vi ci an Twnships, Thunder ay Mining ivisin,, ntari.. TTL. NUMR F I..M aifii Nubers T 6767, 6768, 6769, 676, 676,, 676, 676, 676,, 6765, 6766, 6767, 6768, i769,, 676, 676, 676, 676, 676, 6765, 6766, 6767, 6766, 6769., 676, 676, 676, 676, 676, 6765, 6766, V \-

52 ntari tdinistry Natura Resurces rder f the Minister The Mining ct R 65, Whitney ck uppn's Park Trnt, ntari M7 W 6/965-8 f: In the atter f ining cais: T t 8 incusive T 6767 t 6 incusive in the Twnships f Leduc, Legaut, ter and Vician. n cnsideratin f an appicatin fr the recrded hder, under Sectin 77 Subsectin f The Mining ct, hereby rder that irbrne Gephysica (ectragnetic, Magnetjpge'- be extended unti and incuding March, 98 care Resurces Incrprated tie fr fiing reprts and pans in supprt f 'recrded n eceber. - 8 ate care Resurces Inc West radway Vancuver,.. V6J W6 erdat 88 Nashua rive Mississauga, ntari LV R ttentin: Sctt gg. \Signature f ybiractr. Land Manageent ranch cting cc: Mining Recrder Thunder ay, ntari (8/) T

53 ntari Ministry f Natura Resurces Getechnica Reprt pprva Fie Mining Lands ents T: Gephysics ents dtfrved Wish t see again with crrectins Signature T: Gegy - xpenditures ents f" pprved j Wish t see again with crrectins ate Signature T: Gecheistry ents [*"j pprved Wish t see again with crrectins ate Signature j[t: Mining Lands Sectin, R 66, Whitney ck. (Te: 5-8) 59 ( 8/)

54 pprved KeprU f Wrk sent ut Ntkt f Jnen fied i pprva after Ntice f Jnten sent ut upicate sent t Resident Gepist upicate sent t.f,r..

55 98 7 ur Fie: Yur Fie: Mrs. udrey ayes Mining Recrder Ministry f Natura Resurces P.. x 5 Thunder ay, ntari P7 5G6 ear Mada: e have received reprts and aps fr an irbrne (ectragnetic, Magneteter and VLF) Survey subitted n Mining ais T et a In the Twnships f Leduc Legaut ter and Vivian. This ateria wi be exained and assessed and a stateent f asessent wrk credits wi be Issued. Yurs sincerey,.. Yundt irectr Land Manageent ranch Whitney ck, R 66 Queen's Park Trnt, ntari M7 M Phne:(6) arr:c cc: cc: Tciare Resurces Ine -557 West radway Vancuver,.. V6J U6 erdat Liited 88 Nashua rive Mssssauga, ntari LV R ttentin: Sctt gg

56 care -557 West radway Vancuver,.. V6J W6 "- Teephne (6) 7-8 March, 98. Ministry f Natura Resurces, Whitney ck, R 66, Queen *s Par k, Trnt, ntari. M7 W Genteen: ncsed herewith tw cpies f Reprt n bined eicpter-rne Magnetic and ectragnetic Survey with aps and ne duy cpeted cpy f the Prvince f ntari Technica ata Stateent. We trust the encsed eets with the requireents f the Ministry f Natura Resurces. Yurs very truy, LLR RSURS IN. (Mrs.) G.T. arke, ccuntant.

57 Ministry f Natura Resurces Fie. ntari GPYSIL - GLGIL - GMIL TNIL T STTMNT T TT S N PPNIX T TNIL RPRT FTS SWN R N NT RPT IN RPRT TNIL RPRT MUST NTIN INTRPRTTIN, NLUSINS T. Type f Survey(s) eucfw Twnship r rea rea and Twnships per attached ai nder(s) LLR RSURS IN i -557 West radway, Vancuver,, MINING LIMS TRVRS List nuericay Survey pany. uthr f Reprt ddress f uthr Scer f (prefix) (nuber) vering ates f Survey. Tta Mies f Line u^ t S 8 (inecutting t ffice) w. cgits SPIL PRVISINS RITS RQUST Gephysica YS per cai i NTR days (incudes ine cutting) fr first survey. NTR days fr each additina survey using sae grid. ectragnetic. Magneteter Radietric ther Gegica. Gecheica. IRRN RITS (Specia prvisin credits d nt : appy ~ t -F airbrne surveys) F.prfrnagnptir (enter days per cai).r-aiei iietnc T:. SIGNTUR: Res. Ge...Quaificatins. Previus Surveys Fie N. Type ate ai der TTL LIMS (5/79)

58 GPYSIL TNIL T GRUN SURVYS If re than ne survey, specify data fr each type f survey Nuber f Statins Nuber f Readings Statin interva Line spacing Prfie scae ^ ^. ntur interva. Instruent ccuracy Scae cnstant. iurna crrectin ethd. ase Statin check-in interva (hurs). ase Statin catin and vaue ^ -^. Instruent i cnfiguratin i separatin ccuracy L.J Methd: ] Fixed transitter Sht back In ine Parae ine Frequency Paraeters easured. (specify V.L.F. statin) Instruent Scae cnstant rrectins ade. ase statin vaue and catin evatin accuracy. S Instruent ' Z Methd Tie ain Frequency ain Paraeters - n tie Frequency c y Pwer. ectrde array Q ectrde spacing. Type f eectrde ff tie Range. eay tie Integratin tie

59 SLF PTNTIL Instruent Range. Survey Methd.^ ^^^ rrectins ade. RIMTRI Instruent. Vaues easured. nergy windws (eves)^^^^-^^^^^^ ^^-^ ^ -.^ ^-^^^^ ^-. eight f instruent ackgrund unt. Size f detectr- ^^ ^^ ^.^ ^.^^^^ ^^^.- ^^ verburden - -^^, ^^^^^^ - (type, depth incude utcrp ap) TRS (SISMI, RILL WLL LGGING T.) Type f survey-...^. Instruent ^^^^^^^ ccuracy ^^ ^^ ^^ ^ ^^ Paraeters easured. dditina infratin (fr understanding resuts). IRRN SURVYS Type f gnrvpy(s) -gugtgjfc. --fr-\ j *rftpg.t\cl j Instruent(s) G&^Vs J^&^Qg^y ^ Q^n&^Us djs X (specify fr each type f survey) ccuracy (specify fr each type f rrvey) ircraft &Z&ffPT&LZ -STftr? Sensr atitude ' iwthus f ^ Surftkx-s f Navigatin and fight path recvery ethd nxm*. ircraft atitude / jget Le Spacing. Mies fwn ver tta area Ji ver cais ny Yfe

60 GMIL SURVY - PRUR RR Nubers f cais fr which sapes taken. Tta Nuber f Sapes. Type f Sape. (Nature f Materia) verage Sape Weight Methd f ectin NLYTIL MTS Vaues expressed in: per cent ~ p. p.. p. p. b. u, Pb, Zn, Ni,, g, M, s,-(circe) Si rizn Saped. rizn evepent. Sape epth Terrain rainage evepent stiated Range f verburden Thickness. SMPL PRPRTIN (Incudes drying, screening, crushing, ashing) Mesh size f fractin used fr anaysis thers Fied naysis (~ xtractin Methd. naytica Methd- Reagents Used Fied Labratry naysis N. xtractin Methd. naytica Methd - Reagents Used ercia Labratry (- Nae f Labratry xtractin Methd. naytica Methd Reagents Used -.tests).tests).tests) GeneraL Genera.

61 ft care esurces Inc West radway Vancuver,.. V6J W6 Teephne (6) 7-8 xaine Lake Mining ais, Leduc Twnship, Thunder ay Mining ivisin, ntari. TTL NUMR F LIMS ^ 8 ai Nubers T 67587, 67588, 67589, 6759, 6759, 6759, 6759, 6759, 67595, 67596, 67597, 67598, 67599, 675, 675, 675, 675, 675, 6755, 6756, 6757, 6758, 6759, 675, 675, 675, 675, 675, 6755, 6756, 6757, 6578, 6759, 675, 675, 675, 675, 675. Partridge Lake Mining ais, Legaut and ter Twnships, Thunder ay Mining ivisin, ntari. TTL NUMR F LIMS ai Nubers T 6755, 6756, 6757, 6758, 6759, 675, 657, 675, 675, 675, 6755, 6756, 6757, 6758, 6759, 675, 675, 675, 675, 675, 6755, 6756, 6757, ter Lake Mining ais, ter and Vivian Twnships, Thunder ay Mining ivisin, ntari. TTL NUMR F LIMS * ai Nubers T 6767, 6768, 6769, 676, 676, 676, 676, 676, 6765, 6766, 6767, 6768, 6769, 676, 676, 676, 676, 676, 6765, 6766, 6767, 6768, 6769, 676, 676, 676, 676, 676, 6765, 6766.

62 Q v ri J Mb LGULT TWP en n I z c - ^T? j] :u rn en en r-. LINSLY TWP G-8 5 I 5 w ZZ I ^ - ^ Ge IJJ -^ * - ^ S 7 -* 5 5 > S T, ra fr Q Z u M Z z n i x -- * r r w 5 f" > z ) n tn i 55 Z S ^ i ) 9 ) I I. - * z en en Z 5 S 5 i en z en en x w G ^- w ) en S z c > en in i^ ] 5 S ) tn -n Z c i- en en TJ z ] S r- ^ u en r- w en c 5 w J ^ p c < J d 5S Z ^,- Z X en ^z^ 5 I r ffi w z.t ^ z (7 P w " L i - Z > -n en en ^ - en n ) - I en ) en z W KJ * -, f- I ^ ' R J

63 e-iea Waters Twp. G-7 Mb 68- * s S" s yi V M t? aj w * X Z ) T) ( - -n rv i w v i t.* _!,' -J -n * J p TP r ) - e a Q. en c/5" r Q ]* " r L - \ \ S - -- * L.k "~S" " 'M".T I i i --K w -, ' ' J ~ -- J- -i -J--.-i _. 7" *. T.* r i T a T. ' ^ s - Legaut Twp. G -7

64 ^ ISPSITIN F RWN LNS TYP F UMNT SYML LPIRR TWP. G-65 M M IGWY N RUT N. TR RS LGN PTNT, SURF S. MINING RIGTS... 9 TRILS..SURF RIGTS NLY...^...,,... SURVY LINS:, MINING RIGTSNLY ^^...,..,.^... Q LS SURF 8i MINING RIGTS M ", SURF RIGTS NLY,...,...,.^^. ", MINING RIGTSNLY..^^...^... Q LIN F UPTIN ^_ ^ T RR-IN-UNIL ^..... RSRVTIN... (J) NLL _......,.. SN 8 GRVL ^... g) NT: M INING RIGTS IN PRLS PTNT PRIR T MY 6, 9, VST IN RIGINL PTNT Y T PULI LNS T, R.S.. 97, P. 8, S 6. SUS. IM NMWMINIK - - ^- RIVR LPIRR TWNSIPS, S LINS, T. LTS, MINING LIMS, PRLS, T UNSURVY LINS: LT LINS PRL UNRY MINING LIMST. RILWY N RIGT F WY UTILITY LINS NN PRNNIL STRM FLING R FLING RIGTS SUIVISIN R MPSIT PLN RSRVTINS RGINLSRLIN MRS R MUSKG RS W ITRWN FRM ISPSITIN MINS TRVRSF MNUMNT S.R.-SURF RIGTS M.R. -MINING RIGTS escriptin rder N. at* ispsitin Fie M T --t~----\~ -. ' - IT T8 T ^ [675 T V T "T fa" 7^: ' ~"~ ~ - ~~ ~ 'f ^(6756 ""- -- I SN ft GRVL GRVL RSRV FIL 686 M.T. G RVL PIT N* -I6 M.T.. GRVL P IT ' N* -I7 i e) a: SL: IN ^ INS Q U L. I Q LJ J LGULT MTRS 6 KM) ( KM i- ^ cr. LK TWNSIP LGULT MN.R. MINISTRTIV ISTRIT NIPIGN MINING IVISIN TUNR Y LN TITLS/ R GISTRY IVISIN M F ISSU JUN rtna TRNT IN85e.655 LTR T! T 7)5^9, ^759, R 759 S5565 [5955,5955 \ t [655^7 j688j(* j SUT F LGULT TWP. G-II 5M ate TUNR Ministry f Natura Resurces FRURY, I9PI Y Land Manageent * ranch Nuber G-7 i."

65 ) Q - IIV/ Mb' \PRJT TWR UNRY SUT TTY LK G- I rn r PRJT PRNT TWR G-69 ) ) ~ z* 5. ^ W W e i- ^ -* Q) * S S a n n > 5 fe* r i i x S Z Z g i [ w Z * Z x x5 z (n -" S; i = '5s w "j.8* rr* nt Z X " > ) X S a S rt -T, Z p 5? P S = J -" g^ w Vi - S i "~ ^ 5 Z VJ j-. ) ~ 5 5 a.? " z x I /) Z s n -n z d z s z z I en n ^ VJ Z c z z Z c ( ^ ( Z M ^ -r, ^ z z - Z z ) s? - S " ci n 5 c w?; 5 n ^ /) r- j < 5* W -* -^. ^- ^" ^ yi 5 I fs i 5 -- en Z - T) / W z rt c -t z r * c n I.qWT-IVIV

66 nductivity thickness in ns RT M SYSTM RSPNS VRTIL LF-PLN 5 inphase respnse M nav, in-phase aph'ude 7 p p ntfpreted :nduc: axis Z within bedrck riznta cntr. Pssib* cnductr axis within bedrck verage bird height Line spacing LLR RSURS LT. IRRN LTRMGNTI SURVY INTRPRTTIN MP GRLTN R NTRI SL /, ^z^&s-^ eceber 98.t-J~"'!.'Wfti-.i

67 nductr ii* ^ '" within btdrck Pssibe c nductr nis within bsdrck riznta cntr..,..... based n pht aydwn verage bird height,,.,.... etres -:-v- "* **p?#* Line spacing efr*s LLR RSURS LT. T 6*56 IRRN LTRMGNTI SURVY INTRPRTTIN MP GRLTN R NTRI L / eceber 98 Ne5.655 LTR

68 M RSPNS TPiijndjc'r aiis" u within b edrck Pssibe cnductr axi w ithin bedrck nductivity thickness in hs ( > 5 (g) 5-5!5-5 (e) () -8 - < 5 Inpnase respnse riznta cntr based n pht aydwn verage bird height etres Line spacing etres 87 ' LLR RSURS LT. IRRN LTRMGNTI SURVY INTRPRTTIN MP GRLTN R NTRI 66 SL /, / ite Kietre T' eceber 98 VRT LIMIT N. T N MP N' N5.655 LTR G

69 LLR RSURS LT. IRRN LTRMGNTI SURVY PRFILS - 95 z. (caxia) GRLTN R NTRI. i '*' " SL i,. - * -, - f eceber 98 T RT LIMIT

70 LLR RSURS LT. IRRN LTRMGNTI SURVY PRFILS - 95 z. (caxia) GRLTN R NTRI 66 LL /, / ie 5 Kietre '# fi, VRT LIMIT eceber 98

71 p.p.. i t In-phase Quadrature 87 ' 9 5 LLR RSURS LT. IRRN LTRMGNTI SURVY PRFILS - 95 z. (caxia) GRLTN R NTRI 66 SL /, / ie 5 Kietre T eceber 98 W RT LIMIT N. T. S. N

72 L LGN gaas. 5 gaas. gaas. 87 ' 9 5 LLR RSURS LT. TTL FIL MGNTI MP GRLTN R NTRI 66 S L F /, 5 ' Kietre T eceber 98 T RT LIMIT N. T. N - N5.655 LTR

73 -^^ '-"if fjj i a ^p L a J r ^i^ial ^ I--^^^P ^I^K :- ^V ^* ^ ^ J Q w ^J K J J ( ) J - ) PJ rvj S ( (M r (NJ ^: n^ ^ rg r J * t -N- LGN I 5 ' gaas... gaas. gaas LLR RSURS LT. TTL FIL MGNTI MP GRLTN R NTRI S LL /, 66 : / ie 5 Kiefre T RT LIMIT i eceber 98 N LTR

74 -J- LGN gaas 5 gaas gaas 87 ' 9 5 LLR RSURS LT. TTL FIL MGNTI MP GRLTN R NTRI SL /, 66 / ie t 5 Kietre T eceber 98 W RT LIMIT N.T. S, N MP N LTR

75 N LGN / /..... Statin N Lines - 5 -Sfatin NSS 87 ' 9 5' LLR RSURS LT. VLF-M TTL FIL NTUR MP GRLTN R NTRI SL /, 66 / ie. 5 Kietre eceber 98 VRT LIMIT

76 LGN V. X.... '/... Statin N 87 ' 9 5 LLR RSURS LT. VLF-M TTL FIL NTUR MP GRLTN R NTRI SL /, 66 / ie 5 Kietre " eceber 98 N.T. S. N :

77 Statin N LLR RSURS LT. VLF-M TTL FIL NTUR MP GRLTN R NTRI GL /, eceber 98 N59.655