REPORT ON THE DRILLING AND THE BOREHOLE ......Report on the Drilling and the Borehole Geophysical...

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010

15309 FEB 2 l 1994

MINING LANDS BRANCH

Report on the Drilling and the Borehole Geophysical Programs

Tri Origin Exploration Ltd.

Sault Project

Runnalls Township, Ontario

(N.T.S. 41N/8)

July 29 to September 23, 1993

YR. A. Campbell M.J.Perkins

\ 4iNaasE97ai a.isaes RUNNALLS

Cant

IntroductionLocation and AccessProperty DescriptionPrevious WorkPrevious work by Tri Origin Exploration Ltd.Present WorkRegional GeologyProperty GeologyDiamond Drilling ProgramBorehole PEM surveyConclusions and RecommendationsReferencesStatement of Qualifications

Figure 1. Figure 2. Figure 3.

Table l. Table 2.

Appendix l, Appendix 2, Appendix 3,

Figures

Location of Sault Project. Sault Project Claim Map. Drill Hole Location Map

Tables

Sault Project Claims. Drill Hole Information.

Appendices

Drill Hole Records and Sections Geochemical Analysis Certificates. Borehole PEM Survey Report

Maps (attached)

010C

Pagel l l78 B S

10 13 15151617

23

11

414

198597

Geology Compilation and Drill Hole Location Map, North Sheet, 1:5000 scale.

Geology Compilation and Drill Hole Location Map, South Sheet, 1:5000 scale.

Sault Project Drilling 1993

\Introduction

From August 9 to September 23, 1993 a diamond drilling program was conducted on Tri Origin Exploration Ltd.' s Sault Project located in northern Ontario. Near the end of the drilling campaign, a borehole PEM survey was completed on eight of the drill holes. This report summarizes the work completed.

The drilling program was designed to test a number of favourable targets delineated by an earlier Induced Polarization (IP) survey. Geological mapping indicates that the primary cause of the IP responses appears to be sulphide iron formation units composed primarily of pyrite and pyrrhotite with minor sphalerite. Several of the sulphide iron formations assayed anomalous for gold prompting the drilling program to determine if economic mineralization improves at depth.

For the most part, the drilling program confirmed the nature of the IP response and the borehole PEM survey supplied additional information concerning direction and strength of the conductors. Included in this report are the drill logs, plan maps, drill sections, assay data,and a copy of the borehole PEM survey report.

Location and Access

The Sault property is located 100 kilometres north-northeast of Sault Ste. Marie, within the eastern half of Runnalls Township, northern Ontario (N.T.S. 4IN/8) (Figure 1) .

The property is accessible by the Trans Canada Highway #17 from Sault Ste. Marie to local logging roads situated 60 kilometres north near Batchawana Bay. Then travel east- northeast along the logging roads for 60 kilometres. Recent logging activities in Runnalls Township have increased road access considerably over the last year. The locations of these all weather gravel roads are indicated on the attached 1:5000 Compilation maps. In addition, the Algoma Central Railway and power lines are adjacent to the property. An alternate access is by float equipped fixed-wing aircraft based at Batchawana Bay or by helicopter from Sault Ste. Marie.

Property Description

The Sault property is comprised of 104 unpatented mining claims totalling 1920 hectares (figure 2). The description of the claims is summarized in Table l and includes the claim number, recording date, anniversary date, and number

Sault Project Drilling 1993 l

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GENERAL GEOLOGYO 10 l*.

LEGEND

PROTEROZOIC ROCK

SEDIMENTARY ROCK

v v | VOLCANIC ROCK

PAST PRODUCING MINES

TrI Origin Exploration Ltd.

SAULT PROPERTY - ONT

PROPERTY LOCATION

Don- | By R.V

TABLE 1: DESCRIPTION OF CLAIMS

OA1M NUMBER

1136231

1136232

1136233

1136234

1136235

1136236

1136237

1136238

1136239

1136240

1136241

1136242

1136243

1136244

1136245

1136246

1136247

1136248

1136249

1136250

1136251

1136252

1136253

1136254

1136255

1136256

1136257

1136258

1136259

1136260

1136261

1136262

1136263

1136264

1136265

RECORDING DATE

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

ANNIVERSARY DATE

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

16 HECTARE UNITS

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1


\1136266

1136267

1136268

1136269

1136270

1136271

1136272

1136273

1136274

1136275

1136276

1136277

1136278

1136279

1136280

1136281

1136282

1136283

1136284

1136285

1136286

1136287

1136288

1136289

1136290

1136291

1136292

1136293

1136294

1136295

1136296

1136297

1136298

1136299

1136300

1136301

1136302

1136303

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1


\1136304

1136305

1136306

1136307

1136308

1136309

1136310

1136311

1136312

1136313

1136314

1111714

1111715

1111716

1111717

1111718

1111719

1111720

1111721

1111722

1111723

1111724

1111725

1111726

1111727

1111728

1111729

1179152

1179154

1165545

1165546

104

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

04/10/89

06/08/92

06/08/92

31/05/93

31/05/93

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

05/10/96

06/08/98

06/08/98

31/05/95

31/05/95

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

2

15

2

120


\ of 16 Hectare units contained in each claim. As of October 12, 1993 all claims are in good standing and owned by Tri Origin Exploration Ltd. located at 15449 Yonge St., Suite 102, Aurora, Ontario, L4G 1P3.

Previous Work

Past work in the vicinity of the Sault Property has been limited in part due to poor access and mineral rights ownership of a large number of townships by Algoma Central Railway (ACR) .

Jalore Mining Company Limited (1953) conducted an airborne survey over the map area. Banded oxide-facies iron formation was detected during ground follow-up of selected anomalies (Grunsky 1980).

Algoma Central Railway completed an airborne Electromagnetic Survey over the Batchawana greenstone belt in 1962 and trenched several sulphide showings east of Doyle Lake.

Rio Tinto (1964) completed ground geophysics, geology surveys and trenching over 19 conductors identified from the ACR survey. Graphite and sulphide occurrences hosted within felsic volcanic and sedimentary rocks were confirmed in 14 of these conductors, within the Doyle Lake area. Eight conductors are within the Tri Origin Property and previous work by Rio Tinto defined elevated gold and copper values associated with three of these conductors. Anomalous gold, 0.01 ounce per ton Au across 45 ft., was detected from trenching a sequence of east-west trending acid to basic lavas and sediments on Grid E-2, located immediately northwest of Doyle Lake.

Conductor E-3 which straddles the northern property boundary, is underlain by schistose felsic volcanic rocks and assayed 0.01 ounce per ton Au and Q.07% Cu across 4 ft. Up to Q.30% Cu across 25 ft. is reported from trenching on Grid F-2 (North Grid), overlapping the volcanic/sedimentary rock contact.

Canex Aerial Exploration Ltd. (1966) drilled one hole into an airborne anomaly near the northern boundary, within the property limits and intersected a pyrite-pyrrhotite-graphite conductor.

Geophysical Engineering (1975) completed two drill holes to test airborne anomalies immediately north, and 1200 metres southeast of Doyle Lake. Both holes intersected pyrite and pyrrhotite hosted within felsic volcanic rocks.

Sault Project Drilling 1993 7

Manwa Exploration (1984) flew a Dighem airborne electromagnetic survey over Runnalls Township, outlining eight isolated conductors on the property.

Granges Exploration Ltd. (1986) performed follow-up ground geophysics and geologic mapping on the airborne anomalies defied by the Manwa surveys. Seventeen drill holes were completed to test eighteen conductors. Ten drill holes were located within the confines of TriOrigin's property to test 5 separate conductors. Anomalous gold was detected on the West Grid in hole 86-13, with assays up to 5.5 grams per tonne over 0.80 metres, underlain by a carbonate-rich disseminated pyrite horizon within quart z-sericite schist. Four follow-up holes, 86-18, 19, 20, and 21 were drilled on the same horizon in an attempt to trace the auriferous sulphide zone, located at the volcanic/sedimentary contact. Up to 7 metres of massive sulphide, pyrite and pyrrhotite containing anomalous values in zinc and gold was intersected along a strike length of 150 metres, however gold values greater than 500 ppb at the volcanic/sedimentary contact were only detected in hole 86-19 which assayed 2.56 grams per tonne over 0.40 metres. The sulphide horizon coincides a NNW trending airborne electromagnetic conductor which extends for 2400 metres.

The Ontario Geologic Survey (1990) flew an Airborne Electromagnetic Survey over the entire Batchawana greenstone belt. Six isolated conductors are defined by the Aerodat Survey within the property boundary. However, the survey was flown in an north-south direction, locally parallel to stratigraphy and may have missed some anomalies. A regional lake sediment geochemical survey was also completed over the Batchawana greenstone belt by the OGS (Fortescue, 1990) .

Previous Work by Tri Origin Exploration Ltd.

In 1989-90, Tri Origin completed 33 kilometres of linecutting, reconnaissance and detailed geologic mapping, prospecting, 25.6 kilometres of induced polarization (IP) surveys and 903.5 metres of diamond drilling in 7 holes, on the property.

In 1992, TriOrigin completed 60 kilometres of linecutting and geologic mapping and 40 kilometres of IP surveys. Eleven trench areas (approximately 100 x 5 metres) were excavated over six IP responses. Forty-eight preliminary rock samples were taken from nine trench areas and assayed for Au. Anomalous gold values were obtained in 3 trench areas, ranging up to 3.40 grams per tonne.

In early 1993 a humus geochemistry sampling program was


\completed over areas surrounding the IP responses delineated in the 1990 and 1992 geophysical surveys. Eight hundred and forty-two samples were analyzed for Cu, Pb, Zn, and Au.

Present Work

From August 9, to September 23, 1993; 12 BQ diamond drill holes were completed totalling 2477 metres. A total of core samples were taken.

In addition several days were spent examining the geology along logging roads cutting through the property. 32 rock grab samples were taken of sulphide iron formations discovered and assayed for copper, lead, zinc and gold.

Regional Geology

The Sault property lies within the Batchawana Greenstone Belt of the Superior Province. This belt is an Archean-aged greenstone belt consisting of a thick succession of supracrustal rocks. The dimensions of the greenstone belt is roughly 40km x 20km and is bordered by Lake Superior in the west, Montreal River to the north, Goulais River to the east, and Harmony River to the south.

The area has been geologically mapped by Siragusa (1986), Grunsky (1980), and Grunsky (1987a). The area has been subdivided into an Early Precambrian Intrusive complex including migmatite, granodiorite and trondhjemite; and a supracrustal sequence that has been deformed and metamorphosed by later quartz monzonite stocks and plutons (figure 1) . The supracrustal assemblage has been subdivided into a lowermost mafic to intermediate volcanic platform predominated by flows, overlain by felsic to intermediate rocks of pyroclastic through volcaniclastic derivation and capped by a thick sequence of clastic sedimentary rocks (Robinson, 1993). The property straddles a northwest- trending volcano-sedimentary contact which represents a major structural/stratigraphic break. The sequence dips steeply to the northeast and is overturned; tops are west to southwest. The volcano-sedimentary contact is characterized by a transitional facies change from felsic pyroclastic and volcaniclastic rocks to a clastic sedimentary dominated assemblage. The area is intruded by a northwest-trending swarm of diabase dykes. Major northeast trending faults such as the Batchawana River and Montreal River faults offset stratigraphy resulting in significant geological changes across these faults.


Property Geology (Robinson, 1993)

The Sault property is underlain by felsic volcanic and clastic sedimentary rocks, trending N 20 W to N 60 W and dipping 70 northeast to vertical. The volcanic/sedimentary rock contact forms an arcuate trend which extends northwesterly along the western portion of the property approximately 300 metres west of Doyle Lake (figure 3) . The property is bounded to the southwest by the Grey Owl Lake Stock, in addition an elongated apophyses or porphyritic felsic intrusive rock has intruded the felsic volcanic sequence near the regional volcano/sedimentary rock contact (figure 3) . Mafic volcanic rocks occur north and east of the property. Up to seven (7) stratabound chert- sulphide - bearing stratigraphic units are within the felsic volcanic rocks and one or more chert -sulphide -bearing units are within the overlying clastic sedimentary rocks.

Multiple northwest -trending diabase dykes crosscut the stratigraphy. A major splay of the Batchawana River fault crosses the south part of the property. Correlation of geological units southward across this fault is uncertain.

Felsic Volcanic Rocks

The property geology is predominantly underlain by a thin to thick bedded sequence of felsic tuff. The felsic volcanic sequence ranges in fragment size from fine ash tuff, crystal tuff to lapilli tuff. Quartz-plagioclase-muscovite schist and discrete disseminated to semi -massive sulphide zones occur within the felsic volcanic and sedimentary rock assemblage. Disseminated pink garnet, up to X-2%, and green amphibole (hornblende) porphyroblast s and layers are common accessory minerals within the felsic tuff.

Felsic lapilli tuff occurs south and east of Doyle Lake, extending northward to the property boundary. Fragments up to 12cm, hosted within a fine grained intermediate matrix are noted, and locally contain porphyroblastic aluminous mineral assemblage including garnet (Valliant, 1991; Grunsky, 1978) . Northeast of Doyle Lake, lapilli fragments are contained within a matrix of semi -massive to massive pyrite, which coincides with an airborne electromagnetic anomaly. Felsic tuff is quartz and sericite rich, and commonly contains quartz and/or feldspar crystal -rich layers. The felsic volcanic rocks grade westward and stratigraphically upward into a clastic sequence derived from tuff.

Clastic Sedimentary Rock

Clastic sedimentary rocks regionally form a central


LEGEND

IP Anomaly A Sulphide Zone

. Geological Contact

Diamond Drill Hole

Trench location

Tri OriginExploration Ltd.

sedimentary basin flanked by a mixed mafic to felsic volcanic base. Thin to thick bedded greywacke predominates the western portion of the property. Sedimmentary rocks and felsic tuff interfingers adjacent to the Grey Owl felsic intrusion bounding the West grid.

The felsic volcanic and clastic sedimentary units (greywacke) are locally interfingered and display a westward facies change towards a clastic-dominant succession. Clastic sedimentary rocks are thin to thick bedded, dark grey to brown, fine grained and lack quartz or feldspar crystals. The greywacke unit has a light brown weathered surface and commonly contains lQ-25% accessory biotite and chlorite. Up to 5% accessory andalusite occurs as 2 to 5 mm, subhedral porphyroblasts forming bands and disseminations, in close proximity to a definite IP anomaly at the north end of the West grid.

The sedimentary rocks are locally difficult to distinguish from felsic tuff.

Iron Formation

Up to 7 or more semi-continuous chert and sulfide facies iron formation units have been identified on the property in outcrop, drill core and interpreted from IP surveys. Iron formation subcrops along TL 1000 S/1100 E for in excess of 500 metres in length and ^0 metres in width. Grey to white microcrystalline quartz (chert) is intercalated with siliceous and locally sericitized felsic tuff. The chert matrix contains l to 5% pyrite, and lesser amounts of pyrrhotite as disseminations, veinlets and bands up to 10 cm wide. Accessory graphite, up to 40*, has been reported from previous trenching and drilling by Granges, Canex Aerial and Rio Tinto. Anomalous gold up to 1663 ppb was detected from surface sampling. Previous trenching by Rio Tinto also encountered anomalous concentrations of Cu up to Q.30% across 25 feet. Pale pink to tab garnet, up to 13s, occurs as an accessory mineral in a siliceous matrix. Garnet in iron formation is optically different than garnet within felsic tuff.

Grey Owl Felsic Intrusive Rocks

The Grey Owl felsic intrusive stock forms a pronounced topographic high bounding the volcano-sedimentary sequence along the western margin of the property. The felsic intrusive rocks are most commonly massive to foliated, medium grained, granodiorite and trondhjemite according to Grunsky (1981) . A small felsic intrusive stock occurs within the felsic volcanic succession between the West grid and the Doyle Lake grid, and a second felsic intrusive stock


\TABLE 2: 1993 DRILLHOLE PROGRAM

HOLE

#

T93-08

T93-09

T93-10

T93-11

T93-12

T93-13

T93-14

T93-15

T93-16

T93-17

T93-18

T93-19

TOTAL

12

LOCATION

LINE

972E

646E

1063E

12 8 BE

1526E

2725N

900N

610N

100S

410N

600S

1200N

-

STATION

550S

575S

900S

797S

850S

750E

525E

575E

500E

600E

500E

500E

-

BEARING degrees

220220220

220

220

250

250

250

250

250

250

250

-

INCL. degrees

-60-60-60-60-60

-60

-65

-65

-65

-60

-65

-45

-

DEPTH

meters

294214

183

276

198

180

192

189

200

201

189

161

2477


\a one (1) metre split were 1941 ppb and 1149 ppb both from heavy concentrations of sulphide in hole T93-15. Some of the other holes had gold values associated with heavy- concentration of sulphide in the 100's of ppb. In a number of the hole the sulphide intervals were intruded by late diabase dykes. The graphite conductors were not anomalous. A more detailed desnption of the results and gold values is attached in Appendix l and 2.

Survey Staff

The drilling program was supervised by R.A.Campbell, 3277 Golden Eagle Dr., Burlington, Ontario, and Michael J. Perkins, 514 Crawford St., Toronto, Ontario. Certificates of qualification are attached.

Drilling was completed by St-Lambert Drilling Co. Ltd., PO Box 473, Valleyfield, Quebec, J6S 4V7.

Borehole PEM Survey

At the request of Tri Origin, Crone Geophysic St Exploration Ltd. conducted a borehole PEM survey on eight of the drill holes. The survey was conducted near the end of the drilling program from Sept. 9-18, 1993. The holes consisted of three from the northern part of the property (Doyle Lake Grid) and five from the southern part of the property (West Grid). The details of the survey are found in Crone's report attached in appendix 3.

Conclusions and Recommendations

Anomalous gold values have been obtained from massive to semi-massive sulphide mineralization which includes pyrite, pyrrhotite and minor sphalerite. The width and strike length of these sulphide horizons is encouraging and could host a sizeable gold deposit. The geological setting is similar to that of both Hemlo deposit and the Bousquet camp.

Further drill testing along the sulphide horizons is reccomended.

R.A. Campbell Michael J. Perkins

Oct. 22, 1993


\References

Grunsky, E.G. 1980. Geology of the Cowie Lake Area, District of Algoma; Ontario Geological Survey, Report 192, 67p.

Grunsky, E.G. 1987a. Precambrian geology of the Batchawana synoptic project area, Grey Owl Lake sheet, District of Algoma; Ontario Geological Survey, Preliminary Map P.3063, scale 1:50,000.

Robinson, D. 1993. Summary report: Sault project;Unpublished company report, Tri Origin Expl. Ltd.,

Siragusa, G.M. 1986. Geology of the Batchawana-Pangis area, District of Algoma; Ontario Geological Survey, Report 243, 56p.

Valliant, R.I. 1991. Summary report: Sault project;Unpublished company report, Tri Origin Expl. Ltd.,


t CERTIFICATE of QUALIFICATION

I, Michael James Perkins, currently living at 514 Crawford Street, Toronto, Ontario, certify the following:

1. I currently hold two diplomas in Exploration Geology obtained in 1982 and 1983 at Sir Sandford Fleming College.

2. I have completed three years towards a BSc. in geology at the University of Toronto.

3. I have been employed in most capacities of an exploration geologist for the past 10 years.

4. I was present on the property during theperiods covered, and completed or supervised all work covered in this report

Michael J. Perkins July 28, 1993


CERTIFICATE OF QUALIFICATION

As author of this report on the Sault property of Tri Origin Exploration Ltd., I hereby make the following statements:

1. My name is Robert Anderson Campbell, and I am a Consulting Geologist retained by RAG Geological Consultants Inc. My business address is 3277 Golden Eagle Dr., Burlington, Ontario, L7M 2S4.

2. I have received the following degrees in the Geological Science:

B.A. 1978 University of California atSanta Barbara, Santa Barbara, California

M.Se. 1985 University of Western Ontario,London, Ontario

3. I have been practising my profession for over thirteen years.

4. I am a member of the Prospectors and Developers Association of Canada.

I have neither received nor do I expect to receive any interest, direct or indirect, in Tri Origin ExplorationLtd.

Dated at Burlington, Ontario

^ _____ October 12, 1993

Robert Anderson Campbell


RUNNALLS TOWNSHIP

f MO MO no too

TRI ORIGIN EXPLORATION LTD.

SAULT PROPERTY CLAIM MAP

October, rtgarm t prepared by ROBINSON EXPLORATION SERVICES LTD.

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III

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i \ vNl?13 \\ i \Q.j^ 90-2 M

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\

LEGEND |L^ 'Felsic Intrusive Rocks ^ !l \

Sedimentary Rocks

Felsic Volcanic Rocks

Mafic Volcanic Rocks

IP Anomaly 4 Sulphide Zone

. Geological Contact

Diamond Drill Hole

Trench location

1km

i

Tri Origin l Exploration Ltd.

Appendix 3. Crone Geophysics k Exploration's Borehole PEM Survey Report


CRONE GEOPHYSICS a EXPLORATION LTDion? \VOU ;i;i)AU:K(.',U). MISSISSU'CiA. OMAKIO. CANADA L5C IVS

ILL: i4l(u 27(I-IKW(. - F-AX: t4]oi:7(i-.U?: . TKLLX: Oo-W^MI

Preliminary Interpretation Report September 2 8, 1993

Client: Bob ValliantTri Origin Exploration

Survey: Borehole PEM SurveyCrone Geophysics k Exploration Ltd.September 9-18, 1993

Project: Doyle Lake and West GridsSault ProjectBatchawana, OntarioCanada

By: Ken NurseCrone Geophysics 6 Exploration Ltd.

Introduction:A report giving survey details and a preliminary

interpretation of the time domain EM survey of eight boreholes in the Batchawana area of Ontario. The Crone three component borehole PEM survey was carried out in September 1993 by Crone Geophysics S Exploration.

This report includes a summary of the field survey particulars, plan and section maps, copies of field data and a quick interpretation of said data.

Survey Details:Survey information can be found in the appendix of this

report. No significant equipment problems were encountered, however the weather and access to the holes caused loss of survey time. One day was lost due to heavy rainfall. Eventhough the holes were short, all but one less than two hundred metres, transportation to the holes was difficult with equipment having to be transported by hand. Site geologists Andy Campbell and Mike Perkins aided in this undertaking. Accommodation was provided by Tri Origin at Meakin's Redcliff logging camp.

Preliminary InterpretationA brief analysis of each hole's data is below. Sketches of

probable conductor locations are included in the Appendix's plan and section maps for each borehole.

Doyle Lake GridOf note, holes T93-10 and T93-11 are separated by less than

two hundred metres, and thus overlapping regions of sensitivity are observed.

Preliminary Interpretation Report 2s

Hole T93-10Four individual conductors can be observed in the section, the

most dramatic at 120m. This off-hole expression dominates the section. Superimposed on this is several other anomalies.

Depth 95m:A minor in-hole 8 channel anomaly. Cross-component data

indicates it continues below and to the west of the hole.Depth 120m:A 20 channel edge anomaly that has a very high conductance.

The off-hole portion of this conductor is approximately 50m radially from the hole, below and to the east.

Depth 160m:A very conductive in-hole anomaly that continues below and to

the east of this intersection.Depth EOH;All channel amplitudes are building with the early channels

increasing positively whereas the late channels are going negative in the axial component. This suggests another edge anomaly of very high conductance. The cross-hole data is somewhat inconclusive since a full expression is not observed, but it appears to suggest the conductor continues below and to the west of the probable hole intersection or closest approach.

Hole T93-11This section has a significant off-hole anomaly at 180m with

some in-hole hits as well.Depth 180m;A 20 channel off-hole anomaly 75-100m radially from the hole

above and to the west. This conductor has a very high conductance.Depth 205m:An edge anomaly, continuing above and to the west. It's

response is being masked by the 180m anomaly.

From holes T93-10 and T93-11.....Both these holes, T93-10 and T93-11, are responding to two or

more conductors located between them. The significant off-hole responses are due to one, or more likely, multiple parallel conductors. The anomaly at the bottom of hole T93-10 is not, as expected, observed in T93-11. It is in the opposite direction with very high conductance and seems interesting.

Hole T93-12A moderate to weak off-hole anomaly at 150m hole depth. It is

approximately 75m radially above and to the west from the hole.

Preliminary Interpretation Report 3*

Mast GridSimilarly to the Doyle Lake grid, holes T93-15 and T93-17 have

overlapping areas of investigation. The other three holes are isolated. In all instances anomalies are located above the hole, and generally occur as multiple conductors.

Hole T93-14Multiple conductors are observed and their resulting responses

are being superimposed. This makes an accurate interpretation more difficult. It appears to be a large off-hole response from one or multiple parallel conductors with individual lenses intersecting the hole.

Depth 105m:Strong in-hole conductor with current migration above and to

the north of this depth.Depth 125m;Another sharp strong in-hole conductor that also extends above

to the north.Depth ~120m:The approximate location of a long wavelength moderate off-

hole anomaly, on the order of 100m from the hole to north and above the hole. It's shape is quite probably distorted by the above observed conductors. Cross component data also indicates that it is above and to the north of the hole.

The in-hole intersections are part of a more conductive complex above and to the north of the hole. Late currents are migrating about 100m radially off the hole, however, if it is multiple parallel conductors, this distance could be significantly less.

Hole T93-15This hole and T93-17 are responding to related conductors

located between them. Multiple conductors are superimposing themselves, similar to hole T93-14.

Depth 105m:An in-hole (probable edge) strong conductor extending above

and to the south.Depth 120m:Another edge anomaly with similar characteristics to the

above.Depth 120-125m;This is the rough centre of a broad off-hole anomaly that is

asymmetric suggesting its extending downhole. Cross component data indicates it is above and to the south. Distance to the conductor is on the order of 100m, however the superposition of multiple conductors could be exaggerating this value.

Preliminary Interpretation Report 4*

Hole T93-17Depth 110m:Most likely a very conductive in-hole conductor, probably 10-

20m thick, continuing above and to the north. The early channels (chl-5) are crossing over, suggestive of a thick conductor, yet the PP channel does not support this (it doesn't diminish in amplitude significantly). Possibly a thick conductor stops near the hole and the change in signature is due to current migration from one face to another. In this instance, a copy of the drill log could clear up this ambiguity.

Depth 120-150m:A broad off-hole conductor, or associated with the conductor

at 110m. Due to its apparent thickness, estimates of distance to it are difficult, but less than 100m above and to the north are indicated. The intersection at 100m depth is most likely associated with this response.

From holes T93-15 and T93-17.....The two significant anomalies of holes T93-15 and T93-17 are

probably a continuous horizon of a thick conductive layer or multiple layers extending between the two holes. More conductive material is approximately equidistant from the holes. Significant conductances on either side of these holes cannot be observed from the data (i.e. the holes bracket the high conductivity zone).

Hole T93-16A near off-hole conductor (25-50m) of high conductance lying

above the hole and to the north at 120m axial depth. Current migration patterns suggest it extends northwards, but the more conductive material is not to distant from the hole.

Hole T93-18A low to moderate conductance anomaly at 100m depth, about 50m

radially above and to the south of the hole.

Preliminary Interpretation Report S*

Summary:The majority of the conductors found lie above the holes. The

exception is that of T93-10 on the Doyle Lake grid. Most anomalies have high conductances and occur as multiple conductors. The superposition of these conductors distorts the resultant sections, thus giving erroneous (or suspect) distance estimates (generally too high). However, direction data is consistent in all cases. With multiple conductors and shallow hole depths, distant anomalies are hard to discern since the in-hole intersections greatly mask the more subtle and longer wavelength responses.

A complete report with more indepth discussion of some of the peculiar responses can be provided if so desired. In such case, geologi: information and the IP interpretation could be used in conjunction with this data to give a more complete interpretation of the region. However, this report does give the essential raw interpretation of the collected data.

Sincerely,

Ken Nurse Geophysicist

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Scale: 1:2500 Unit Scale: lcm ^ 10 nT/s-BO

- 190m 1 1 97m


ClientGridDate

Scale: 1:2500-se

BORE HOLE





c 193m

CRONE GEOPHYSICS k EXPLORATION LTDBOREHOIL-E

Client Grid Date

Data

Scale: 1:2500-80 -66

10rr,

^40!•50m- 60m70m

90m- 100m •110m

: 130m - 140m

- 160nr,170m

- 180m

: Tri Origin Exploration Hole : T93-18 : West Grid Tx Loop : 18-Collar : Sept 17, 1993 File name : TISXYJD.PEM

Corrected for Probe Rotation using Rotation Tool #1 X COMPONENT dBx/dt nanoTesla/sec - 20 channels

Unit Scale: lcm - 10 nT/s

-40 , -ee , jj9iSto± t ee ^ * 6e ^8e

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CRONE GEOPHYSICS St EXPLORATION LTDBOREHOLE

Client Grid Date

Data

Scale: 1:2500

-se -60

: Tri Origin Exploration Hole : T93-18 : West Grid Tx Loop : 18-Collar : Sept 17, 1993 File name : TISXY^.PEM

Corrected for Probe Rotation using Rotation Tool #1 Y COMPONENT dBy/dt nanoTesla/scc -20 channels

Unit Scale: lcm =

, - 4e , - B(? . 433iSII±. ^e M8 , ^ , ^10 nT/t

IBfti

36m 40m 50m

- 60m 70m 80m 90m

110m: 180m130m140m

160m 170m 180m


ClientGridDate

BORE H OIL, E




Scale 1:2500-80 -60


^j^-40 -80

^ 10 nT/s

10m

30m 40m

66m

70m

80m 90m 106m 116m 120m

f 130m

f !40m

180m

2. 15309RECEIVED

FEB 2 l 1994

MINING LANDS BRANCH

Appendix

Field Summary.Plan MapsSection Maps.Survey Data

Logarthmic Plots, Linear Plots.

.A-2 ,A-5 .A-7

.A-15

.A-49

Appendix A-

Appendix: Survey Summary

Survey :Date: September 9-18, 1993 Projects: Doyle Lake Grid

K.-!st Grid

Location: Batchawana , Ontario Canada

System Configuration:Survey Type: Borehole Pulse EM Transmitter Settings

Time base: 16.66 msecsRamp time: 1.5 msecsTransmitter: 2000W Crone PEM Transmitter

Receiver SettingsStacking: 512ZTS: 1530 usecsCoil Delay: 90 usecsReceiver: Crone Digital PEM Receiver (v4.00)

Cross Component Probe Derotation Method: Orientation Tool #1

GridHole T93-10:

Location: 10+63E/9+OOS Direction: 220 0 at -600 dip Surveyed Depth: 180m Surveyed Components: X Y Z

Loop 10-Collar:Size: 200m x 200mLocation: 10+OOE/12+OOE 8+OOS/10+OOSCurrent: 16 amp peak @ 76 voltsWire: 12 gauge wireGrid Azimuth: Base line at 130Y3100 True

Hole T93-11:Location: 12+88E/7+97S Direction: 2200 at -60 0 dip Surveyed Depth: 272m Surveyed Components : X Y Z

Loop 11-Collar:Size: 200m x 200mLocation: 11+OOE/13+OOE 6+50S/8+50SCurrent: 16 amp peak @ 76 voltsWire: 12 gauge wireGrid Azimuth: Base line at 130V3100 True

A-3

Hole T93-12:Location: 15+26E/8+50S Direction: 220 0 at -60 0 dip Surveyed Depth: 195m Surveyed Components : X Y Z

Loop 12-Collar:Size: 200m x 200mLocation: 14+OOE/16+OOE 7+OOS/9+OOS

Note: Does not use line 16+OOE but is paced and compassedacross .

Current: 16 amp peak @ 76 volts Wire: 12 gauge wire Grid Azimuth: Base line at 130Y3100 True

GridHole T93-14:

Location: 5+25E/9+OON Direction: 2500 at -650 dip Surveyed Depth: 190m Surveyed Components: X Y Z

Loop 14-Collar:Size: 200m x 200mLocation: 4+25E/6+25E 8+OON/10+OONCurrent: 16 amp peak @ 76 voltsWire: 12 gauge wireGrid Azimuth: Base line at 160Y3400 True

Hole T93-15:Location: 5+75E/6+10N Direction: 250 0 at -650 dip Surveyed Depth: 185m Surveyed Components : X Y Z

Loop 15-Collar:Size: 200m x 200mLocation: 4+75E/6+75E 5+OON/7+OONCurrent: 16 amp peak @ 76 voltsWire: 12 gauge wireGrid Azimuth: Base line at 160V3400 True

Hole T93-16:Location: 5+OOE/l+OOS Direction: 2500 at -650 dip Surveyed Depth: 197m Surveyed Components : X Y Z

Loop 16-Collar:Size: 200m x 200mLocation: 3+50E/5+50E 0+00/2+OOS

Appendix A-

Current: 16 amp peak @ 76 voltsWire: 12 gauge wireGrid Azimuth: Base line at 160Y3400 True

Hole T93-17:Location: 6+OOE/4+10N Direction: 250 0 at -60 0 dip Surveyed Depth: 197m Surveyed Components: X Y Z

Loop 17-Collar:Size: 200m x 200mLocation: 4+75E/6+75E 3+OON/5+OONCurrent: 16 amp peak @ 76 voltsWire: 12 gauge wireGrid Azimuth: Base line at 160Y3400 True

Hole T93-18:Location: 5+OOE/6+OOS Direction: 2500 at -650 dip Surveyed Depth: 185m Surveyed Components: X Y Z

Loop 18-Collar:Size: 200m x 200mLocation: 5+OOE/7+OOE 5+OOS/7+OOSCurrent: 16 amp peak @ 76 voltsWire: 12 gauge wireGrid Azimuth: Base line at 160V3400 True

Survey Crew;Operator: Ken Nurse, geophysicist Crew: Andrew Kamo, geological engineer

1000 E 1100 E 1200 E 1300 E 1400 E 1500 E 1600 E

000 S

700 S

800 S ——

900 S

1000 S——

1100 S

Tx Loop 11-Collar

Tr Loop 12-Collar

T93-12 Q

100m

l 198m

/

Scale 1:500060 O 60 100

(meters)

Tri Origin ExplorationDoyle Lake Grid

3-D Borehole Pulse EM Survey Borehole k Loop Location MapHoles: T93- 10.T93- 11 ,T93- 12

Survey Date: September 10-12, 1993

Crone Geophysics Se JExpioraifon Ltd.

500 L 000 f: 700 F 000 E

900 N — -

000 N

Tx Loop 14-Collar

T93-14

TOO N ——

f j 00 N

500 N

•J 00 N

300 N ——

Tx Loop 15-Coliar

T93-15

Tx Lcfcp 17-CoDar

e T93-l

200 N

100 N

100 S

Tx Loop le-Collar

,T9!-16

300 3

400 S ——

500 S

300 S

700 S

a avo om o

l

Tx/oop IB-Collar

T93-18

Scale 1:500050 il W [1)0


3-D Borehole Pulse EM Survey Borehole k Loop Location MapHoles: T93- 14.T93- 15.T93- 16

T93-17 and T93-18Survey Date: September 13-17, 1903

Crone Goophjrsdca A Exploration Ltd.

Ontario41N0BSE9781 2.15309 RUNNALLS 300

Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines

Geoscience Approvals Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: Fax:

(705) 670-5853 (705) 670-5863

March 18, 1994 Our File: 2.15309Transaction #: W9450.00002

Mining RecorderMinistry of Northern Developmentand Mines60 Church StreetSault Ste. Marie, OntarioP6A 3H3

Dear Sir/Madam:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS 1136262 ET AL IN RUNNALLS TOWNSHIP

The assessment work credits for Geophysics filed under Section 14 of the Mining Act Regulations have been approved as outlined in the original submission.

The approval date is March 10, 1994.

If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5855.

Yours sincerely,

GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

•fol/jl Enclosures:

cc: Resident GeologistSault Ste. Marie, Ontario

Assessment Files Library Toronto, Ontario

Ministry ofNorthern Developmentand Mines

Ontario

nation c

Report of Work Conducted After Recording Claim

Mining Act

TDOCUMENT No. W9*i 50 -* GQ&Q 3- '* * s/ -W ^ \*^

f 1 ' **.

eraonal Information collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about its collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mine*, Fourth Floor, 159 Cedar Street, iudbury, Ontario, P3E 6AS, telephone (70S) 670-7264.

nstructlons: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining

Recorder. O 1 (T O A- A separate copy of this form must be completed for each Work GroupM e JL O O v/- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

Recorded HoW*r(s)

IRLClient No.

TKAddress

IP*MlfwIQ DtVmOn

/By-Work Performed (Check One Work Group Only)

Work Group

X Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

B&re-Mo^ P^H Survey

L

"^RECEIV^rT"•^ *- * ij K J

rtB ^ I '994 .

SNG^ANDSGHA^^

' . ' ' i 1 j '

1 . .

Total Assessment Work Claimed on the Attached Statement of Costs l Z. 00

Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

ron4~ Woi \M~ltrA IV&

.7*7? GfiMcn fi J. L7fi1l^

J, S/*/

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

l certify that at the time the work was performed, the claim* covered In this work report were recorded In the current holder'* name or held under a beneficial Interest by the current recorded holder.

Date

k* 17, HWRecorded Holder or Agent (

Certification of Work Report

For Office Use OnlyTotal Value Cr. Recorded (bat* Recorded

Notice for Amendments Sent

l certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after Its completion and annexed report is true.

Name and Address of Person Certifying

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Ontario


i duament du Nord

el des mines

Statement of Costs for Assessment Creditttat des coQts aux fins du credit d'evaluationMining Act/lol aur lea mlnea

m0600^

Personal Information collected on thlt form Is obtained under the authority of the Mining Act. Thlt Information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed lo the Provincial Manager. Minings Lands. Ministry of Northern

nent and Mines, 4th Floor. 159 Cedar Street, Sudbury, OntarioP3E 6A5, telephone (705) 670-7264.

Les renselgnements personnels contenus dans la presente formula sont recuelllls en vertu de la Lot aur lea mines et sen/Irani a tenlr s. (our un regjstre des concessions mlnleres. Adresser toute queslton sur la collece de ces renselgnements au chef provincial des terrains mlnlers, mlnlstere du Devetoppement du Nord et des Mines, 159, rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Dlrtct Coeta/CoOts directs

Type

WagesSalalrea

Contractor's and Consultant's Fees Droltade ('entrepreneur et de I'expert- eonaeH

Supplies Used Foumtturea uUllaeea

Equipment Rental Location de materiel

Description

Labour Maln-d'oeuvreField Supervision Supervision sur le terrain

TyS-^? N^*'*2"t h rf SurtALj

1

Type

Type

Amount Montan!

\cnoaJ/^ô

Total Direct Costa Total des coOts directs

Totals Total global

lw***

/U35to

iwrtjt

2. Indirect Coata/CoQta Indlrecta* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour to remboursement des Iravaux de rehabilitation, tos coats Indlrects ne sont pas admlsslbles en (ant que travaux d'evaluation.

Type

Transportation Transport

Food andLodging Nourriture ethebergementMobilization and Demobilization Mobilisation et demobilisation

Amount Allowable ( Montan! admissibleTotal Value of Asse (Total of Direct and A Indirect eotts)

DescriptionType

P If C*" * i O .

RECEIVE

FEB 2 1 ;99.

MINING LANnnm^

Amount Montan!

^ f\ J-i OS

•"••^••i

jfiH ' 7.0iSub Total of Indirect Costa

Total partial daa couta Indlrectanot greater than 20H of Din (n'excedant pas 20 H des t• ••••AlftA ^dbjMA \tmtmttm tdktA

llowaMe d svatuatM (TeUdMM

set Costa) wOta directs)leducrMHn AMdbMto

Totals Total global

)

i&fwoWo7,W

100*7.0?

W/kcoM hdm

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification Is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des coOts dans tes 30 jours sulvant une demande a eel effet. Si la verification n'est pas effectuee, le mlnistre pout rejeter tout ou une partie des travaux d'evaluation presentee.

Filing Discounts

1. Work filed within two years of completion Is claimed at 10046 of the above Total Value of Assessment Credit.

Remises pour depot

1. Les travaux deposes dans tos deux ans sulvant tour achievement sont rerrtxwreesalOOô^lavaleorlotalesusmemîrô^creoltd'evahîon.

2. Work filed three, four or five years after completion Is claimed at 504b of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment CredK Total Assessment Clairnedx 0.50

2. Les travaux deposes trois. quatre ou cinq ana apres tour achevement sont rembourses a 50 tt de la valeur totale du credit d'evaluation susmentkmne. Volr tos calculs d-dessous.

Vtleur totale du credit d'evaluationx 0,50

Evaluation totale demand**

Certification Verifying Statement of Coat*

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that M -*(Recorded Holder, Ag*nt, Potit^h In Comparfy)

to make this certification

Attestation de I'ttat dea coOta

J'atteste par la presente :quo les montants Indiques sont le plus exact possible et que ces depenses ont ete engagers poUr effectuer les travaux d'evaluation sur les terrains Indiques dans la formula de rapport de travail cl-)olnt.

Et qu'a litre de . le suls autorlse(Ututelr* *nr*gtetre, r*pr***nUnt. poM* occup* dans la oornpsgnl*)

i falre cette attestation.

Noli : Dint can* formul*. loriqu'll d*ilgn* d** p*rtonn*s. l* masculln *tt utlll** lu t*nt n*utr*.

41N0HSE9701 2.15309 RUNNALLS

Ministry ofNaturalResources


Ontario

INDEX TO LAND DISPOSITION

PLAN

G-2420TOWNSHIP

RUNNALLS

RECEIVED

FEB 2 11994

MINING LANDS BRANCH

M.N.fl. ADMINISTRATIVE DISTRICT

WAWAMINING DIVISION

SAULT STE. MARIEUNO TITLES/REGISTRY DIVISION

ALGOMA

't

Scale 1:20 000

1000 1000 2600M*tr*s M*lr*t

10X10 1000 2000 3000 4000 5000 6000 7000 0000 WOO 10000fMt

Contour Interval 1 0 Metre*

AREAS WITHDRAWN FROM DISPOSITIONMRO- Mining Rights OnlySRO- Surface Rights Only *M 4- S - Mining and Surface Rights ' \

SYMBOLS Description Order No. Data Disposttlon

BoundaryTownship, Meridian, Baseline.

Road allowance; surveyed shoreline

Lot/Concession; surveyed, unsurveyed

Parcel; surveyedunsurveyed

Right-of-way; roadrailway utility

Reservation

Cliff, Pit, Pile

Contour interpolated Approximate Depression......,..............

norizoniwj ............ ........,..... .......... LL±

Flooded land........................,............. i-c-^i-z-i-i-i-x-i

Mine head frame ................... .......................... H

Pipeline (above ground) ............................ —— ——

Railway; single Irack............................... -i——'———

\F'**

^ )

\

7 C•M

1

Si

double track abandoned.

Road; highway, county, township accesstrail,bush........,..,...

Shoreline (original).

Transmission line

Wooded area. \

y.

MSPOSmON OF CROWN LANDSPatent

Surface 4 Mining Rights Surface Rights Only Mining Rights Only.....

LeaseSurface ft Minin.i Rights Surface Rights Only Mining Rights Only.

B Q

Licence of Occupation

Order-in-Council

Cancelled

Reservation.

Sand A Gravel............

..T

.OC

THE INFORMATION THAT APPEARS ON THtS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD- DfTlONAt INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON

Th n. Ch

DATE OF JS8UE

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Map bM* and land diapositiot, diafting by Surveys and Mapping Branch, Ministry of Natural Resources.

The disposition of land, location of tot fabric and pare*! boundaries on this index was compiled for administrative purposes only.

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REPORT ON THE DRILLING AND THE BOREHOLE ......Report on the Drilling and the Borehole Geophysical...

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Transcript of REPORT ON THE DRILLING AND THE BOREHOLE ......Report on the Drilling and the Borehole Geophysical...