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File Created: 03-Mar-2014 by Nicole Barlow (NB)
Last Edit:  17-Mar-2026 by Del Ferguson (DF)

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NMI
Name ADDIE 1 Mining Division Cariboo
BCGS Map 093A054
Status Showing NTS Map 093A11W
Latitude 052º 33' 37'' UTM 10 (NAD 83)
Longitude 121º 21' 39'' Northing 5824619
Easting 611115
Commodities Gold Deposit Types H05 : Epithermal Au-Ag: low sulphidation
Tectonic Belt Intermontane Terrane Quesnel, Kootenay
Capsule Geology

The ADDIE 1 showing is located 1.4 kilometres west-southwest of the south end of Spanish Lake and 5 kilometres north of Hobson Arm, Quesnel Lake, approximately 70 kilometres northeast of the city of Williams Lake and 14 kilometres southeast of Likely. Access is provided by paved road to the community of Likely from Williams Lake, with the remaining distance accessed by the Spanish Lake forestry roads.

Regionally, the area is underlain by Middle to Upper Triassic Nicola Group banded slates and tuffs of the Quesnel Terrane, with basaltic Upper Triassic Nicola volcanics to the west and Upper Proterozoic to Paleozoic Snowshoe Group metasediments to the northwest. To the east, the Eureka thrust fault marks a major tectonic boundary between the Intermontane and Omineca belts.

The Addie 1 occurrence is underlain by Upper Triassic to Middle Jurassic metasediment and volcanics. A strong southeast to northwest structural grain is thought to be an expression of the Spanish fault, which parallels the northern Eureka fault. The south flank of the Spanish Lake valley is dominated by the Spanish Lake anticline. North of this feature, stratigraphy is largely tuffaceous phyllite, argillite and subordinate associated sedimentary rock; to the south, a mixture of volcanic wacke, debris flows and serpentinite. The north side of Spanish Lake is largely underlain by graphitic pelite.

The mineralization style on the Addie 1 property is shale- or siltstone-hosted veins emplaced during regional metamorphic events. Sediment-hosted gold mineralization on the adjacent Spanish Mountain gold project (MINFILE 093A 043) occurs as disseminated mineralization throughout argillite, siltstone and greywacke and higher grade quartz veins in greywacke.

The area of principal interest is underlain by argillite, mudstone, siltstone, greywacke and conglomerate. These rocks have been weakly metamorphosed and complexly folded and faulted. Disseminated and vein-controlled gold mineralization occurs in all rock types, but is primarily concentrated in argillite units where they are cross-cut by a broad north trending structural corridor.

A 2011 diamond drilling program by Dajin Resources in the Addie 1 showing area exhibited scattered intervals of gold mineralization throughout, ranging from two metres to thirty metres in length, averaging from 0.10 to 0.14 gram per tonne gold (Assessment Report 36573). Drill holes AD1-2011-001, 002 and 005 returned near surface 21.2, 22 and 29.9 metre intercepts averaging 0.114, 0.108 and 0.116 gram per tonne gold, respectively.

WORK HISTORY

Gold exploration has been ongoing in the surrounding area since the Barkerville gold rush in the 1850s. In 1933, A. Bayley and F. Dickson discovered gold veins on the flank of Spanish Mountain; exploration interest has been consistent since that time. In 2005, Dajin Resources Corp. conducted a 51-sample stream sediment program that identified elevated gold and arsenic values (Assessment Report 28279).

Between April 1, 2006, and January 7, 2007, Dajin conducted an 83-sample stream sediment program that further identified elevated arsenic and gold values on the property. Transition metal enrichments and the occurrence of graphitic phyllite have suggested a possible platinum group metal occurrence (Assessment Report 28867). In 2007, a helicopter-borne magnetic and electromagnetic survey was flown on the property. Results suggest the southeastward extension of stratigraphy and structures associated with the adjacent Spanish Mountain gold occurrence (MINFILE 093A 043; Assessment Report 29424).

In 2009, Dajin conducted a 660-sample B-horizon soil program showing coincident gold, arsenic and molybdenum anomalies. Zinc, copper and chromium anomalies were found to have a broader and contrasting geographic distribution compared to gold. Slightly elevated platinum values were associated with gold, whereas palladium values were associated with zinc (Assessment Report 31186).

In August 2010, Dajin conducted a 920-sample B-horizon soil program, reinforcing and expanding the anomalous gold and arsenic zones (Assessment Report 31803). In 2011, Dajin conducted a soil sampling survey. Results of this survey reproduced known gold anomalies and showed that values increased with sample depth, suggesting stronger and more representative values could be present in areas where previous sampling was too shallow (Assessment Report 32576).

Also in 2011, Dajin Resources Corp. completed 12 NQ diamond drill holes, totalling 2484 metres, on the Spanish Lake property. Six holes were drilled on the south target area (Kangaroo 2 showing - Minfile 093A 306)) and six holes drilled approximately 1 kilometre north, in the Addie 1 occurrence area. In 2012, Dajin released results from their drill program targeting two geochemical and geophysical targets. The company planned to conduct further trenching, ground geophysics and structural mapping before their next drill program (Press Release, Dajin Resources Corp., April 27, 2012).

C.J. Greig re-evaluated the 2011 drill results and conducted more soil sampling in the southwest part of the property in 2016 with little encouragement (Assessment Report 36573). In 2018, C.J Greig and Evergold Corp. reviewed previous geophysical surveys. The production of 3D inversion models of the magnetics yielded several targets throughout the property, three of which are proximal to known mineralization discovered during historic work. The focus of the study was to identify areas of favourable carbonaceous sedimentary rocks where they are cut by north to northwest trending structures that may represent faults (Assessment Report 38121).

In 2019, Evergold Corp. conducted a soil program in the northeastern part of the property. Three discreet west-northwest trending gold ± arsenic ± molybdenum anomalies ranging from 1500 to 500 m in length were outlined southeast of the north 2011 geochemical drill target area. In 2024, the claims had reverted back to L. Addie who conducted programs of prospecting and rock sampling across the property south and west of Spanish Lake. The highest gold value in rocks sampled (130 parts per billion) was in the vicinity of the Kangaroo 2 showing (Assessment Report 42597).

Bibliography
EMPR BULL 97
EMPR GeoFile 2005-1
EMPR P 1990-3
EMPR PFD 520776, 681609
CJES 14, pp. 606-638; 25, pp. 1608-1617; 30, pp. 1262-1274
GAC Special P.45, pp. 433-482
GSC OF Map 920
PR REL Dajin Resources Corp., Apr. 27, 2012

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