Ontario Geological Survey
Permanent Link to this Record:
MDI52D16SE00004
| Record Name(s) | Rainy River ODM/17 Zone - 2010, 34 Zone - 1995, Rainy River Gold Project - 2005 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Producing Mine |
| Date Created | 2002-Jul-25 |
| Date Last Modified | 2023-Aug-03 |
| Created By | |
| Revised By |
Primary Commodities: Gold, Silver
Secondary Commodities: Zinc
Township or Area: Richardson
Latitude: 48° 50' 7.35" Longitude: -94° 0' 42.54"
UTM Zone: 15 Easting: 425750 Northing: 5409649 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52D16SE
Point Location Description: New Gold 2020 NI 43-101
Location Method: Data Compilation
1967: anomalous copper was noted in the region. Noranda registered claims and performed geophysics. 1971: Ministry of Natural Resources mapped the north-central part of the Rainy River Greenstone Belt. International Nickel Corp of Canada (INCO) undertook ground geophysics and drilled 2 DDH. 1972: Hudson’s Bay Exploration and Development (HBED) undertook airborne and ground geophysics. 1973: HBED drilled 54 DDH. Exploration was curtailed after insufficient encouragement. 1988: OGS map P3140 was produced, based on the interpretation of aeromagnetic data and geological mapping carried out by Johns. Mapping was supported by an OGS drill program, which resulted in the discovery of a gold-grains-in-till anomaly. Mingold Resources followed up on this anomaly and staked 85 claims and optioned patented lands. They did till sampling, including RC drilling, which gave inconclusive results. 1992: Nuinsco optioned patented lands from Western Troy Resources in September. 1993-1998: Nuinsco drilled a total of 597 widely-spaced RC drill boreholes. Nuinsco drilled a total of 217 DDH totalling 49,515 m. 1994: Nuinsco discovered the 17 Zone via core borehole. 1995: Nuinsco discovered the 34 Zone (Cu-Ni-PGE) followed by intensive diamond drilling.1997: Nuinsco discovered the 433 Zone, 500 m north of 17 Zone. 1999: Nuinsco conducted core drilling targeting the 34 Zone and a magnetic anomaly in Tait Township. 2000: Nuinsco conducted an audio magneto-telluric geophysical survey. Several targets were defined and drilled but these proved to be unmineralized. 2004: Nuinsco drilled 8 DDH totalling 1,549 m into the 34 Zone. 2005: Rainy River Resources completed the acquisition of a 100% interest in the project from Nuinsco in June. Rainy River relogged key sections of historical drill core, created a GIS database, conducted geological mapping, structural modelling and drilled more than 100 RC holes. In addition, 17 DDH were drilled, totalling 3,800 m. 2006: Rainy River drilled 121 DDH, totalling 55,219 m. Geotech Ltd was contracted to fly a Vtem airborne geophysical survey. Crone Geophysics & Exploration was contracted to conduct 3D borehole Pulse EM surveys. 2007: Rainy River drilled 179 DDH. JVX Ltd. was contracted to do an IP survey of 9 holes. Abitibi Geophysics was contracted to do ground gravity & EM surveys. 2008: Rainy River drilled 112 DDH totalling 59,719 m. Quantec Geophysics was contracted to do a Titan 24 survey. Fugro Airborne Surveys Corp. was contracted to do an airborne magnetic gradiometer survey. Preliminary pit slope design and waste management assessment was begun. amineral resource estimate was completed by Caracle Creek International Consulting. 2009: Rainy River drilled 124 DDH totalling 68,453 m. SGS Canada was contracted to begin preliminary metallurgical testing. SRKprepared a mineral resource statement incorporating information from an additional 112 core boreholes (59,719 m), drilled during 2008. 2010: Rainy River drilled 163 DDH totalling 84,648 m, discovering the Western Area mineralization approx. 800 m NW of the ODM/Beaver Pond mineralization. Environmental baseline studies were begun by Klohn Crippen Berger. SRK Consulting (Canada) Inc”) prepared a revised mineral resource statement to incorporate information from 124 core boreholes (68,453 m), drilled on the Project during 2009.2011: Rainy River drilled 157 DDH totalling 77,222 m. SRK updated the mineral resource statement to incorporate information from 163 core boreholes (84,648 m), drilled on the Project during 2010. A subsequent update, dated June 29, 2011, was prepared by SRK to consider additional drilling (50 boreholes, 26,509 m) completed on the Project between December 2010 and February 27, 2011. This resource update was the basis for the 2011 PEA. 2012-13: Rainy River drilled 225 DDH, totalling 77,969 m. 2013: Rainy River filed a feasibility study for the project. In October, New Gold acquired 100% ownership of Rainy River Resources. 2014-16: New Gold carr
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2.51035 | 20000007110 | 20000007110 |
| W9610.00056 | 52D16SE0001 | 52D16SE0001 |
| W9610.00140 | 52D16SE0011 | 52D16SE0011 |
| W9610.00092 | 52D16SE0008 | 52D16SE0008 |
| 2.15614 | 52C13SW0006 | 52C13SW0006 |
| 2.15372 | 52C13SW0005 | 52C13SW0005 |
| 2.18086 | 52C13SW0007 | 52C13SW0007 |
| 2.15685 | 52C13NW0016 | 52C13NW0016 |
| 2.15275 | 52C13SW9300 | 52C13SW9300 |
| 2.18381 | 52D16SE2003 | 52D16SE2003 |
| 2.18089 | 52D16SE2001 | 52D16SE2001 |
| W9610.00098 | 52D16SE0009 | 52D16SE0009 |
| 2.18085 | 52D16SE2002 | 52D16SE2002 |
| 2.47546 | 20000006185 | 20000006185 |
| 2.52859 | 20000007470 | 20000007470 |
| 2.51523 | 20000007345 | 20000007345 |
Province: Superior
Subprovince: Wabigoon
Belt: Rainy River
Geological Age: Archean
Feb 09, 2011 (C Ravnaas) - Gold and 34 Base Metal zones: The occurrence falls within the 2.7 Ga Rainy River Greenstone Belt which forms part of the Wabigoon Subprovince. The occurrence is centered on Richardson Township. To the north of Richardson Township lies the Sabaskong granitoid batholith. The Black Hawk Stock lies to the East of Richardson Township. A package of metasedimentary rock is found south of Richardson Township. Wedged in between these lithologies are a conformable series of tholeiitic mafic and overlying calc-alkalic intermediate to felsic metavolcanic rocks, striking almost east-west and dipping to the south. Intermediate rocks (dacites) host most of the Rainy River gold mineralization. Reference: Mineral Resource Estimate Technical Report completed by SRK Consulting for Rainy River Resources July 2009.
| Rock Type | Rank | Composition | Texture | Relationship | Intermediate Tuff-Breccia | 1 | Dacitic | Flows, Tuffs And Tuff-Breccia | Host |
|---|---|---|---|---|
| Mafic lava flow-unsubdivided | 2 | Qz-Ank Veins With Sphalerite | Hanging Wall Cap Unit | Host |
| Vein | 3 | Chalco_Galena | Late Remobilized | Host |
Feb 09, 2011 (C Ravnaas) - Gold Zone: Several mineralized zones have been delineated by exploration on the RRGP to date. Gold mineralization is found in the southern Cap Zone, the central ODM17, Beaver Pond and West Zones and the northern HS and 433 Zones. Recent studies suggest that there are at least two stages of gold mineralization within the RRGP, an early pervasive disseminated stage as well as a later stage of cross-cutting veinlets that often contain visible gold. Gold mineralization at the RRGP is hosted by pyrite-rich felsic metavolcanic and volcaniclastic rocks of dacitic composition, and by metasedimentary rocks; • The auriferous rocks are extensively altered, strongly depleted in sodium, and the primary minerals are replaced by secondary assemblages; • Gold and electrum occur as inclusions in pyrite, disseminated in sphalerite, in carbonates (ankerite) and in fine-grained silicates. The gold-bearing pyrite forms relict anhedral grains, whereas the gold-rich sphalerite are late-stage sulphides rimming and infilling fractures; • Gold mineralization took place during two separate episodes. An early episode is represented by the auriferous pyrite, and was probably contemporaneous with early silica and sericite alteration in the metasedimentary rock, and silica and clinozoisite alteration of the feldspars in the metavolcanic rocks. The circulating hydrothermal fluids that were enriched in iron, manganese, gold, silver and silica precipitated pyrite with gold/electrum, and amorphous silica with manganese; • Metamorphism resulted in the coarsening and recrystallization of quartz, crystallization of garnet, and the crystallization of metamorphic sericite. Subsequent brecciation and deformation of the partly metamorphosed, mineralized rocks resulted in the development of tectonic features such as fragmentation of pyrite, the release of gold and the development of tectonic fabrics such as augen texture, pressure shadows anastomosing and deformed sericite veins; • The “late” sphalerite had an important role in the reconcentration of primary gold into economic grade. Reference: Mineral Resource Estimate Technical Report completed by SRK Consulting for Rainy River Resources July 2009. 34 Base Metal Zone In 1995, drill hole NR-95-34 intersected massive and disseminated (net textured) Ni-Cu-PGE-Au- Ag-Co bearing sulphide within a chloritised, talcose, carbonatised, and locally serpentinised, maficultramafic (MUM) host. The irregular “tadpole shaped” MUM host is elongated along a NE-SW orientation (strike of 045°) and is discordant to local bedding. The body has been emplaced into the 17 Zone. The predominate rock type is composed of a melagabbro or pyroxenite containing 11-19 wt% MgO. The 34 Zone is a polymetallic zone of magmatic sulphides occurring as a series of lenses in depressions along the base of a late, tubular, maficultramafic intrusion. It comprises massive, net-textured and disseminated sulphides containing significant nickel, copper, PGE, silver, gold and cobalt. The host rock is unmetamorphosed but locally altered into serpentine and talc. The mafic-ultramafic intrusion crosscuts stratigraphy. The 34 Zone extends at least 350 metres along strike. The host intrusion is approximately 100 metres thick and plunges at twelve degrees to the west. The limits of The 34 Zone are poorly constrained owing to the discontinuous nature of the mineralization and a lack of drilling data. Reference: Exploration Summary Technical Report completed by Nuinsco Resources Ltd. December 2003.
Jan 29, 2019 (Therese Pettigrew) - The 34 Zone is hosted in a late-stage mafic-ultramafic intrusion, crosscutting the 17 Zone. The main lithological units include dunite, pyroxenite, pyroxene-gabbro, and gabbro. The lowermost units contain significant sulphide mineralization enriched in copper, nickel, gold, and platinum group metals (Kwong et al., 2018).
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 2 | Pyrite | Economic | Ore | ||||
| 3 | Sphalerite | Economic | Ore | ||||
| 4 | Silver | Economic | Ore | ||||
| 3 | Quartz | Economic | Gangue | ||||
| Sericite | Alteration | Sericitization | 1 | Extreme | Replacement | ||
| Chlorite | Alteration | Chloritic | 3 | Strong | Replacement |
Dec 22, 2014 (C Ravnaas) - Gold Zones: The lowest grade, disseminated gold mineralization is mostly associated with deformed volcaniclastic (permeable) dacites. Zones of higher gold mineralization are often associated with strong silicification and finely layered foliation-parallel sphalerite and pyrite. Visible gold is typically associated with narrow (<2 cm thick) quartz veinlets, narrow pyrite veins or a sphalerite/ pyrite-rich breccia matrix. Detailed mineralogy studies have revealed that gold and electrum occur as inclusions in pyrite or in close association with sphalerite, carbonates (ankerite) and fine-grained silicates. The gold-bearing pyrite occurs as relict, anhedral grains, whereas the goldrich sphalerite represents late-stage sulphides that formed rims on or infilled fractures in pyrite. Reference: Mineral Resource Estimate Technical Report completed by SRK Consulting for Rainy River Resources July 2009. 34 Base Metal Zone: At present, it is known to extend 350 m along strike with widths of >100m and a shallow plunge of about 12ºW along the trend of the MUM body. In the lowest part of the MUM, intercumulate sulphides (py, po, cpy) comprising up to 5%-15% of the mode occur. These sulphides are composed dominantly of pyrite and pyrrhotite, and in the thickest parts of the MUM, the progression may attain 35m. Weighted average grades are up to 0.2% nickel over 34.85 metres but individual assays may be considerably greater, e.g. 2.05% nickel (over 1.0m). To the east intercepts of sulphide are more complex; sulphide is more abundant where blebs of sulphide grade through intercumulate/net textured sulphide into a massive sulphide base. The interval over which sulphide occurs comprises a much higher proportion of the total MUM intercept (i.e. up to 70%) than in the west and the interval over which significant grades are obtained may attain thicknesses of 7 metres or more. FROM Rainy River Resources Ltd., press release, Oct. 10 2012.
Oct 30, 2020 (Therese Pettigrew) - The ODM/17 Zone is a series of east-west trending, south dipping lenticular sheets hosted within calc-alkaline dacites of the intermediate fragmental volcanic succession. The zone is cut by numerous NNE trending faults. The ODM/17 Zone has presently been defined over a strike extent of 1,600 m and to depths of 975 m. The true width of the zone is approximately 200 m. High-grade lenses plunge south-west (aligned with the L2 stretching lineation). Mineralization in the ODM/17 Zone is open below the modelled depth. Three styles of gold mineralization are observed in the ODM/17 Zone. Low grade intervals are characterized by tightly folded pyrite stringer veins and disseminated pyrite in sericite-quartz-chlorite altered host rocks. Moderate-grade intervals are characterized by tightly folded and foliation parallel pyrite-sphalerite and pyrite stringer veins, commonly associated with stronger silica and weak garnet alteration. High-grade gold mineralization is associated with deformed quartz-pyrite-gold veinlets that overprint other mineralization styles. The 34 Zone comprises magmatic nickel copper sulphide mineralization associated with precious metals (gold, platinum group metals) within a tubular, ~100 m thick, late-stage pyroxenite gabbro intrusion which cross cuts the ODM/17 Zone and post-dates the main gold mineralization event. The host pyroxenite-gabbro intrusion is unmetamorphosed, but locally altered into serpentine and talc. Magmatic sulphides vary from massive to net-textured and disseminated. Gold and silver mineralization occur within 5 to 50 m thick dislocated (and therefore discontinuous) north-east oriented pods over a strike length of 500 m with a down-dip plunge of 100 m (McCann et al., 2020). Zone 17 is contained within a northwest-trending shear zone which cuts quartz eye dacite. This zone has a strike length of 1km, is carbonatized and contains up to 5% py and trace chalcopyrite. DDH 97-06 intersected 37.8 m grading 3.4g/t with a 0.27 m section grading 2559 g/t Au. Four main styles of mineralization have been identified on the Rainy River gold project:1) moderately to strongly deformed, auriferous sulphide and quartz-sulphide stringers and veins in felsic quartz-phyric rocks (ODM/17, Beaver Pond, 433 and HS zones; 2) deformed quartz-ankerite-pyrite shear veins in mafic volcanic rocks (Cap / South Zone); 3) deformed sulphide-bearing quartz veinlets in dacitic tuffs/breccias hosting enriched silver grades; and 4) Cu-Ni-PGE mineralization hosted in a younger mafic-ultramafic intrusion (34 Zone) (SRK Technical Report, April 9, 2012).
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| Rainy River Mine | 2022 | Measured + Indicated Resource | 16931000 | NewGold MD&A Dec 31 2022 | 1,501,000 oz Au contained, 3,627,000 oz Ag contained | Gold 2.76 g/t, Silver 6.7 g/t |
| Rainy River Mine | 2022 | Proven + Probable Reserve | 60362000 | NewGold MD&A Dec 31 2022 | 2,493,000 oz Au contained, 6,176,000 oz Ag contained | Gold 1.28 g/t, Silver 3.2 g/t |
| Rainy River Mine | 2020 | Measured + Indicated Resource | 23127000 | 2020 NI 43-101 | 2.57 gpt Au and 6.90 gpt Ag for 1,915,000 oz Au and 5,120,000 oz Ag | Gold 2.57 g/t, Silver 6.9 g/t |
| Rainy River Mine | 2020 | Proven + Probable Reserve | 77572000 | 2020 NI 43-101 | Proven and Probable; 1.06 gpt Au and 2.50 gpt Ag for 2,636,000 oz Au and 6,266,000 oz Ag | Gold 1.06 g/t, Silver 2.50 g/t |
| Rainy River Mine | 2019 | Measured + Indicated Resource | 23127000 | 2020 NI 43-101 | 2.57 gpt Au and 6.9 gpt Ag for 1,914,000 oz Au and 5,120,000 oz Ag | Gold 2.57 g/t, Silver 6.9 g/t |
| Rainy River Mine | 2019 | Inferred Mineral Resource | 3479000 | 2020 NI 43-101 | 1.77 gpt Au and 2.4 gpt Ag for 198,000 oz Au and 268,000 oz Ag | Gold 1.77 g/t, Silver 2.4 g/t |
| Rainy River Gold | 2018 | Measured + Indicated Resource | 63109000 | 2018 NI 43-101 | 1.06 gpt Au and 3.8 gpt Ag for 2,142,000 oz Au and 7,651,000 oz Ag | Gold 1.06 g/t, Silver 3.8 g/t |
| Rainy River Gold | 2018 | Proven Mineral Reserve | 34189000 | 2018 NI 43-101 | 0.94 gpt Au and 2.3 gpt Ag for 1,031,000 oz Au and 2,516,000 oz Ag | Gold 0.94 g/t, Silver 2.3 g/t |
| Rainy River Gold | 2018 | Probable Mineral Reserve | 86263000 | 2018 NI 43-101 | 1.15 gpt Au and 3.6 gpt Ag for 3,189,000 oz Au and 9,882,000 oz Ag | Gold 1.15 g/t, Silver 3.6 g/t |
| Rainy River Gold - All Zones | 2014 | Measured + Indicated Resource | 177361000 | NI 43-101 Feb 14, 2014 | Grade 1.09 g/t Au and 2.57 g/t Ag for 6,236,000 oz Au and 47,635,000 oz Ag | Gold 1.09 g/t, Silver 2.57 g/t |
| Rainy River Gold | 2014 | Inferred Mineral Resource | 20655000 | NI 43-101 Feb 14, 2014 | Grade 1.16 g/t Au and 2.58 g/t Ag for 773,000 oz Au and 1,717,000 oz Ag | Gold 1.16 g/t, Silver 2.58 g/t |
| Rainy River Gold | 2014 | Measured + Indicated Resource | 81260000 | New Gold Summary of Mineral Reserve and Mineral Resource Estimates at Dec 31, 2014 | Grade 1.11 g/t Au and 3.8 g/t Ag for 2,896,000 oz Au and 9,999,000 oz Ag | Gold 1.11 g/t, Silver 3.8 g/t |
| Rainy River Gold | 2014 | Proven Mineral Reserve | 22682000 | New Gold Summary of Mineral Reserve and Mineral Resource Estimates at Dec 31, 2014 | 1.14 g/t Au and 1.9 g/t Ag for 830,000 oz Au and 1,370,000 oz Ag | Gold 1.14 g/t, Silver 1.9 g/t |
| Rainy River Gold | 2014 | Probable Mineral Reserve | 81594000 | New Gold Summary of Mineral Reserve and Mineral Resource Estimates at Dec 31, 2014 | 1.12 g/t Au and 3.1 g/t Ag for 2,942,000 oz Au and 8,040,000 oz Ag | Gold 1.12 g/t, Silver 3.1 g/t |
| 34 Nickel Zone | 2013 | Indicated Mineral Resource | 145000 | Hardie et al., Feasibility Study on Rainy River Deposit May, 2013 | Indicated Resource 43-101 Compliant: cut-off 0.35 g/t Au 145 000 t grading 0.66 g/t Au, 0.26 g/t Pt, 0.67 g/t Pd, 3,477 ppm Ni, 2,414 ppm Cu | Copper 2414 ppm, Gold 0.66 g/t, Nickel 3477 ppm, Palladium 0.67 g/t, Platinum 0.26 g/t |
| Year | Tonnes | Commodities | Reference | Comment |
|---|---|---|---|---|
| 2022 | 8535000 |
Gold 229822 Ounces |
NewGold MD&A Dec 31, 2022 https://s28.q4cdn.com/380852864/files/doc_financials/2022/q4/NGD-Q4-2022-MD-A.pdf | 0.91 g/t Au |
| 2021 | 14514000 |
Gold 234469 Ounces |
NewGold MD&A Dec 31, 2022 https://s28.q4cdn.com/380852864/files/doc_financials/2022/q4/NGD-Q4-2022-MD-A.pdf | 0.88 g/t Au |
| 2020 | 2367000 |
Gold 228919 Ounces |
New Gold Management’s Discussion and Analysis for 2020 | |
| 2019 | 6830000 |
Gold 253772 Ounces |
New Gold Management’s Discussion and Analysis for 2019 | |
| 2018 | 12296000 |
Silver 200000 Ounces Gold 227284 Ounces |
New Gold 2018 Financial Review | |
| 2017 | 1808000 |
Silver 40000 Ounces Gold 28509 Ounces |
New Gold 2018 Financial Review |
Map - Off Lake-Burditt Lake, Rainy River District
Publication Number: M2325 Scale: 1:63,360 Date: 1976
Author: Blackburn C.E.
Publisher Name: Ontario Division of Mines
Location:
Publication - Technical Report on the Rainy River Mine, Ontario, Canada
Publication Number: 2018 43-101 Date: 2018
Author: Kwong, N., Libera, M.D., Nussipakynova, D., Hampton, A.P., Sirait, B.
Publisher Name: New Gold Inc.
Location: SEDAR
Thesis - Physical Volcanology and Hydrothermal Alteration of the Rainy River Gold Project
Publication Number: MSc Thesis Date: 2011
Author: Wartman, Jakob M.
Publisher Name: University of Minnesota
Location: Kenora RGP
Map - Geological series, gold grains in rotasonic drill core and surface samples (1987-1988) Fort Frances-Rainy River area, District of Rainy River
Publication Number: P3140 Scale: 1:100,000 Date: 1988
Author: Bajc A.F.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 1999, Resident Geologist Program, Red Lake Regional Resident Geologist Report: Red Lake-Kenora Districts
Publication Number: OFR6003 Date: 2000
Author: Hinz P., Storey C.C., Gosselin S.D.M., Blackburn C.E., Kosloski L.
Publisher Name: Ontario Geological Survey
Location:
Thesis - Geologic and structural controls on ore style and distribution in the Archean Rainy River Gold deposit, Wabigoon Subprovince, Ontario
Publication Number: Date: 2016
Author: Pelletier, M., Mercier-Langevin, P., McNicoll, V.
Publisher Name: Institut national de la recherche scientifique, Quebec
Location:
Map - Emo area, District of Rainy River, Ontario
Publication Number: M1954-02 Scale: 1:63,360 Date: 1997
Author: Fletcher G.L., Irvine T.N.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Off Lake-Burditt Lake area, District of Rainy River
Publication Number: R140 Date: 1976
Author: Blackburn C.E.
Publisher Name: Ontario Division of Mines
Location:
Map - Rainy River sheet, District of Rainy River, geological compilation series
Publication Number: P0309 Scale: 1:126,720 Date: 1997
Author: Davies J.C.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Report of Activities 1997, Resident Geologists Program, Red Lake Regional Resident Geologist's Report: Red Lake-Kenora Districts
Publication Number: OFR5969 Date: 1998
Author: Blackburn C.E., Hinz P., Storey C.C., Kosloski L., Ravnaas C.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian geology, Rainy River area, District of Rainy River
Publication Number: P3110 Scale: 1:50,000 Date: 1988
Author: Johns G.W.
Publisher Name: Ontario Geological Survey
Location:
Publication - Rainy River Project, Exploration Summary and Mineral Resource Estimate for the #17 Zone
Publication Number: 2003 43-101 Date: 2003
Author: Mackie, B., Puritch, E., Jones, P.
Publisher Name: Nuinsco Resources Ltd.
Location:
Publication - Independent Technical Report for the Rainy River Property in North-Western Ontario, Canada
Publication Number: 2008 43-101 Date: 2008
Author: Caracle Creek International Consulting Inc.
Publisher Name: Rainy River Resources
Location: SEDAR
Publication - Mineral Resource Evaluation, Rainy River Gold Project, Western Ontario, Canada
Publication Number: 2011 43-101 Date: 2011
Author: SRK Consulting (Canada) Inc.
Publisher Name: Rainy River Resources
Location: SEDAR
Publication - Technical Report for the Rainy River Gold Project, Northwestern Ontario, Canada
Publication Number: 2012 43-101 Date: 2012
Author: SRK Consulting (Canada) Inc.
Publisher Name: Rainy River Resources
Location: http://www.newgold.com
Publication - NI 43-101, Feasibility Study of the Rainy River Project, Ontario, Canada
Publication Number: 2014 43-101 Date: 2014
Author: BBA Inc.
Publisher Name: New Gold
Location:
Publication - NI 43-101 Technical Report for the Rainy River Mine in Ontario, Canada
Publication Number: 2020 43-101 Date: 2020
Author: McCann, F., Smith, H., Molavi, M., Ross, A., Nussipakynova, D., Millar, A.
Publisher Name: New Gold Inc.
Location: SEDAR
Publication - New Gold In.c Management’s Discussion and Analysis for the Three Months Ended March 31, 2021, p.14
Publication Number: Date: 2021
Author: New Gold Inc.
Publisher Name: New Gold Inc.
Location: SEDAR
We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.
Please review our Terms of Use agreement for this data product.
For detailed information regarding this mineral record please contact the Kenora Resident Geologist District Office