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Northstar Gold Corp.

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Summary

Project:

Miller

Deposit:Miller
Location:Canada
Commodities:Gold
Date:6/27/2019
Report Code:NI43-101
Report Type:Exploration/Drilling Update
Project Stage:Pursuing Resources Definition
Report details:27-6-2019: Northstar Gold Corp. announces an Exploration/Drilling Update report for its Miller deposit at the Miller project. Independent technical report for the Miller Gold Property. Ronacher McKenzie Geoscience ("Ronacher McKenzie") of Sudbury, Ontario
Resources:x
CP/QP:[Overall Report]: Trevor Boyd, Elisabeth Ronacher (Ronacher McKenzie Geoscience Inc.)
ABSTRACT:Ronacher McKenzie Geoscience ("Ronacher McKenzie") of Sudbury, Ontario, Canada was contracted by Northstar Gold Corp. (“Northstar”) to review the Miller Gold Property (the “Property”) located in the Catharine, Pacaud, Boston and McElroy Townships in northeastern Ontario and prepare an Independent Technical Report (the "Report"). The Report was prepared in accordance with the National Instrument 43- 101 – Standards of Disclosure for Mineral Projects (“NI 43-101”). The Property is located in the Larder Lake Mining Division of Northeastern Ontario, 18 km south of Kirkland Lake and 5 km east of the village of Boston Creek within the Catharine, Pacaud, Boston and McElroy Townships. The Property consists of 84 contiguous, unpatented claim cells covering approximately 1,100 ha in the Larder Lake Mining Division. All claims are 100% owned by Northstar. In addition, Northstar also holds two Freehold Patents L17916 and L17917 with both mining and surface rights in the northwest corner of Catharine Township, which are contiguous with the rest of the Property. Each patent has an area of 15.83 ha for a total of 31.67 ha. Surface rights for the mining claims are owned by the Crown, except for 11 SRO patents which are held by third parties. The Miller Gold Property is located within the Archean volcano sedimentary assemblage of rocks of the Western Abitibi Subprovince in the Superior Province. Metavolcanic rocks in the Property area of known age fall in the range of 2750 - 2700 Ma and are cut by an Algoman age granitic intrusion. Most of the metavolcanics are of the Catharine Assemblage, which consists of mafic to intermediate volcanic rocks, subordinate pyroxene komatiite and minor felsic metavolcanic rocks. Ultramafic and mafic to intermediate intrusive rocks occur as stocks and sills emplaced into the metavolcanic rocks. Relatively undeformed, younger alkaline to calc-alkaline felsic intrusive rocks were emplaced into the metavolcanic rocks as irregular stocks and dykes, which include the Allied, West Allied, Planet, and Meilleur syenite intrusions. These named ‘Syenite’ intrusions were U/Pb on zircon dated at 2662+- 18 Ma and are highly altered from the leaching of quartz and addition of Na. These intrusions are an important spatial component of the Miller Gold Property geology and the location of the gold mineralization. Lamprophyre dykes cut all other units.

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