GoldON Resources Ltd. announced the completion of its latest fieldwork program on its 100%-owned McInnes Lake property (the "Property"). The underexplored 12,598-hectare Property covers the majority of the McInnes Lake greenstone belt in northwestern Ontario. The exploration program focused on mapping and sampling of areas around previously identified fertile peraluminous granite plutons and derived exocontact pegmatites in two areas of the Mc innes Lake greenstone belt, McInnes North Pluton and the Lower Bay Pluton.

The goals of the fieldwork were to identify various phases of fertile granite plutons, verify rare metal mineralogy in the plutons and adjacent pegmatite dykes, and delineate potential lithium dispersion halos adjacent to fertile granite plutons. Detailed fieldwork and sampling covered a total of 50 square kilometres (km) and amassed 231 grab and channel saw bulk rock samples and 20 blocky K-feldspar separates to assess the degree of fractionation in the peraluminous pegmatitic granites. All samples have been submitted to analytical labs for rare metal chemistry.

Reference hand specimens from various localities are currently under petrographic investigation to verify rare metal mineralogy. In addition, four mineral identification separates were submitted to a commercial geoscience lab for X-Ray diffraction verification. Highlights of the field program include: Spodumene tentatively identified as green-black-altered, euhedral inclusions, up to 5 by 7 millimetres, hosted in blocky K-feldsPar in the westernmost exocontact pegmatite approximately 200 metres (m) east of the McInnes North Pluton.

This is similar to the altered spodumene observed in the Dryden and Georgia Lake pegmatite fields by GoldON's Technical Advisor, Frederick W. Breaks, PhD, PGeo. Peraluminous granites consist of potassic pegmatite, fine-grained leucogranite and pegmatitic leucogranite2 units and contain the following accessory minerals: deep orange, possible spessartine garnet, tourmaline, muscovite, biotite, possible white beryl, and fine-grained Ta-Nb oxides. Blocky K-feldspar samples, to assess the degree of rare metal potential, exhibit a variable degree of albitization that typically occurs late in pegmatite evolution via auto-metasomatism.

Veins and small masses rich in albite contain accessory muscovite, yellow-green sericite, biotite, red garnet, specks of black, non-magnetic, possible Ta-Nb oxide minerals and possible white beryl.