This project is located in the Upper East Region of Ghana, West Africa, and is at an advanced exploration stage. There is significant production from a number of gold mines in the region, as well as from numerous small artisanal workings. In 2018 the project had achieved a JORC Exploration Target of almost 300,000oz.
This project includes 4 contiguous exploration licenses totalling ~300km2 in central Tanzania. The main features are the NW-trending Chenene Hills of sheared granite within rolling plains formed mainly of eroded granitic soils. A belt of metamorphosed schists and quartz-feldspar gneiss rocks outcrops along the margins of the granites within the licenses, exposed intermittently above granitic soil plains. Pegmatites are hosted in these metamorphosed rocks of the Dodoma formation within the ‘Hombolo- Msangani belt’, a NW-SE trending belt approximately 35 km long and 13 km wide. Folding was later deformed by NW shearing. Pegmatites were emplaced prior to the shearing.
Lithium-bearing pegmatites have previously been locally identified in this metamorphic belt at Dulu, as well as in neighbouring areas to the other licenses.
In 2023 a first-pass surface sampling program identified a ~950m pegmatite with up to 1.08% Li2O.
The Soalara Eocene limestone deposit is laterally consistent, at/near surface, and located immediately adjacent to the old Soalara Port in the south‐west of the island of Madagascar, 28kms south of the Toliara port.
In September 2023 a JORC Mineral Resource Estimate of 440 Million tonnes of high purity limestone was confirmed. This MRE represents 97% weight calcium carbonate above a 95.3% CaCO3 cut-off, using a selective mining method.
This resource will soon likely enter scoping study phase with a view to identifying pathways to mining the resource.
Copyright © 2023 AUSTEC MKII PTY LTD - All Rights Reserved.
Powered by GoDaddy
We use cookies to analyze website traffic and optimize your website experience. By accepting our use of cookies, your data will be aggregated with all other user data.