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Consolidated Tin Mines Ltd.

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Summary

Project:

Einasleigh

Deposit:Chloe
Location:Australia
Commodities:Copper-Zinc-Lead-Gold-Silver
Date:2/12/2018
Report Code:JORC
Report Type:Exploration/Drilling Update
Project Stage:Pursuing Resource Increase/Upgrade
Report details:12-2-2018: Consolidated Tin Mines Ltd. announces an Exploration/Drilling Update report for its Chloe deposit at the Einasleigh project. Drilling results incl. 45.3m @ 6.13% Zn, 0.25% Cu, 2.16% Pb, 28.17g/t Ag from 373m. Consolidated Tin Mines Ltd (ASX: CS
Resources:(not mentioned in this report)
CP/QP:[Overall Report]: Max Tuesley (Internal)
ABSTRACT:Consolidated Tin Mines Ltd (ASX: CSD) (‘’CSD” or the “Company”) is pleased to report all assay results from the 2017 drilling programs have now been received. Standout results from the Chloe deposit are provided below. These new high-grade zinc-copperlead-silver results are from five diamond drill holes completed in late 2017 at the Company’s 100% owned Einasleigh Project located 250k south west of Cairns in north Queensland, and 140k south west of the Company’s wholly owned mineral processing mill at Mt Garnet. November 2017 step out drilling has now extended the strike and down dip potential of significant zinc mineralisation at the Chloe Prospect (Figure 1), with mineralisation open in all directions. The Chloe Prospect is situated within the Einasleigh Project on Exploration Permit for Minerals (EPM) 13072 held by Consolidated Tin Mines Limited (CSD) (Figure 2). The tenement area has historically received periodic exploration with a number of prospective targets yet to be adequately tested with bedrock drilling. As part of its focused exploration strategy CSD is growing Resources at Einasleigh and progressing the discovery of new standalone projects. The base metal deposits in the Einasleigh district, which includes the Chloe deposit, occur within the Proterozoic Georgetown Inlier. In an Australian context, several workers have drawn parallels between the Mt Isa, Broken Hill and Georgetown Inliers, in terms of sequences and mineralisation styles envisaging the “Diamantina Orogen”. In this theory, these Inliers were part of one geological terrane during sedimentation, orogenesis and at least some periods of mineralisation.

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