26 November 2021
Future Metals NL
("Future Metals" or the "Company")
Results of 2021 Annual General Meeting
The Board of Future Metals (ASX/AIM: FME), the platinum group metals ("PGM") exploration and development company, is pleased to announce in accordance, inter alia, with ASX Listing Rule 3.13.2 and Section 251AA of the Corporations Act, details of the results and proxies received in respect of its 2021 Annual General Meeting ("AGM") held earlier today.
All resolutions, as set out in the Notice of Annual General Meeting and associated Explanatory Statement dated 26 October 2021, were duly passed on a poll. The poll results and proxies received are available at the following link:
http://www.rns-pdf.londonstockexchange.com/rns/7284T_1-2021-11-26.pdf
For further information, please contact :
Future Metals NL |
+61 8 9480 0414 |
J ustin Tremain |
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Strand Hanson Limited (Nominated Adviser) |
+44 (0) 20 7409 3494 |
James Harris |
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W H Ireland Limited (UK Broker) Harry Ansell/Katy Mitchell |
+44 (0) 207 220 1670
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The information contained within this announcement is deemed by the Company to constitute inside information as stipulated under the Market Abuse Regulation (EU) No. 596/2014 as it forms part of United Kingdom domestic law pursuant to the European Union (Withdrawal) Act 2018, as amended ("MAR").
Notes to Editors :
About the Panton PGM Project
The Company's 100% owned Panton PGM project is located 60 kilometres north of the town of Halls Creek in the eastern Kimberly region of Western Australia, a tier one mining jurisdiction. The project is located on three granted mining licences and situated just one kilometre off the Great North Highway which accesses the Port of Wyndham.
The Panton PGM Project has a JORC Mineral Resource estimate of 14.32Mt @ 4.89g/t PGM, 0.31g/t Au, 0.27% Ni.
The Panton mineralisation occurs within a layered, differentiated mafic-ultramafic intrusion referred to as the Panton intrusive which is a 10km long and 3km wide, south-west plunging synclinal intrusion. PGM mineralisation is hosted within two stratiform chromite reefs, the Top and Middle reefs, within the ultramafic sequence.