OK, OK.
I'm doing some checking ecat, trying to expand my knowledge and correct some misunderstandings in the process too perhaps.
This is from the IGO website. My bolding.
'The Tropicana and Salt Creek joint venture concession packages comprise approximately 3,200km2 and 2,300km2 of tenements respectively stretching over more than 250 kilometres in strike length along the Yilgarn Craton and Fraser Range Mobile Belt Collision Zone.
Tropicana lies to the west of a major tectonic suture between the Yilgarn Craton and the Proterozoic Albany-Fraser Province that stretches over 550km. The majority of the project covers tectonically reworked Archean rocks which form the eastern margin of the Yilgarn Craton. The regional geology is dominated by granitoid rocks, felsic to mafic paragneiss and orthogneiss, and felsic to ultramafic intrusive and volcano-sedimentary rocks. Tropicana is a rare example of a large gold deposit within high grade metamorphic rocks that have undergone widespread recrystallisation and melting.'
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- Ann: Appendix 3Y Ross Taylor - 30 June 2016-LSR.AX
OK, OK. I'm doing some checking ecat, trying to expand my...
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