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Hydrothermal dolomite distribution in the Emanuel Range as a constraint on timing of fault movement during mineralisation on the Lennard Shelf, Western Australia

24/09/2021 by Thomas Brand

Hydrothermal dolomite distribution in the Emanuel Range as a constraint on timing of fault movement during mineralisation on the Lennard Shelf, Western Australia

 

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Publication Name: Australasian Exploration Geoscience Conference 2019

Authors: Heather Middleton*, Vicki Pedone, Dennis Arne

Date Published: September 2019

Number of Pages: 6

Abstract:

At least four petrographically, geochemically, temporally and spatially distinct dolomites have been identified in mid-late Devonian carbonate banks and reefal buildups of the Emanuel Range on the south eastern Lennard Shelf. Detailed mapping of the distinct dolomite bodies and their relationship to extensional faults and MVT-sulphide mineralisation has allowed the structural evolution of the southeastern Emanuel Range to be reconstructed providing constraints on the structural evolution of the range during oil migration and MVT mineralisation.

Tags: AEGC

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