Defining a base metal mineral systems footprint in the Edmund Basin of the Capricorn Orogen, Western Australia

Heta Lampinen

doi:10.26182/5b6d0a4986fe6

Defining a base metal mineral systems footprint in the Edmund Basin of the Capricorn Orogen, Western Australia

Heta Lampinen

School of Earth and Oceans

Research output: Thesis › Doctoral Thesis

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Abstract

The polymetallic -1590 Ma Abra deposit is hosted within 1680-1450 Ma sediments and is concealed under thick weathered regolith. The deposit was investigated as a natural laboratory to define the size and geometry of multi-scale footprints associated with mineral systems. Deep crustal-scale basement structures beneath the deposit form a triple-junction that is overlain by a vertically zoned mineral footprint containing white mica, chlorite and carbonate. Hydrothermally altered overlying sediments indicate that deposit formed through sub-seafloor replacement. The mineral footprint of the deposit has been preserved through weathering and was mapped at the surface from ground-truthed remote sensing data.

Original language	English
Qualification	Doctor of Philosophy
Awarding Institution	The University of Western Australia
Supervisors/Advisors	Laukamp, Carsten, Supervisor Occhipinti, Sandra, Supervisor Fiorentini, Marco, Supervisor
Thesis sponsors	Australian Government Research Training Program
Award date	27 Jul 2018
DOIs	https://doi.org/10.26182/5b6d0a4986fe6
Publication status	Unpublished - 2018

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10.26182/5b6d0a4986fe6

THESIS - DOCTOR OF PHILOSOPHY - LAMPINEN Heta Maria - 2018
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Cite this

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title = "Defining a base metal mineral systems footprint in the Edmund Basin of the Capricorn Orogen, Western Australia",

abstract = "The polymetallic -1590 Ma Abra deposit is hosted within 1680-1450 Ma sediments and is concealed under thick weathered regolith. The deposit was investigated as a natural laboratory to define the size and geometry of multi-scale footprints associated with mineral systems. Deep crustal-scale basement structures beneath the deposit form a triple-junction that is overlain by a vertically zoned mineral footprint containing white mica, chlorite and carbonate. Hydrothermally altered overlying sediments indicate that deposit formed through sub-seafloor replacement. The mineral footprint of the deposit has been preserved through weathering and was mapped at the surface from ground-truthed remote sensing data. ",

keywords = "mineral footprint, reflectance spectra, mineral systems, weathering, sediment-hosted, hydrothermal alteration, base-metal deposit, crustal architecture",

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language = "English",

school = "The University of Western Australia",

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N2 - The polymetallic -1590 Ma Abra deposit is hosted within 1680-1450 Ma sediments and is concealed under thick weathered regolith. The deposit was investigated as a natural laboratory to define the size and geometry of multi-scale footprints associated with mineral systems. Deep crustal-scale basement structures beneath the deposit form a triple-junction that is overlain by a vertically zoned mineral footprint containing white mica, chlorite and carbonate. Hydrothermally altered overlying sediments indicate that deposit formed through sub-seafloor replacement. The mineral footprint of the deposit has been preserved through weathering and was mapped at the surface from ground-truthed remote sensing data.

AB - The polymetallic -1590 Ma Abra deposit is hosted within 1680-1450 Ma sediments and is concealed under thick weathered regolith. The deposit was investigated as a natural laboratory to define the size and geometry of multi-scale footprints associated with mineral systems. Deep crustal-scale basement structures beneath the deposit form a triple-junction that is overlain by a vertically zoned mineral footprint containing white mica, chlorite and carbonate. Hydrothermally altered overlying sediments indicate that deposit formed through sub-seafloor replacement. The mineral footprint of the deposit has been preserved through weathering and was mapped at the surface from ground-truthed remote sensing data.

KW - mineral footprint

KW - reflectance spectra

KW - mineral systems

KW - weathering

KW - sediment-hosted

KW - hydrothermal alteration

KW - base-metal deposit

KW - crustal architecture

U2 - 10.26182/5b6d0a4986fe6

DO - 10.26182/5b6d0a4986fe6

M3 - Doctoral Thesis

ER -

Defining a base metal mineral systems footprint in the Edmund Basin of the Capricorn Orogen, Western Australia

Abstract

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