[Extract] The formation of orogenic gold deposits is generally described as a complex interplay between deformation, permeability, rock strength and hydrothermal fluid pressure. Despite it being widely known that orogenic gold deposits form from low salinity, carbon dioxide-bearing fluids, the importance of this fluid composition in the context of the physical processes of deformation and fluid behaviour is commonly overlooked. In this study we combined fluid inclusion research with structural and numerical modeling in order to link these processes in the world class (10Moz.) Late Archean Sunrise Dam gold deposit
<div>Orogenic gold deposits contribute the majority of gold recovered globally throughout history. H...
The Boulder Lefroy-Golden Mile (BLF-GMF) fault system is the most intensely mineralized structure (>...
Gold mineralization at the Ballarat East deposit, central Victoria, Australia, is hosted in lodes th...
The Late Archean Sunrise Dam gold deposit (~10 Moz) is hosted within greenschist-facies rocks and is...
The hydrothermal fluids responsible for gold mineralization at the Ballarat East gold deposit (the s...
Deformation is intimately linked to fluid conditions in fault related ore systems such as orogenic g...
The Sunrise Dam Gold Mine is the largest gold deposit in the eastern part of the Yilgarn craton. In ...
Gold deposits in the Tanami and Kurundi-Kurinelli goldfields of the Northern Territory, Australia, h...
Fluid inclusion microthermometry, Raman spectroscopy and noble gas plus halogen geochemistry, comple...
The Telfer Au (+Cu) deposit is one of Australia's premier gold-producers, currently accounting for a...
Copyright © 2007 Society of Economic GeologistsSimilarities in mineralization and alteration style, ...
The Tanami Gold Mine (TGM) is situated 600km NW of Alice Springs in the Paleoproterozoic 'Granites-...
© 2012 Dr. Alison Maree FairmaidThe Ballarat East gold deposit (408t) is the second largest orogenic...
The Tropicana gold deposit is located adjacent to the margin of the Yilgarn craton in the Albany–Fra...
Orogenic gold deposits are comprised of complex quartz vein arrays that form as a result of fluid fl...
<div>Orogenic gold deposits contribute the majority of gold recovered globally throughout history. H...
The Boulder Lefroy-Golden Mile (BLF-GMF) fault system is the most intensely mineralized structure (>...
Gold mineralization at the Ballarat East deposit, central Victoria, Australia, is hosted in lodes th...
The Late Archean Sunrise Dam gold deposit (~10 Moz) is hosted within greenschist-facies rocks and is...
The hydrothermal fluids responsible for gold mineralization at the Ballarat East gold deposit (the s...
Deformation is intimately linked to fluid conditions in fault related ore systems such as orogenic g...
The Sunrise Dam Gold Mine is the largest gold deposit in the eastern part of the Yilgarn craton. In ...
Gold deposits in the Tanami and Kurundi-Kurinelli goldfields of the Northern Territory, Australia, h...
Fluid inclusion microthermometry, Raman spectroscopy and noble gas plus halogen geochemistry, comple...
The Telfer Au (+Cu) deposit is one of Australia's premier gold-producers, currently accounting for a...
Copyright © 2007 Society of Economic GeologistsSimilarities in mineralization and alteration style, ...
The Tanami Gold Mine (TGM) is situated 600km NW of Alice Springs in the Paleoproterozoic 'Granites-...
© 2012 Dr. Alison Maree FairmaidThe Ballarat East gold deposit (408t) is the second largest orogenic...
The Tropicana gold deposit is located adjacent to the margin of the Yilgarn craton in the Albany–Fra...
Orogenic gold deposits are comprised of complex quartz vein arrays that form as a result of fluid fl...
<div>Orogenic gold deposits contribute the majority of gold recovered globally throughout history. H...
The Boulder Lefroy-Golden Mile (BLF-GMF) fault system is the most intensely mineralized structure (>...
Gold mineralization at the Ballarat East deposit, central Victoria, Australia, is hosted in lodes th...