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Technical discussions
Using fluid inclusions in mineral exploration.
Main contents index
Other fluid inclusion methods and some useful links
Other topics
Viewpoints
Geo-Mathematical tools
GIS and GPS methods and tools

- Geochemical
exploration using hydro-thermal fluids
- An introduction
to fluid inclusions and their application in mineral
exploration
- Mineral exploration using fluid inclusion data - the Baro-acoustic decrepitation method
Other fluid inclusion methods and some useful links
Other topics
- Exploration of the Mt. Boppy Au deposit
region, Cobar, NSW, Australia: by K.G.McQueen
- Intrusion related gold at Okote, Southern
Ethiopia: by Solomon Geda
- Exploring
for
Au using fluid inclusions in the Tanami region, NT,
Australia: by T. Mernagh
- Gold exploration using baro-acoustic decrepitation
- Using Baro-acoustic decrepitation data in exploration at the Drake mineral field, NSW and the application of curve fitting to the decrepitation data
- Understanding
baro-acoustic decrepitation. The theorey explained.
Viewpoints
- Explaining the formation of CO2-only fluid inclusions
- Gold deposition from heterogeneous aqueous, CO2-rich fluids: resolving the enigmatic and misleading hypothesis of deposition from CO2 only fluids.
- Gas dominated inclusion assemblages may be trapped from aqueous dominated heterogeneous fluids by disproportional trapping
- Fluid inclusion
morphology can prove heterogeneous inclusion trapping of
pure CO2 inclusions.
- Do IOCG deposits form from
CO2-rich fluids?
- Why don't exploration geologists use or understand fluid inclusions? (a case study of a porphyry deposit at Cadia, NSW, Aust.)
Geo-Mathematical tools
GIS and GPS methods and tools
About this Website
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discussions relevant to fluid inclusion research or mineral
exploration methods are welcome for publication here.
Free use policy: All material on this website is released under either the Creative Commons (CC BY-NC-SA) or Copyleft policies.
Contacts
Author and maintainer
Free use policy: All material on this website is released under either the Creative Commons (CC BY-NC-SA) or Copyleft policies.
Contacts
Author and maintainer