Applied mineral exploration methods, hydrothermal fluids, baro-acoustic decrepitation, CO2 rich fluids
Viewpoints:

How CO2 inclusions form from aqueous fluids

Understanding heterogeneous fluids : why gold is not transported in CO2 fluids

Gold-quartz deposits form from aqueous heterogeneous fluids: NOT from CO2 fluids

Inclusion shapes can prove heterogeneous FI trapping

Disproportional FI trapping from heterogeneous fluids explains gas-dominant systems

A discussion of H2 analysis by mass spectrometry

A mechanism to form H2 in the MS ioniser during analyses


News:

Sangan skarn Fe deposits, Iran

New model 205 decreptiometer

Studies of 6 Pegmatite deposits

A study of the Gejiu tin mine, China


Exploration using palaeo-hydrothermal fluids

Using opaque minerals to understand ore fluids


Understanding baro-acoustic decrepitation.

An introduction to fluid inclusions and mineral exploration applications.



 Interesting Conferences:


AGCC expo, Adelaide, Aust. Oct. 14-18 2018

-----2019-----

ECROFI, June 24-26, Budapest, Hungary

AOGS, Singapore, 28 Jul-2 Aug 2019

SGA, Glasgow Scotland, Aug. 27-30 2019


Comprehensive Geology Conference Calendar


Magnetite & Haematite


Magnetite and haematite both commonly give good decrepigrams and decrepitation is particularly useful to investigate these opaque minerals.

 Magnetite and haematite are often considered to be homogenous materials, but the decrepitation method reveals them to be quite variable. These variations can be used as an exploration tool and have also provided insight into the genesis of these deposits.
 

Tennant Creek Au & Cu mines, NT, Australia

 At the Tennant Creek mines, Au and Cu occur within massive magnetite/haematite/chlorite hosts, there being little or no quartz present. Intense decrepigrams are produced by both magnetite and haematite samples shown in the following 2 figures. For comparison, magnetite from the same BIF formation at Arltunga, some 500km away was analysed. This sample gave no decrepitation and it is inferred from this that the Tennant Creek deposits are hydrothermal rather than of sedimentary origin, counter to other widely adopted genetic models. In addition, the decrepitation of haematite suggests that this is a primary phase and not simply a weathering product derived from the magnetite as that would have destroyed any fluid inclusions.

Location map of Australian deposits



 
 

Upper Beaver mine, Ontario, Canada

 Similar mineralization to that at Tennant Creek occurs at the Upper Beaver mine, Ontario with Au in massive magnetite. Magnetite samples from 2 close mine shafts show strong decrepitation with substantial temperature variations. Samples from a bulldozer cut some 300m away gave no decrepitation and the results can be used to discriminate between potentially mineralized and barren magnetite.



 
 

Lyon magnetite skarn, Nevada, USA.

The Lyon deposit in Nevada is a magnetite skarn with low grade Cu and Au mineralization. Samples of magnetite from one of the exploration drillholes show widely varying decrepitation. This complexity within the magnetite is not apparent either from the core logging or chemical analyses.


 



 

Other magnetite skarns

Other magnetite skarns at Leadville, Colorado and Afton, British Columbia similarly show strong decrepitation in magnetite samples.



 

Comparison of various magnetite samples

Magnetite samples show a great range of variability, which can be used to discriminate between different types of magnetite and also to discern zonation within individual magnetite bodies. Note that the carbonatite samples show unusually low decrepitation temperatures, and the auriferous magnetites sampled to date frequently have higher decrepitation temperatures, with decrepitation  peaks being near 650o C.


 





 
 

Haematite Concentrates

Concentrates used in the steelmaking industry have also been analysed and decrepitation is being evaluated as a means of quality control of ore feed to concentrating plants.
 
 



 

Fresh and re-analysed magnetite


To confirm that the decrepitation sounds measured are not merely mechanical noises, this magnetite sample was analysed twice in succession. The second analysis (green) gave only background counts with a few counts from inclusions which just survived the first analysis at the 800 C cutoff temperature. This confirms that the counts being measured are the result of an irreversible phenomenae, such as inclusion decrepitation, rather than thermal expansion noises - which would be present in both analyses.


 
 
   

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