Applied mineral exploration methods, hydrothermal fluids, baro-acoustic decrepitation, CO2 rich fluids
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Gold at Okote, Ethiopia

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:

Kalgoorlie Au data

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.



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PACROFI 2020, Calgary Canada, May 18-20 2020

ACROFI 8,Townsville, Qld, Aust. June 16-18 2020

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Comprehensive Geology Conference Calendar


Relation of fluid inclusion geochemistry to wallrock alteration and lithogeochemical zonation at the Hollinger-McIntyre gold deposit, Timmins, Ontario, Canada

Ted J. Smith, Stephen E. Kesler
CIM Bulletin, April 1985, pp35-46.

ABSTRACT    (abbreviated)
Zonation patters are well developed in the mafic metavolcanic rocks that host epigenetic quartz-carbonate-gold vein mineralisation at the Hollinger-McIntyre deposit.

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Lithogeochemical zoning is equally well developed as variations in whole-rock abundances of As, Au, Ba, Rb and Sb.
As and Ba form the most useful zonation patterns, outlining individual ore zones as well as broader trends of mineralisation.

Gas chromatographic analyses of fluid inclusions in the quartz-carbonate veins indicate that the mineralising fluid was an H2O-CO2 mixture. Locally, CH4-rich fluid inclusions are associated with graphitic and/or carbonaceous wallrocks. Fluid inclusions in ore-bearing veins have higher CO2 contents than those in non-ore veins. Extensive sampling and analyses of the veins from the area surrounding the deposit reveals a well developed zonation of CO2 contents about the main zone of mineralisation. Low CO2 levels (1-2 mole%) in veins are peripheral to the deposit and increase to over 12 mole% in mineralised zones.

The observed zonation of the carbonate alteration assemblages is the result of CO2 addition to the wallrock, which is consistent with the zoning of CO2 in the fluid inclusions.

The zoning patterns delineated in this study are useful in exploration both on a deposit scale and on the scale of individual ore zones.

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FLUID INCLUSION ZONATION

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The amount of CO2 in the samples effectively distinguishes between ore and non-ore samples. In general, ore samples have group 1 (CO2 rich) compositions, whereas non-ore samples have group 2 (low CO2) compositions (Fig. 20)(below). With a cutoff value of 4% CO2 approximately 83% of the ore samples would be identified as anomalous. The distinction is not as accurate for the non-ore sample group where 64% of the samples have CO2 contents below 4 mole %.

co2 content histogram

CO2 levels in the fluid inclusions show distinct zoning relationships to the mineralisation. Figure 21 (below) shows contours of mole % CO2 for the surface vein-quartz samples. Low CO2 values of 1% to 2% surround the mine area and increase to values of over 12 % in the mineralised zones on the Hollinger property. It is interesting to note that high CO2 values show a good correlation with the distribution of the intensely carbonatised Assemblage IV rocks. Lower values tend to be found in veins in less altered rocks. Careful examination of the fluid inclusions shows that the high CO2 values observed in our analyses reflect actual CO2-rich compositions rather than contamination from carbonate minerals.

hollinger contours co2

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Application of Zoning to Exploration

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CO2 levels in fluid inclusions in quartz veins in areas peripheral to mineralised areas are low, less than 4 mole %, whereas values of 4 % and above are restricted to areas of ore-grade mineralisation. Samples with significant amounts of CH4 (greater than 2 mole %) are associated with wallrocks of graphite or carbonaceous material.The distinction in terms of CO2 content between ore and non-ore samples still holds for these graphite samples. Obviously this method can only be applied to rocks which contain quartz veins and is most useful in exploration on an ore-zone scale, in evaluating the gold potential of individual veins within a larger vein system.


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