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


Decrepitation data on pegmatites of the Massif Central, France


The pegmatites in the French Massif Central contain rare metals, tungsten, tin and uranium and have been extensively researched. In the past they have produced tin, tungsten and uranium, but at present they are actively mined for industrial minerals including clay.  A comprehensive summary of these deposits is in the field trip guide book for the 13th SGA meeting, Nancy, France, 2015.

Rare metal, W and U deposits and related granites from the NE French Massif Central.      by   Michel Cuney and Christian Marignac    2015  (155 pages)


Location

massif central within france location


massif central sample location map


Summary

A few of the quartz samples in this study show weak low temperature decrepitation near 270 C indicating the presence CO2 rich fluids, but such fluids seem to be of minor amounts. Other pegmatite deposits (eg Tanco, Canada) often show more prominent CO2 fluid contents. There are many variations in the quartz decrepitation features between 350 C and 550 C indicating multiple fluid events, but the significance of these events is not clear from this data.

The feldspar sample from the Beauvoir clay pit (2506D) is interesting as it shows that inclusions have been preserved in the feldspar and the weak low temperature decrepitation at 250 C shows that CO2 rich fluids were present during feldspar formation. Such CO2 rich fluids seem to have been less abundant during quartz formation at this same location.

Pegmatite samples from the French massif central show interesting variations over this large area, but they mostly lack CO2 rich fluids. It is not clear from this limited data if fluid inclusion decrepitation data correlates with economic mineralization or mineral exploration potential.


Results

Only rare centimetre-sized fragments of quartz were present at La Puelle quarry, present in late stage vugs. Both samples show significant low temperature decrepitation at 280 C, indicating the presence of CO2 rich fluids. But these fluids may post-date the main pegmatite crystallization event.

sample 2502

Quartz samples from the Margnac pegmatite also show distinct low temperature decrepitation near 250 C, due to CO2 rich fluids in the inclusions.
sample 2503

Samples from the Chabannes pegmatite lack low temperature decrepitation, indicating the absence of CO2 rich fluids.
sample 2504

Quartz from the Chedeville workings has no low temperature decrepitation peak and lacks CO2 rich fluids. There is only weak decrepitation in these samples -  the fluid inclusions are unusually small or rare.
sample 2505


At the Beauvoir clay mine pit, quartz contains trace amounts of Cassiterite. These samples also lack low temperature decrepitation and CO2 rich fluids. Sample 2506D was of feldspar, hence the decrepitation above 650 C. The feldspar contains a fluid inclusion population with a decrepitation temperature peak at 420 C, noticeably less than the co-existing quartz peak temperatures of 450 to 480 C. It seems odd that feldspar would form at a lower temperature than co-existing quartz, and this temperature probably does not accurately indicate the crystallization temperature of the feldspar.  Note that there is a small decrepitation peak at 250 C on the feldspar sample (mauve colour) indicating the presence of CO2 rich inclusions within the feldspar.

sample 2506


Eleven quartz samples from the Montebras clay mine pit (next 3 graphs) lack low temperature decrepitation and CO2 rich fluid inclusions. There are some interesting variations with dual decrepitation peaks at about 440 C and 490 C on 3 samples, 2507D, 2508C and 2509D suggesting that there were multiple quartz formation events.
sample 2507

sample 2508

sample 2509

Summary (back to top)

Sample descriptions

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