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:

New model 205 decreptiometer

Studies of 6 Pegmatite deposits

A study of the Gejiu tin mine, China

A magnetite study - Bergslagen region, Sweden

Exploration using palaeo-hydrothermal fluids

Using opaque minerals to understand ore fluids

Decrepitation using Fe-oxide opaques

Understanding baro-acoustic decrepitation.

An introduction to fluid inclusions and mineral exploration applications.



 Interesting Conferences:


AAG 2017 at RFG2018, June 16-21 2018, Vancouver, Canada

IMA 2018, Melbourne Aust., Aug 13-17 2018

IAGOD, Salta Argentina, Aug. 28-31 2018

ACROFI-2018, Beijing, Sept. 11-17 2018

SEG, Keystone Colorado, Sept. 22-25 2018

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

-----2019-----

AOGS 2019 Singapore

ECROFI, June 24-26, Budapest, Hungary

SGA, Glasgow Scotland, Aug. 27-30 2019


Comprehensive Geology Conference Calendar


The BGS model 205 decrepitometer

March, July 2017

Because the model 105 decrepitometer operated on a PC computer with an ISA card slot (now superseded), the model 105 decrepitometer instrument has been redesigned and the software re-written to operate on a standard single-board Linux computer. This system uses the same furnace, sample tube assembly and power control unit as the model 105 instrument.

Although it operates in the same manner as the previous model 105, the software has been completely updated to be more convenient and has a full graphical interface, operating in the Xwindows environment. The temperature and counts are monitored and shown on screen during the analysis, and simultaneously plotted on screen as the temperature rises. The data is saved to a file upon completion, and the graphical plot can also be printed if required and easily regenerated from the saved data file for additional review.

The system now provides the complete computer as part of the instrument. It can be operated stand-alone with the addition of a monitor, keyboard and mouse, or operated remotely across a network using the included wired lan connector.  The computer and its interface electronics is in a compact 10 * 12 * 5 cm enclosure.

The computer and interface electronics unit.

decrepitometer 205 computer unit



The complete system includes the computer, furnace and enclosure, sample tube with detector and control electronics.

complete decrepitometer 205



This is a screen-capture of the model 205 instrument interface including the plot of a sample in progress.

model 205 instrument interface


The weighed sample is added to the sample tube, which is inserted into the furnace and the door of the enclosure is closed. The sample information and control settings are entered into the control window and the "GO" button is clicked. The entire analysis is then completed automatically without further user intervention. At the end temperature, the furnace is turned off and the control window re-appears to allow analysis of additional samples. The plot remains in view, with additional plot windows being created for additional samples. It is necessary to allow the furnace to cool before analysing subsequent samples.

Samples of 0.5gm are normally used while samples as small as 0.2 gm or up to 2 gm can be analysed according to the fluid inclusion abundance in the sample. The heating rate used is almost always 20ºC per minute, but the instrument can also be operated at 10ºC or 40ºC per minute. Analyses are usually performed on quartz samples, but other minerals containing fluid inclusions can also be used, such as carbonates, feldspars and opaque minerals such as haematite and magnetite. Sulphides can also be analysed, but they can be corrosive and this reduces the life of the temperature sensor. Quartz samples are usually analysed up to 620ºC because there is no activity above the alpha to beta phase transition at 573ºC, however the instrument can be used for analyses up to 800ºC.

The system can be installed in a normal quiet laboratory location as ambient sounds are suppressed. However loud sounds or vibration can interfere and should be avoided. Because it can be operated remotely across a network the room can be unoccupied during the analysis.

All the normal Linux operating system features are available including printing and gnuplot. Data can be exchanged either by using USB memory disks or across the network and the system can be accessed from microsoft computers using the SMB protocol. Network access from Apple systems has not been tested, but should be possible.

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