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

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


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


ECROFI, June 24-26, Budapest, Hungary

AOGS, Singapore, 28 Jul-2 Aug 2019

SGA, Glasgow Scotland, Aug. 27-30 2019

Comprehensive Geology Conference Calendar

East Kemptville Sn samples

Kingsley Burlinson
Burlinson Geochemical Services Pty. Ltd.
Darwin, NT, Australia

Samples collected in 1999 after mine closure. Limited access only to dumps and mined out pit face.


Run h1598.tb2, Sample 2001A, Semi transl coarse white qz with cassiterite
Run h1600.tb2, Sample 2001B, Semi transl. coarse white qz., equivalent to 2001C but larger lump
Run h1602.tb2, Sample 2001C, Semi transl. coarse white qz. Equiv to 2001B but smaller lump and clearer qz.


Run h1603.tb2, Sample 2002A, Semi transl. coarse grey-white qz. Eminor chlorite
Run h1604.tb2, Sample 2002B, Milky coarse grey-white qz. Equiv to 2002C
Run h1605.tb2, Sample 2002C, Milky & semi transl coarse grey-white qz. Equiv to 2002C