
The fluid inclusion laboratory is supervised
by Dr. Virginia
Sisson, Assistant Professor
As minerals crystallize
in the presence of fluids, these fluids are trapped when the normal crystal
growth is interrupted. This occurs in the growth of all minerals, which
experience stresses or foreign objects which dislocate the plane of growth.
Disruption after the crystal has stopped growing can cause cracking, and
any surrounding fluids will then enter the cracks. In either case, the mineral
will grow around the fluid, sealing in the exact conditions of fluid entrapment,
i.e. composition and pressure-temperature conditions. Sizes of fluid inclusions
range from less than one micron to several centimeters. The optical equipment
in this laboratory allows us to observe those greater than 2 microns in
diameter, and those that are larger than 20 microns are extremely rare in
metamorphic rocks.
A heating-cooling
stage is used to bring the sample through a range of temperatures. Liquid
nitrogen is pumped through, allowing a minimum temperature between -180
and -190 degrees Celsius. A variable voltage source connected to a thermal
coil is the heat source, and a thermocouple is used to monitor temperature
to 0.1 degrees Celsius. As the sample is brought through temperature ranges,
groups of fluid inclusions are observed for phase changes. The type of phase
change is dependent on the fluid system and conditions of entrapment. Water
and NaCl systems trapped at low pressures will show melting of ice below
0° Celsius and a homogenization of the liquid and vapor phases to the
liquid phase above 70° Celsius. A H2O-CO2 system may show the formation
and disappearance of clathrate (a cage of CO2 around H2O) and separate melting
of CO2 and H2O. There are many other systems that are possible, including
hydrocarbons. Careful observation and documentation of the type and temperature
of such changes is necessary. Photomicrographs taken by a 35mm camera system
mounted to the microscope are useful for observation of complicated systems.
Current
research in the fluid inclusion lab includes
- Venezuelan eclogites and associated quartz boudins
- Mantle xenoliths from the Cascades Range
- Aqueous and hydrocarbon inclusions from Alaska
- eclogites from Oman
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Last Modified June
19,1997
by Rebecca Kessler
feel free to send questions or comments
kessler@owlnet.rice.edu