What is an inclusion in geology ?
Inclusion : definition
A fluid inclusion is a cavity of often microscopic size (1 to 100 µm on average) within a mineral, but which can be exceptionally pluricentimetric, as in the halite crystal presented below or in the so-called quartz and amethysts "enhydro" or "bubble". These cavities can have the external shape of the host mineral, this is called a negative crystal. Fluid phases are usually salt water with CO2, sometimes H2S) sometimes accompanied by one or more solid phases. There are primary and secondary fluid inclusions, the former being contemporaneous with the crystallization of the host mineral while the latter are formed by healing of late fractures (of tectonic or other origin).