0 -- proses penghasilan kristak
the crystallization of soluble salts.
The intra-suite elemental variations can be best explained by fractional crystallization for reasons presented below.
Crustally-contaminated andesites could be produced by combined assimilation and fractional crystallization of basaltic magmas.
Crystallization proceeded to approximately the same stage in all orbicules, when the felsic shell started to form.
During crystallization of the orbicules, no mechanical transport of crystals out of the system can be proved.
The presence of quartz-filled microcracks in feldspar crystals suggests that deformation continued during cooling and crystallization.
Since the subsequent crystallization to form the orbicules only took place around discrete cores, all other pre-existing nuclei must have been removed.
In other cases parts of the structure (loops or domains) are removed during cloning to facilitate crystallization.
These glasses were formed respectively by over 75 % and 97 % fractional crystallization of basaltic liquid at low pressure.
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