v3.2.2 Update information

Version：3.2.8227.39346 （3.2.2.128）

Date：2022-7-11

Updated：

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1, Fixed a problem in v3.2.0 while using chemical potential as input for some components.

In V3.2.0, the algorithm was changed to achieve higher accuracy, but there is a problem while using chemical potential as input for some components. This problem was recently reported and has been fixed in the updated version.

v3.2.1 Update information

Version：3.2.8223.28415 （3.2.1.127）

Date：2022-7-7

Updated：

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1, Fixed an error in Miac(CHA) a-x model file

This error will make unexpected breakdowns while the Mica(CHA) moedl is used in v3.2.0.126.

v3.2.0 Update information

Version：3.2.8209.1032 （3.2.0.126）

Date：2022-6-22

Updated：

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1、The optimized algorithm improves the precision of results, The calculated curves of the phase diagram and isopleths are much smoother.

By further optimizing the algorithm, the precision of the calculated results is improved. The calculated curves of the phase diagram and isopleths are much smoother and can be comparable to THERMOCALC's results. The new version is sometimes 10 to 40% slower than the previous version.

Fig 1, The result from GeoPS v3.1

Fig 2, The result from GeoPS v3.2

2、The new version optimized the function of modeling the fractional crystallization of magma.

In the previous version, to achieve the function of separating all solids, it is necessary to add all possible solid phases as separated phases. In the new version, the keyword "Solid" can be used to refer to the Solid-phase, thus enabling the separation of all Solid phases.

Fig 3，The parameter setting of modelling magma crystallization

Fig 4，the result of fractional crystallization

Fig 5，The result of equilibrium crystallization

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