It is a low-temperature hydrothermal phase occurring in zeolite facies alteration of mafic rocks.
2.
The zeolite facies is generally considered to be transitional between orogenic regional metamorphism are not required.
3.
Generally plutonic and volcanic rocks are not greatly affected by zeolite facies metamorphism, although amygdaloidal texture.
4.
If the illite crystallinity is > 1.0, it corresponds with a metamorphic shallow diagenetic zone or zeolite facies.
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Zeolite facies metamorphism usually results in the production of low temperature clay minerals into higher temperature polymorphs such as kaolinite and vermiculite.
6.
Illite crystallinity can be used to trace the low grade metamorphic transition from zeolite facies to greenschist facies ( diagenetic zone to epizone ).
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Zeolite facies is considered to start with temperatures of approximately 50-150 �C and some burial is required, usually 1-5 km.
8.
If the illite crystallinity values fall in the 0.42-1.0 ?? range, it corresponds with a metamorphic deep diagenetic zone or zeolite facies.
9.
Zeolite facies is most often experienced by pelitic sediments; rocks rich in aluminium, silica, potassium and sodium, but generally low in iron, magnesium and calcium.
10.
As the rock enters the submetamorphic field, generally Zeolite facies metamorphism, clay minerals begin to recrystallize into low-temperature metamorphic phyllite minerals such as chlorite, prehnite, pumpellyite, glauconite and so forth.
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