Schistosity is developed parallel to the axial plane of the folds.
2.
For coarser grained rocks, schistosity is used to describe secondary foliation.
3.
To qualify for the name a rock must also exhibit schistosity or some foliation or layering.
4.
Concomitant with the thrusts, a schistosity developed that affected the basement as well as the sedimentary cover implying an alpine origin.
5.
S1 schistosity is defined by hornblende and chlorite, and this mineralogical association suggests that the deformation occurred under upper greenschist to lower amphibolite facies conditions.
6.
In their geometrical arrangement, oblique foliations are somewhat similar to ( type I ) S-C-fabric, in which the elongated grain fabric becomes a true schistosity / foliation.
7.
Schistosity and gneissic banding ( the two main types of foliation ) are formed by directed pressure at elevated temperature, and to interstitial movement, or internal flow arranging the mineral particles while they are crystallizing in that directed pressure field.
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