The
perthitic potassium feldspar occurs as subhedral to euhedral twinned crystals up to 1.
Lee MR, Parsons I (1995) Microtextural controls on weathering of
perthitic alkali feldspars.
6%) Microcline often intergrown graphically and are sometimes
perthitic with albite occurring as patchy perthite.
The main minerals in the sample are quartz,
perthitic orthoclase, plagioclase with sericite, epidote and chlorite.
Pocket zones are characterized by quartz crystals,
perthitic microcline, platy albite, orthoclase, biotite, lithium-iron micas and kaolinite.
The feldspar fraction is dominantly altered orthoclase feldspar and
perthitic ortho-clase feldspar with traces of microcline and plagioclase.
Lee MR, Parsons I (1995) Microtextural controls of weathering of
perthitic alkali feldspars.
Perthitic and myrmekitic intergrowths are observed in few sections.
Its amount increases abruptly close to the contacts of the anorthosites with silicic rocks, where
perthitic alkali feldspar partly replaces plagioclase.
Detailed field and petrographic studies reveal that Jura granitoids are megaporphyritic in nature containing phenocrysts of plagioclase and
perthitic feldspar.
Quartz (~ 30%) and
perthitic K-feldspar (~ 60%) with subordinate albite grains is the main constituent indicating the hypersolvus character, alkali amphiboles (Table 3) in the amount of around 10 % are the only mafites, mica minerals are practically absent.
The cavities are lined with euhedral crystals of smoky quartz, greenish
perthitic orthoclase .