Micas are monoclinic.
Cynthia Micas is 165 cm.
There are almost 40 different minerals in this group called micas, and their common characteristics are a) they are phyllosilicates, and b) they have perfect basal cleavage, and c) form monoclinic crystals. In the hand sample they are glittery and some are coloured. Have a crack at the article Micas in wikipedia.
Cynthia Micas was born on February 2, 1990, in Berlin, Germany.
Your question is unclear. Muscovite is not a group name, but there are a number of polytypes, as listed by Fleischer's Glossary, 2008: -2M1, -1M, , and -2M2. The micas are divided into three main subgroups: true micas, brittle micas, and interlayer-deficient micas. These total about 44 species. There are also six incompletely investigated micas that are now considered to be series.
phyllite is a type of metasedimentary rock. The parent rock likely contained clays and/or micas, which have metamorphosed into micas and aligned due to pressure. This shiny surface is produced by the alignment of the minerals.
The silicon-oxygen tetrahedral bonds in micas create a sheet structure with weak bonds between the sheets. This allows micas to cleave along these weak planes, resulting in their characteristic perfect basal cleavage.
The silicon-oxygen tetrahedra in micas are arranged in sheets, allowing for weak bonds between the layers. This layered structure is what gives micas their characteristic cleavage properties, as the weak bonds between the layers allow the mineral to easily split along parallel planes.
Platy minerals are micas(muscovite and biotite) and chlorite
Mica is a group of sheet silicate minerals (e.x of micas : Biotite, muscovite)
Minerals could include clays, feldspars, quartz, micas, and pyrite
The 'common' or rock-forming minerals, such as quartz, feldspars, micas, calcite, etc.