Mica comes in a variety of forms and colors. The most common micas are biotite, which is dark colored, and muscovite, which is light in color.
Micas are monoclinic.
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.
the arrangement of the atoms in mica
The easiest minerals to recognize in a rock most times is Quartz, Feldsper and Micas.
Mica is a class of minerlas, not a rock. Different micas have different chemical compositions.
Micas are monoclinic.
Cynthia Micas is 165 cm.
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
Marble primarily consists of the mineral calcite, which is a crystalline form of calcium carbonate. It may also contain other minerals like dolomite, quartz, or micas. The characteristic veining and colors in marble come from impurities present during its formation.
Mica is a group of sheet silicate minerals (e.x of micas : Biotite, muscovite)
Minerals could include clays, feldspars, quartz, micas, and pyrite
The micas are used as dielectrics.