No
It is important because silicate in feldspar help feldspar not to chip or break as easily. It helps it keeps it shape and the form. Silicate makes the color the color feldspar is when you look at it. Hope this helps
Yes, orthoclase is a silicate mineral. It is a common member of the feldspar mineral group and has a chemical composition that includes silicon and oxygen.
A sheet-like silicate structure refers to a mineral arrangement where silicate tetrahedra are stacked in a sheet-like fashion. Examples include minerals like mica and clay minerals, where the tetrahedra are arranged in continuous flat layers. These structures give the minerals their characteristic properties, such as cleavage and low hardness.
Quartz and feldspars are the most common silicate minerals of the crust.
Assuming you meant 'Feldspar' - it's a group of rock-forming silicate based minerals.
feldspar
Feldspar
Yes
It is important because silicate in feldspar help feldspar not to chip or break as easily. It helps it keeps it shape and the form. Silicate makes the color the color feldspar is when you look at it. Hope this helps
The simple answer is... Feldspar has a much higher complex and stable tetrahedral orientation in comparison to that of any other Silicate variation higher up on the reation series latter. Feldspar is one of the most stable variations in orientation of, what boils down to, silicate tetrahedra. Because Feldspar is technically a form of silicate tetrahedra orientation, I am assuming you are asking how the silicate tetrahedra orientations vary from its most simple (i.e. Olivine) to its mosts complex (i.e. quartz/FELDSPAR) forms. Esentially a Silicate Ion SiO4^-4 is the most basic building block of FELDSPAR. Knowing this, as you move from the top of Bowen's reaction series, we see a gradual stabilization of the various Silicate tetrahedral orientations. These orientations include (in order of stability/complexity): [TOP OF REACTION SERIES] Individual (Singular form) Silicate Tetrahedra (i.e. Olivine) Chain (Linear form) Silicate Tetrahedra (i.e. Pyroxine) Double Chain (Bilinear form) Silicate Tetrahedra (i.e. amphibole) Sheet Silicate Tetrahedra ('2-D' form) (i.e. Mica: Biotite or Muscovite) Framework Silicate Tetrahedra ('3-D' form) (i.e. FELDSPAR) [BOTTOM OF REACTION SERIES]
No. Feldspar is a silicate mineral.
Quartz, Feldspar, Muscovite, Biotite are among most common silicate minerals.
Quartz, feldspar or mica
Orthoclase is a common silicate mineral belonging to the feldspar group. It is a potassium aluminum silicate mineral. It is commonly found in igneous rocks and has a pink to white color.
Quartz, feldspar, mica, and pyroxene are common members of the silicate mineral family.
It is important because silicate in feldspar help feldspar not to chip or break as easily. It helps it keeps it shape and the form. Silicate makes the color the color feldspar is when you look at it. Hope this helps
Feldspar is a compound. It is a group of rock-forming tectosilicate minerals that are made up of aluminum, silicate, and potassium, sodium, or calcium ions.