I do, if the question still stands. Only 2-5 kg of the stuff though.
i have a deposit of illite smectite . an am currently grinding it in small quantities. You can contact me at bellablueearth@yahoo.com
Feldspars commonly weather into clay minerals such as kaolinite, illite, and smectite through a process called hydrolysis. This conversion is facilitated by the breakdown of feldspar's aluminum-silicate framework by water and acids present in the environment.
Shale is primarily composed of clay minerals such as illite, kaolinite, and smectite, along with quartz, feldspar, and organic matter. It may also contain various accessory minerals depending on its specific geological history.
Illite is a clay mineral that typically has a fine-grained texture. It has a pale color, usually ranging from white to light gray, but can also be yellow or greenish. Illite has a layered structure with a sheet-like appearance, composed of individual crystalline plates. It exhibits a relatively low plasticity, meaning it does not easily mold or deform. Illite is known to have good water-holding capacity, making it useful for retaining moisture in soil.
The chemical weathering of feldspar produces clay minerals, such as kaolinite, illite, and smectite. This process involves the breakdown of the feldspar mineral structure through reactions with water and acids in the environment. As feldspar weathers, it releases elements like potassium, sodium, and silica, which contribute to the formation of new clay minerals.
Slate is mainly composed of the minerals quartz and muscovite or illite
coals minerals illite clay, pyrite, quartz, and calcite.
coals minerals illite clay, pyrite, quartz, and calcite.
Red clay generally consists of clay minerals like kaolinite, illite, and montmorillonite, along with iron oxides like hematite and goethite which give it its red color. It may also contain other minerals like quartz, feldspar, and various trace elements depending on its location. Additionally, red clay often contains organic matter and small amounts of water.
The most common end product of chemical weathering of feldspar is clay minerals such as kaolinite, illite, and smectite. These clay minerals form as a result of the alteration of feldspar minerals in the presence of water and atmospheric gases.
Green Illite clay can be purchased from www.mudderearth.net. You can also purchase it in EBay.
# Quarts # Feldspar # Mica # Pyroxine # Olivine # Amphibole # Calcite # Clay (eg Illite) # Garnet