Graphite schist is mainly composed of graphite, but can also contain other minerals, such as pyrite, depending on the sample
Graphite is a nonsilicate mineral composed primarily of carbon. It does not contain silicate minerals in its chemical composition.
The specific gravity of garnet schist can vary depending on the composition and density of the minerals present. On average, the specific gravity of garnet schist is around 2.7 to 3.2. However, it is recommended to measure the specific gravity of a specific sample to get an accurate value.
Graphite is a foliated metamorphic rock originating from Bituminous Coal.
Graphite can be found in all types of rock (igneous, metamorphic, and sedimentary). Although, it originates from igneous rocks, and is generally most economic in metamorphic rocks.
Schist typically begins as a metamorphic rock called shale, which is composed of clay and other fine-grained sedimentary minerals. Through the process of metamorphism, intense heat and pressure cause the minerals in the shale to recrystallize, forming the distinct foliated structure and mineral composition that characterize schist.
It is a medium-grade metamorphic rock with a preponderance of the platy mineral graphite.
it has a metallic luster usually silver and black :)
schist
The color of schist depends on its mineral composition. It can be gray, yellow, light or dark green, brown, or even black.
Graphite and Diamonds are both allotropes of Carbon.
Mica schist typically does not react with hydrochloric acid because the minerals in mica schist, such as mica and quartz, are generally chemically inert or resistant to acid dissolution. However, acid reactions can vary depending on the specific mineral composition of the schist.
Yes, graphite is commonly found in nature. It is a mineral form of carbon and can be found in rocks and ores, particularly in metamorphic rocks like marble and schist. Graphite is often mined and used for various applications, such as in pencils, lubricants, and batteries.
Both are foliated metamorphic rocks in which individual minerals can be seen with the naked eye. The difference is that gneiss is generally more coarsely crystalline and has color banding and schist smells bad.
Yes, schist is typically porous due to its layered composition of minerals. The porosity of schist can vary depending on the specific mineral content and the degree of metamorphism it has undergone.
Graphite is a nonsilicate mineral composed primarily of carbon. It does not contain silicate minerals in its chemical composition.
The specific gravity of garnet schist can vary depending on the composition and density of the minerals present. On average, the specific gravity of garnet schist is around 2.7 to 3.2. However, it is recommended to measure the specific gravity of a specific sample to get an accurate value.
Graphite is a foliated metamorphic rock originating from Bituminous Coal.