quartz or mica
No, schist is a metamorphic rock type characterized by strong foliation, while mica schist is a specific type of schist that contains a high proportion of mica minerals like muscovite or biotite. Mica schist has a distinct shiny appearance due to the abundance of mica minerals.
Slate is a low-grade metamorphic rock characterized by fine-grained foliated structure. Phyllite is intermediate-grade metamorphic rock with a greater degree of crystallization and foliation than slate. Schist is a medium-grade metamorphic rock with visible mineral grains and strong foliation. Gneiss is a high-grade metamorphic rock with distinct banding of light and dark minerals and high crystallization.
The strong parallel alignment of different mineral bands in a metamorphic rock is called foliation. Foliation is caused by differential stress during the rock's formation, resulting in minerals aligning perpendicular to the direction of stress to create distinct layers or bands. This alignment gives the rock a banded appearance and is a key characteristic used to classify metamorphic rocks.
The schists constitute a group of medium-grade metamorphic rocks, chiefly notable for the preponderance of lamellar minerals such as micas, chlorite, talc, hornblende, graphite, and others. Quartz often occurs in drawn-out grains to such an extent that a particular form called quartz schist is produced. By definition, schist contains more than 50% platy and elongated minerals, often finely interleaved with quartz and feldspar.
Schist is a metamorphic rock characterized by strong foliation, or preferred orientation of minerals, giving it a banded appearance. It forms from the metamorphism of various rock types under high temperature and pressure conditions deep within the Earth's crust. Schist is commonly used in construction and as a decorative stone due to its distinctive appearance.
The group of minerals that typically gives schist its strong foliation are the mica minerals, particularly biotite and muscovite. These minerals have a platy, sheet-like structure that aligns parallel to each other during the metamorphic process, resulting in the characteristic layered appearance of schist. Other minerals such as garnet and staurolite may also be present but contribute less to foliation compared to mica.
No, schist is a metamorphic rock type characterized by strong foliation, while mica schist is a specific type of schist that contains a high proportion of mica minerals like muscovite or biotite. Mica schist has a distinct shiny appearance due to the abundance of mica minerals.
Slate is a low-grade metamorphic rock characterized by fine-grained foliated structure. Phyllite is intermediate-grade metamorphic rock with a greater degree of crystallization and foliation than slate. Schist is a medium-grade metamorphic rock with visible mineral grains and strong foliation. Gneiss is a high-grade metamorphic rock with distinct banding of light and dark minerals and high crystallization.
The strong parallel alignment of different mineral bands in a metamorphic rock is called foliation. Foliation is caused by differential stress during the rock's formation, resulting in minerals aligning perpendicular to the direction of stress to create distinct layers or bands. This alignment gives the rock a banded appearance and is a key characteristic used to classify metamorphic rocks.
Schist is a metamorphic rock primarily composed of minerals such as mica, chlorite, talc, and amphibole. It forms from the metamorphism of other rocks like shale or slate, resulting in a foliated texture due to the parallel alignment of its mineral grains. Schist typically has a medium to coarse-grained texture and often exhibits shiny surfaces due to the presence of mica minerals.
SchistMedium- to coarse-grained, mica-bearing metamorphic rock with well-developed foliation (layered structure) termed schistosity. Schist is derived primarily from fine-grained, mica-bearing rocks such as shales and slates. The schistosity is formed by rotation, recrystallization, and new growth of mica; it is deformational in origin. The planar to wavy foliation is defined by the strong preferred orientation of platy minerals, primarily muscovite, biotite, and chlorite. The relatively large grain size of these minerals (up to centimeters) produces the characteristic strong reflection when light shines on the rock.For the source and more detailed information concerning this subject, click on the related links section (Answers.com) indicated below.
The schists constitute a group of medium-grade metamorphic rocks, chiefly notable for the preponderance of lamellar minerals such as micas, chlorite, talc, hornblende, graphite, and others. Quartz often occurs in drawn-out grains to such an extent that a particular form called quartz schist is produced. By definition, schist contains more than 50% platy and elongated minerals, often finely interleaved with quartz and feldspar.
Schist is a metamorphic rock characterized by strong foliation, or preferred orientation of minerals, giving it a banded appearance. It forms from the metamorphism of various rock types under high temperature and pressure conditions deep within the Earth's crust. Schist is commonly used in construction and as a decorative stone due to its distinctive appearance.
During metamorphism, minerals align perpendicular to the direction of maximum stress, which is known as foliation. This alignment results in a planar fabric within the rock, giving it a layered appearance. The degree of alignment can vary from a weak preferred orientation to a strong and well-developed foliation.
The property of foliation in gneiss, caused by its alternating layers of minerals, makes it resistant to weathering. This foliation gives gneiss a strong and cohesive structure, preventing the rock from easily breaking down in response to weathering processes.
Spar
Mineral acids are strong acids because they completely dissociate in solution to release a high concentration of H+ ions. This dissociation happens easily due to the strong bond between hydrogen and the acidic components in mineral acids, leading to a high degree of ionization and resulting in a low pKa value.