Schist (/ ˈʃɪst / SHIST) is a medium-grained metamorphic rock showing pronounced schistosity (named for the rock). This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates.

2023年8月26日 · Schist is a type of metamorphic rock characterized by its foliated texture, which means it possesses distinct layers or bands of minerals that have undergone significant physical and chemical changes due to heat, pressure, and other geological processes.

Schist is a foliated metamorphic rock made up of plate-shaped mineral grains that are large enough to see with an unaided eye. It usually forms on a continental side of a convergent plate boundary where sedimentary rocks, such as shales and mudstones, have been subjected to compressive forces, heat, and chemical activity.

schistose，英语单词，主要用作形容词，作形容词时译为“（变形岩石）片岩结构的”。 [1] The form of secondary minerals is schistose aggregated and spherical.次生矿物形态主要呈片状集合体和球状体。 Silver minerals in this mine mostly occurred as native silver embedded in quartz and shaPed into grained, schistose or tree-like structure.发现该矿银主要以自然银的形式存在，自然银多呈粒状、片状或树枝状嵌生在石英中。

Schist is a strongly foliated medium-grade metamorphic rock. It is characterized by an abundance of platy or elongated minerals (micas, chlorite, talc, graphite, amphiboles) in a preferred orientation. Varieties of this rock type share similarities in appearance (schistosity) but may be highly variable in composition.

Schist is a type of metamorphic rock known for its distinctive layered or banded appearance. This characteristic, called foliation. This foliation is caused by the alignment of platy minerals, such as mica, chlorite, and talc, being flattened and aligned due to …

Schistosity, mode of foliation that occurs in certain metamorphic rocks as a consequence of the parallel alignment of platy and lath-shaped mineral constituents. It reflects a considerable intensity of metamorphism—i.e., changes resulting from high temperatures, pressures, and.

Schist is a low- to medium-grade metamorphic rock with a well-defined foliation and containing minerals that are visible with the unaided eye. The name derives from the Greek schizo, ‘to tear’, in reference to its very strong fissility.

片状构造（schistose structure）是变质岩中最常见的一种构造。 岩石中片状或长条状矿物连续而平行排列，形成平行、密集纹理，矿物颗粒较粗，肉眼可以清楚识别的叫片状构造。

A schist is a medium- or coarse-grained metamorphic rock characterized by a parallel or subparallel arrangement of the constituent platy, fibrous, and prismatic minerals such as micas, chlorite, talc, certain amphiboles and other minerals.