化學組成, 鍵及結構：(礦物)

不詳

Chemical composition, bonding and structure: (Mineral)

Unknown

原生物：(化石)

雲英岩是一種變質岩。由花崗岩類在高溫氣化熱液作用下經交代蝕變形成。呈灰白、灰綠、粉紅等色，具細、中粒鱗片狀變晶結構和塊狀構造。主要礦物成分為石英、雲母、黃玉、電氣石和螢石等，其次為綠柱石、石榴石、金紅石等。

Living Specimens: (Fossil)

Greisen is a metamorphic rock. By the granite under high temperature hydrothermal gasification formed by metasomatic alteration. It was gray, gray, pink and other colors, with fine, medium-grained crystal structure becomes scaly and massive structure. The main minerals are quartz, mica, topaz, tourmaline and fluorite, followed beryl, garnet, rutile.

雲英岩化的花崗岩擁有糖狀岩理，粒子大小平均1毫米。岩石主要含有石英及白雲母，令外表顯得閃爍而有光澤。雲英岩亦會因受帶有礦物質的熱溶液而變質，形成雲英岩化的花崗岩。

Greisenized have granite-like rock sugar processing, the average size of particle is 1 mm. Rock containing mainly quartz and muscovite, so the appearance looks flashing shiny. Greisen also due to the hot solution with minerals and metamorphic form greisenized granite.

雲英岩中的銣、銫具強烈的光電效應，在電子工業中用來製造各種光電設備及半導體材料。

Rubidium and cesium of greisen with a strong photoelectric effect, in the electronics industry for the manufacture of various optoelectronic devices and semiconductor materials.

此礦床分佈於中國、蘇、馬西亞、緬甸、英國和日本。

This deposit located in China, the Soviet Union, Macia, Myanmar, the United Kingdom and Japan.

雲英岩是一種變質岩，主要是由酸性侵入岩在高溫氣化熱液交代作用下而形成的岩石，主要由石英和白雲母組成，其中石英含量大於50%，雲母含量小於40%，此外尚有黃玉、電氣石、螢石、綠柱石等以及一些金屬礦物。

雲英岩主要發育在花崗岩體的頂部或邊緣，常伴生大量的稀有金屬礦物，包括鎢、錫、鉍、鉬、砷、鈹、鈮、鉭等。

Greisen is a metamorphic rock is dominated by acidic intrusive rocks at high temperature gasification hydrothermal metasomatism formed, composed mainly of quartz and muscovite, quartz content of which more than 50%, mica content of less than 40%, in addition to there are topaz, tourmaline, fluorite, beryl, etc. as well as some metal minerals.

Greisen mainly developed in the top or edge of the granite, often accompanied by a large number of rare raw minerals, including tungsten, tin, bismuth, molybdenum, arsenic, beryllium, niobium, and tantalum.