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Cassiterite - Wikipedia

Cassiterite is a tin oxide mineral, SnO 2. It is generally opaque, but it is translucent in thin crystals. Its luster and multiple crystal faces produce a desirable gem. Cassiterite was the chief tin ore throughout ancient history and remains the most important source of tin today.

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Cassiterite - an overview | ScienceDirect Topics

Cassiterite (SnO 2) is the most important tin ore and it is typically found in veins closely associated with granite, in granite pegmatites and in greisen.The name is from the Greek kassiteros, tin.Cassiterite is tetragonal (space group P4 2 /mnm) and this structure has tin atoms at the corners and center of the unit cell (Fig. 9 A) with cell dimensions a 4.73, c 3.18 Å.

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Cassiterite - Mineral Properties - Used as an Ore of Tin - Geology

Cassiterite is a tin oxide mineral with a chemical composition of SnO 2. It is the most important source of tin, and most of the world's supply of tin is obtained by mining cassiterite. Small amounts of primary cassiterite are found in igneous and metamorphic rocks throughout the world. It is also a residual mineral found in soils and sediments.

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Cassiterita - Wikipédia, a enciclopédia livre

Cassiterita com muscovita. Cassiterita ( português brasileiro) ou cassiterite ( português europeu) é um dióxido natural e principal minério de estanho (SnO 2 ), de cor cinza, preta, vermelha, marrom, branca e amarela, ocorrendo na forma de cristais tetragonais. O nome provém do grego kassíteros (estanho) pelo latim cassitĕru- e francês ...

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Ognevka Ta deposit, Ulan, East Kazakhstan, Kazakhstan

Thoreaulite, Lithiotantite, Rankamaite, Cassiterite, Albite. Ognevka Ta deposit, Ulan, East Kazakhstan, Kazakhstan. Cleavage chip from a large monocrystal of yellow Thoreaulite with minor fragment of white Albite matrix. From outer parts the Thoreaulite is replaced by films of dark Cassiterite and brownish-pink Lithiotantite veinlets and pockets. In cleavage fissures and holes of Albite snow ...

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Highly fractionated Jurassic I-type granites and related tungsten ...

Cassiterite from the wolframite-bearing quartz vein and the drusy quartz vein yield the weighted mean ages of 164 ± 2 Ma and 160 ± 2 Ma, respectively. These ages suggest that both the granitic intrusion and related W-(Sn) mineralization in the Shirenzhang deposit were initiated during the late Jurassic (ca. 160 Ma). The Shirenzhang granitic rocks are weakly peraluminous highly fractionated I ...