stannite उदाहरण वाक्य
उदाहरण वाक्य
- Cassiterite ( SnO 2 ) is the only commercially important source of tin, although small quantities of tin are recovered from complex sulfides such as stannite, cylindrite, franckeite, canfieldite, and teallite.
- It occurred in weathered material with colorless transparent cassiterite [ SnO 2 ], which is thought to have been derived from the oxidation of stannite [ Cu 2 ( Fe, Zn ) SnS 4 ].
- If alkali is added to a solution of SnCl 2, a white precipitate of hydrated tin ( II ) oxide forms initially; this then dissolves in excess base to form a stannite salt such as sodium stannite:
- If alkali is added to a solution of SnCl 2, a white precipitate of hydrated tin ( II ) oxide forms initially; this then dissolves in excess base to form a stannite salt such as sodium stannite:
- 85-90 % of tin is presented by cassiterite, mainly quartz associated and is concentrated in lower structural floor Jurassic sandstone and shale : Cassiterite in developed sulphide mineralization in upper floor of cretaceous volcanites is corroded by sulphides forming stannite and hydro-stannite .-showing vertical zonation in the distribution of mineral assemblages that form ore bodies.
- 85-90 % of tin is presented by cassiterite, mainly quartz associated and is concentrated in lower structural floor Jurassic sandstone and shale : Cassiterite in developed sulphide mineralization in upper floor of cretaceous volcanites is corroded by sulphides forming stannite and hydro-stannite .-showing vertical zonation in the distribution of mineral assemblages that form ore bodies.
- The most common minerals in ore-bearing associations of volcanogenic massive sulfide deposits deposits ( non-metamorphosed or oxidized ) and their modern analogues are pyrite, pyrrhotite, chalcopyrite, covellite, sphalerite, galena, tetrahedrite-tennantite, marcasite, realgar, orpiment, proustite-pyrargyrite, wurtzite, stannite ( carbonates ) quartz and native gold, and are differently distributed in the various associations schematized above.