1) Tin in the deposits occurred mainly as cassiterite.

2) The tangerine and orange scheelite, bright black cassiterite, colourless and transparent board beryl occur in Pingwu, Sichuan Province.

3) Cassiterite - sulfide deposit of Tieshanping at Linwu, located in Xianghualing multi-metal mine, belongs to nervation tin-deposit of fracture-filled and replacement type.

4) They are the effective collecter of cassiterite slime, which proved that the flotation reagent isomerism principle is correct again.

5) Flotation, the election of joint processing cassiterite poly-sulfur mixed ore .

6) In addition to cassiterite and stannite, galena also contains a high amount of tin.

7) Biotite, titanite, cassiterite, rutile, wolframite, scheelite and wolframoixiolite are essentially useful minerals in clarifying the ore-forming potential of granites.

8) The land is rich in minerals such as gold,[http:///cassiterite.html] niobium and cassiterite.

9) If you are looking for a gem with a historic connection to England to proudly adorn your body, Cassiterite must surely be a first choice.

10) The results indicate that collector composed of SHA and P86 is suitable for the flotation of cassiterite ; the other composite collectors are not suitable for the flotation of cassiterite .

11) The flotation experimental results showed that methyl benzyl arsonic acid is an effective collector for wolframite and cassiterite slime.

12) Placer tin deposit in Xupu occurs in alluvial sediment of Quatemary SyStem and CaSSiterite chiefly concentrates at the bottom of Gravel layers.

13) It occurs chiefly as stannic oxide , SnO 2 in cassiterite.

14) This paper studies the collecting property and adsorption mechanism of salicylhydromie acid in cassiterite flotation.

15) One of the key problems in its origin is the solubility of cassiterite in granitic melt.

16) The results showed that copper occurs as chalcopyrite and enargite, tin occurs as cassiterite and custerite, and tungsten occurs as scheelite.

17) The constituents of six ore minerals, especially those of pyrites and cassiterite, are obviously controlled by temporal factors.