摘要
论述了锡氢化物的形成条件和物理化学特征。在岩浆和热液中 ,锡以锡氢化物、锡合金氢化物迁移至地壳浅部 ,锡氢化物、锡合金氢化物被氧化成锡氧化物、锡合金矿物 ,或与硫、硫化氢作用形成锡的硫化矿物。
Forming conditions and physical and chemical characteristics of tin hydride are discussed.Tin in magma and magmatic hydrothermal solution migrates as forms of tin hydride and tin alloy hydride to shallow crust level which,then are oxidized to tin oxide,tin alloy mineral or combine with S,H 2S,forming tin sulfides.
出处
《四川地质学报》
2001年第4期215-222,共8页
Acta Geologica Sichuan
