THE STRUCTURE OF AMARILLITE
摘要
O, was discovered by H. Ungemach in the oxidation zone of sulfide deposit, coexisting with coquimbite in Tierra Amarilla, Chile in 1933. Only its chemical composition, density, crystal form and goniometric data （a: b: c=0.7757: 1: 1.1482, β=95°37′） were published. It was not until 1966 that LI Xi-lin et al. discovered it once again in the oxidation zone of Pb-Zn deposit in Qinghai Province, coexisting with sulfate minerals, and studied it mineralogically in detail.
引用本文（GB/T 7714）
李家驹, 周景良, 董卫. THE STRUCTURE OF AMARILLITE[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 1990.
引文网络
本站仅收录题录与摘要供学习参考，全文版权归属出版方；如有侵权请联系我们删除。