论文部分内容阅读
羟砷铅锌石产于个旧铅锌矿床氧化带,与其他氧化矿物伴生,该矿物呈淡黄色。比重5.67,摩氏硬度4.5—5,反射率11.5—11.6%,二轴(一),分子式PbZnAsO_4OH 1975年,我们在个旧松树脚氧化铅锌矿中发现了一种国内未曾发现的矿物,经分析其分子式为PbZnAsO_4OH。1982年10月,我国新矿物与矿物命名委员会以之作为新矿物报IMA审议。但IMA业已先通过了K.Paul发现的Arsendescloizite~1)(羟砷铅锌石),故我们丢失了发现权。 现将我国产出的羟砷铅锌石的研究结果报道如下:
Hydroxynaphrite is produced in the oxidation zone of Gejiu lead-zinc deposit and is associated with other oxidized minerals, which are pale yellow. Specific gravity 5.67, Mohs hardness 4.5-5, reflectivity 11.5-11.6%, two axes (a), molecular formula PbZnAsO_4OH 1975, we found a non-domestic found in the Gejiu pine foot lead zinc ore minerals, the analysis The formula is PbZnAsO_4OH. In 1982 October, China’s new mineral and mineral naming committee as the new mineral reported IMA review. However, IMA has already passed the Arsendescloizite ~ 1 (K.) found by K. Paul, so we lost the right to discovery. The results of our study on hydroxyl arsenic, lead, and zinc are now reported as follows: