摘要
铋钯碲镍矿是PtTe2－PdTe2－NiTe2矿物系的一个新变种矿物，发现于新疆喀拉通克铜镍矿床中。矿物化学成分式为（Ni，Pd）（Te．Bi）2，阴离子Te／（Te＋Bi）＝0．76（原子），反光显微镜下观察是白色，非均质性显著，反射率约为55％，摩式硬度略大于4。
Bismuthian palladian melonite is a new variety of the PtTe2-PdTe2-NiTe2 mineral series. This mineral was discovered in copper-nickel deposits in kalatongke, Xinjiang. The chemical formula is (Ni, Pd) (Te, Bi)2, and the atomic ratio Te/ (Te +Bi) = 0. 76. When observed under the reflecting microscope, the mineral is white in colour, and strong in anisotropism. The reflective index is 55%, HM≥4.
出处
《矿物学报》
CAS
CSCD
北大核心
1995年第2期150-153,共4页
Acta Mineralogica Sinica
关键词
铋钯碲镍矿
钯
碲
矿物
铜矿床
镍矿床
bismuthian palladian, melonite
new variety mineral
Xinjiang
kalatongke
