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碲锰铁矿（Kuranakhite）最早是1975年发现于俄罗斯南雅库特金矿床氧化带之中，之后国内外均未见报导。本文所述碲锰铅矿发现于陕西省洛南县驾鹿金矿床中，常呈不规则粒状集合体，粒径一般为0．05～0．25nm，浅褐色至棕褐色，半透明，条痕棕色，玻璃光泽，维氏硬度HV=231～438kg／mm2，摩氏硬度HM=4～5。实测密度6．72（2）g／m3。反射色呈蓝灰至浅蓝色，非均性中等，双反射弱，偏光色蓝至灰棕色，无内反射。折射率N=2.01，NB=1．98，Nr=1．96。6个电子深外平均成分PbO为45.40％，MnO2为1641％，TeO3为38．10％，总和99．91％；计算的化学式为Pb0.99M0.92Te1.06O6，简写为PbMnTeO6。X射线粉晶分析主要强线d（I），（hkl）为：0．341（100），（111）；0.2556（60），（130）；0．2043（50），（041）；0．1666（20），（310）；0.1598（40），（241）；0.1472（15），（330）。根据粉晶指标化求得该矿物为斜方晶系，可能的空间群为C，a=0．511（1）um，b=0．891（2）nm，c=0．532（1）nm，a：b=0．57，c：b=0.60；V=0.242（3）nm3，Z=2，Dx=6.66（l）g／cm3。
Kuranakhite was first discovered in the oxidation zone of the South Yakutia gold deposit in 1975 and has not been reported at home and abroad afterwards. The tellurium-manganese lead described in this article was found in the Jiaolu gold deposit of Luonan County, Shaanxi Province, often with irregular granular aggregates, with particle sizes generally ranging from 0.05 to 0.25 nm, light brown to tan, translucent, Mark brown, shiny glass, Vickers hardness HV = 231 ~ 438kg / mm2, Mohs hardness HM = 4 ~ 5. The measured density of 6.72 (2) g / m3. The reflected color is blue-gray to light blue, medium heterogeneity, double-reflection weak, polarized light blue to beige, no internal reflection. The refractive index N = 2.01, NB = 1.98, Nr = 1.96.6 The electronic deep average composition of PbO is 45.40%, MnO2 is 1641%, TeO3 is 38.10% and the sum is 99.91% Chemical formula is Pb0.99M0.92Te1.06O6, abbreviated as PbMnTeO6. X-ray powder analysis of the main strong line d (I), (hkl): 0.341 (100), (111); 0.2556 (60), (130); 0.2043 (50), .1666 (20), (310); 0.1598 (40), (241); 0.1472 (15), (330). The mineral is orthorhombic according to the index of powder crystalization. The possible space group is C, a = 0.511 (1) um, b = 0.891 (2) nm, c = nm, a = b = 0.57, c: b = 0.60; V = 0.242 (3) nm3, Z = 2 and Dx = 6.66 (1) g / cm3.