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1966年在苏联公布研究资料。该矿物为钒铅钡铀矿含钡很高的变种。物理性质呈粉末、薄膜、皮壳状或和铁的氢氧化物及少量准铜铀云母组成致密的集合体。有时可见由小晶体(达2—5 mm)组成玫瑰花状堆积体。晶面夹角为76°和104°。解理
1966 in the Soviet Union published research data. This mineral is a high-barium-containing variant of vanadium-lead-barium-uranium deposits. The physical properties of powder, film, shell or iron hydroxide and a small amount of quasi-copper uranium mica compact assembly. Occasionally it can be seen that small crystals (up to 2-5 mm) consist of rose-like deposits. Crystal plane angle of 76 ° and 104 °. Cleavage