research papers
The crystal structures of two complex minerals of the lead sulfosalt type, sterryite, Cu(Ag,Cu)3Pb19(Sb,As)22(As–As)S56, and parasterryite, Ag4Pb20(Sb,As)24S58, were solved and compared according to modular analysis. These quasi-homeotypic structures are expanded derivatives of owyheeite, Ag3Pb10Sb11S28.