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A re-examination of herzenbergite-teallite solid solution at temperatures between 300 700 deg C

机译:在300700摄氏度之间的温度下重新检查黑锌矿-陨石固溶体

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摘要

In order to investigate the range of the solid solution series in herzenbergite-teallite minerals, samples of different composition were synthesized. Herzenbergite-teallite minerals were synthesized by an evacuated silica glass tube method at 700 deg C. A linear relationship between cell dimensions, a, b and c and composition is established. Extension of solid solution to the Pb-rich portion of the system PbS-SnS is limited; the solid solution area is between Pb_(1.060)Sn_(0.940)S_2 and SnS at 700 deg C. Teallite coexisting with galena was also synthesized by hydrothermal recrystallization at 300, 400 and 450 deg C. The compositions of teallite are Pb_(1.140)Sn_(0.860)S_2 at 300 deg C, Pb_(1.114)Sn_(0.886)S_2 at 400 deg C, and Pb_(1.124)Sn_(0.876)S_2 at 450 deg C, respectively. Their compositions shift towards the PbS end-member form Stoichiometric teallite. The cell dimensions of teallite, which was synthesized hydrothermally, follow the linear relationship between cell dimensions and composition established at 700 deg C.
机译:为了研究黑锌矿-辉石矿物中固溶体系列的范围,合成了不同组成的样品。通过真空石英玻璃管法在700摄氏度下合成Herzenbergite-teallite矿物。建立了晶胞尺寸,a,b和c与组成之间的线性关系。固溶体向系统PbS-SnS的富Pb部分的扩展受到限制;固溶体面积在700℃时介于Pb_(1.060)Sn_(0.940)S_2和SnS之间。还通过在300、400和450℃下进行水热重结晶来合成与方铅矿共存的绿柱石。绿柱石的组成为Pb_(1.140) 300℃时的Sn_(0.860)S_2、400℃时的Pb_(1.114)Sn_(0.886)S_2和450℃时的Pb_(1.124)Sn_(0.876)S_2。它们的组成向化学计量的绿柱石方向转变为PbS末端成员。水热合成的小青石的泡孔尺寸遵循泡孔尺寸与在700摄氏度建立的成分之间的线性关系。

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