Christite, a New Thallium Mineral from the Carlin Gold Deposit, Nevada
American Mineralogist, Volume62, pages421425, 1977 Christite,a newthallium mineral from the Carlin golddeposit, Nevada ARruuRS. Rlorxn U.S. GeologicalSuruey, Menlo Park, California 94025 FnnNr W. Dlcrsor Departmentof Geology,Stanford Uniuersity St anfo rd, Cal ift rnia 9430 5 JoHNF. Slecr U.S. GeologicalSuruey, Reston, Virginia 22092 lNn KevtNL. Bnowx ChemistryDiuision, Diuision of Scientffic and IndustrialResearch, Petone, New Zealand Abstract Christite,TlHgAsSr, occurs with realgar,orpiment, and loranditein bariteveins and with realgar,lorandite, and getchellitein mineralizedcarbonaceous silty dolomite in the Carlin gold deposit,north-central Nevada. The mineralis namedfor Dr. CharlesL. Christof the U.S. GeologicalSurvey. The color is crimsonor deep red, but variesto bright orangein thinnerplates and crystals;the streakis bright orange,and the lusteris adamantine.The mineralis monoclinic,space group P2,/n,a -- 6.113(l),b = 16.188(4),c = 6.1Il(l) A, with0 : 96.71(2)',Z = 4, and cell volume: 600.6A8. Strongest X-ray powderdiffraction lines, in A, andtheir relative intensities are2.98 (10),3.62 (8),3.49 (6),2.692(6),2.216 (5),4.03 (6), and 3.36(5). Electronmicroprobe analyses gave Tl 35.2,Hg 35.1,As 13.1,S 16.6,sum 100.0 weight percent.The mineraloccurs in smallsubhedral to anhedralgrains which usuallylack well-developedforms but may showa bladedor flattenedhabit. Synthetic crystals are tabular, show{010) and {T0l}pinacoids, and {1l0} and {01l} prisms,and haveperfect {010}, excellent {ll0} and {001},and good {T0l} cleavages.Vickers hardness varied from 28.3-34.6and averaged31.5 kg mm-' (10 determinations).Density of syntheticTlHgAsSs is 6.2(2)(meas) and6.37g cm-e (calc).In reflectedlight christiteis grayish-whitewith a faint blue tint, lacks visiblebireflectance, is anisotropic,and has a brilliant red-orangeinternal reflection.
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