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The high Zn content stabilises the sphalerite-type structure of the mineral.",[18,19,20],"Fe","Zn","S",[18,20],[23],"APPROVED",2005,2008,"2","C","B","05a","8","7","Isometric",30,208,"0","5.426",2,"Xenomorphic grains, 5–150 µm in cross section, their segregations filling interstices between the crystals  and grains of adjacent minerals in the matrix of chondrite. Lamellar.","313","383",20,"3.79","Resinous,Sub-Metallic","Brown-black","Black",[47,48],"black","brown",[48,47],"brittle","Gray with distinct brownish tint","None","Isotropic","(19.5) 400,\r\n(19.5) 440,\r\n(19.6) 470,\r\n(19.8) 500,\r\n(19.9) 520,\r\n(20.3) 546,\r\n(20.5) 560,\r\n(20.8) 589,\r\n(20.9) 620,\r\n(21.1) 650,\r\n(21.1) 680,\r\n(21.2) 700","Enstatite chondrite meteorite","Mineralogical Museum, Department of Mineralogy, St. Petersburg State University, St. Petersburg, Russia.","Sphalerite group. \r\nThe iron(II) analogue of sphalerite, browneite, etc. \r\nCompare the pure iron sulphides troilite (FeS) and pyrrhotite (Fe1-xS).","Named for Nickolay Semenovich Rudashevsky (Николай Семенович Рудашевский) (1944-), St. Petersburg, Russia, for his contributions in the study of ore minerals.","2025-09-13 16:48:09",[],[62,68,76,83,87,94,103,111],{"id":63,"name":64,"entrytype":9,"csystem":32,"ima_formula":65,"mindat_formula":66,"hmin":11,"hmax":11,"dmeas":11,"dcalc":67,"primary_image_id":11},42751,"Browneite","MnS","MnS ","3.291",{"id":69,"name":70,"entrytype":9,"csystem":32,"ima_formula":71,"mindat_formula":71,"hmin":72,"hmax":72,"dmeas":73,"dcalc":74,"primary_image_id":75},1110,"Coloradoite","HgTe",2.5,"8.10","8.092",50180,{"id":77,"name":78,"entrytype":9,"csystem":32,"ima_formula":79,"mindat_formula":79,"hmin":72,"hmax":80,"dmeas":35,"dcalc":81,"primary_image_id":82},1834,"Hawleyite","CdS",3,"4.87",10955,{"id":84,"name":85,"entrytype":9,"csystem":32,"ima_formula":86,"mindat_formula":86,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},46067,"Ishiharaite","(Cu,Ga,Fe,In,Zn)S",{"id":88,"name":89,"entrytype":9,"csystem":32,"ima_formula":90,"mindat_formula":90,"hmin":80,"hmax":80,"dmeas":91,"dcalc":92,"primary_image_id":93},2670,"Metacinnabar","HgS","7.65","7.63",15997,{"id":95,"name":96,"entrytype":9,"csystem":32,"ima_formula":97,"mindat_formula":97,"hmin":98,"hmax":99,"dmeas":100,"dcalc":101,"primary_image_id":102},3727,"Sphalerite","ZnS",3.5,4,"3.9","4.096",66200,{"id":104,"name":105,"entrytype":9,"csystem":32,"ima_formula":106,"mindat_formula":106,"hmin":107,"hmax":107,"dmeas":108,"dcalc":109,"primary_image_id":110},3786,"Stilleite","ZnSe",5,"5.42","5.267",22939,{"id":112,"name":113,"entrytype":9,"csystem":32,"ima_formula":114,"mindat_formula":114,"hmin":72,"hmax":72,"dmeas":115,"dcalc":116,"primary_image_id":117},3957,"Tiemannite","HgSe","8.19","8.239",24171,[],[120,126,132],{"id":121,"name":122,"entrytype":9,"csystem":123,"ima_formula":124,"mindat_formula":124,"hmin":11,"hmax":11,"dmeas":11,"dcalc":125,"primary_image_id":11},42371,"Buseckite","Hexagonal","(Fe,Zn,Mn)S","3.697",{"id":127,"name":128,"entrytype":9,"csystem":32,"ima_formula":129,"mindat_formula":130,"hmin":11,"hmax":11,"dmeas":35,"dcalc":131,"primary_image_id":11},27196,"Keilite","FeS","(Fe\u003Csup>2+\u003C\u002Fsup>,Mg)S","3.958",{"id":133,"name":134,"entrytype":9,"csystem":123,"ima_formula":129,"mindat_formula":129,"hmin":98,"hmax":135,"dmeas":136,"dcalc":137,"primary_image_id":138},4029,"Troilite",4.5,"4.67","4.85",24586,[140],{"id":141,"txt":142,"latitude":143,"longitude":144,"country":145},20446,"Indarch meteorite, Hindarx, Aghjabadi District, Azerbaijan",40.0694444,47.2044444,"Azerbaijan",7,[148,152],{"id":149,"year":25,"html":150,"doi":151},396026,"Britvin, S. N., Bogdanova, A. N., Boldyreva, M. M., Aksenova, G. Y. (2008) Rudashevskyite, the Fe-dominant analogue of sphalerite, a new mineral: Description and crystal structure. \u003Ci>American Mineralogist\u003C\u002Fi>,  93 (5) 902-909 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2008.2582'>doi:10.2138\u002Fam.2008.2582\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol93\u002FAM93_902.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2008.2582",{"id":153,"year":154,"html":155,"doi":11},16967083,2021,"(2021) Rudashevskyite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FRudashevskyite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[158],{"id":159,"url":160,"label":161,"formula":162,"spacegroup":163,"year":25},12300,"\u002Fcif\u002F12300.cif","Britvin 2008","(Fe.61 Zn.35 Mn.04) S","F -4 3 m",[165,166],"IMA2005-017","Rudashevskyiet",[168,172,177,181],{"lang":169,"names":170},"ca",[171],"rudashevskyita",{"lang":173,"names":174},"de",[175,176],"IMA 2005-017","Rudashevskyit",{"lang":178,"names":179},"eu",[180],"Rudashevskyita",{"lang":182,"names":183},"it",[184],"rudashevskyite","Q2798720",{"history":11,"applications":11}]