[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:52572":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":12,"weighting":13,"nolocadd":14,"blacklisted":14,"mindat_formula":15,"mindat_formula_note":16,"ima_formula":17,"elements":18,"sigelements":25,"key_elements":26,"impurities":11,"cim":11,"ima_status":27,"ima_notes":11,"ima_history":11,"approval_year":29,"publication_year":30,"discovery_year":11,"strunz10ed1":31,"strunz10ed2":32,"strunz10ed3":33,"strunz10ed4":34,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":35,"cclass":36,"spacegroup":11,"spacegroupset":37,"a":38,"b":39,"c":40,"alpha":41,"beta":42,"gamma":43,"aerror":36,"berror":36,"cerror":44,"alphaerror":36,"betaerror":36,"gammaerror":36,"va3":11,"z":45,"csmetamict":14,"commentcrystal":46,"twinning":47,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":48,"hmin":49,"hmax":11,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":50,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":51,"streak":11,"colour":52,"commentcolor":11,"colors":53,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":57,"opticalsign":11,"opticalalpha":11,"opticalalpha2":11,"opticalalphaerror":11,"opticalbeta":11,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":11,"opticalgamma2":11,"opticalgammaerror":11,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":11,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":11,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":58,"opticalpleochroism":59,"opticalpleochorismdesc":11,"opticalbirefringence":60,"opticalcomments":61,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":62,"otheroccurrence":11,"type_specimen_store":63,"description_short":64,"aboutname":65,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":66,"reviewed_at":11,"variety_of":11,"varieties":67,"group_members":68,"associates":87,"confused_with":88,"type_localities":91,"occurrence_total":44,"citations":98,"images":120,"structures":139,"synonyms":140,"language_names":143,"wikidata_qid":157,"texts":158},52572,"1:1:52572:7","0f6026ac-f0f8-4c85-a74d-c41a3a86310c","Silesiaite","Ssa",0,"mineral",null,55753,23,false,"Ca\u003Csub>4\u003C\u002Fsub>(Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Sn\u003Csub>2\u003C\u002Fsub>)[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>2\u003C\u002Fsub>[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH]\u003Csub>2\u003C\u002Fsub>","Formula according to CNMNC Newsletter 70, establishment of kristansenite group.","Ca\u003Csub>4\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Sn\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH)\u003Csub>2\u003C\u002Fsub>",[19,20,21,22,23,24],"Ca","Fe","Si","Sn","O","H",[19,20,21,22,23,24],[22],[28],"APPROVED",2017,2023,"9","B","C","30","Triclinic",1,"0","10.028","8.408","13.339","90.01","109.10","90.00",2,4,"Space group is C1","Polysynthetic twinning.","Mixed kristiansenite-silesiaite crystals with maximum sizes of ~350 × 100 μm. Silesiaite occurs in the form of Fe-dominant bands, usually reaching only a few micrometers in thickness.",6,"3.737","Transparent","Colourless to rarely greenish-grey",[54,55,56],"colorless","green","gray","Biaxial","High","Visible","Low, but the first order of the interference colour spectrum, is leather brown and ink blue to grey-blue.","Under plane polarized light, the crystals are uncoloured to yellowish.\r\nThe refractive index is between 1.887 (hydroandradite) and 1.55 (Canada balsam).\r\nmean refractive index of ~1.727 calculated from the Gladstone-Dale relation","Granitic pegmatite.","Collections of the Mineralogical Museum, University of Wrocław, Cybulskiego 30, 50-205 Wrocław, Poland, catalogue number MMWr IV7929.","The Fe(III)-analogue of kristiansenite. The Fe3+Sn-analogue of kozłowskiite. Chemically similar to toturite.\r\n\r\nThe content of some of the M sites is somewhat variable:\r\n* M1 = Fe3+ + Sc (mainly), the M2-M4 sites: Sn (Szklarska Poręba material), versus...","For Silesia, Latin name of Śląsk, which is a large area occupying >50% of the southern (south-west and south) part of Poland, and where the type locality is situated.","2025-10-05 17:15:14",[],[69,75,83],{"id":70,"name":71,"entrytype":9,"csystem":35,"ima_formula":72,"mindat_formula":73,"hmin":11,"hmax":11,"dmeas":11,"dcalc":74,"primary_image_id":11},55754,"Kozłowskiite","Ca\u003Csub>4\u003C\u002Fsub>Fe\u003Csup>2+\u003C\u002Fsup>Sn\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH)\u003Csub>2\u003C\u002Fsub>","Ca\u003Csub>4\u003C\u002Fsub>(Fe\u003Csup>2+\u003C\u002Fsup>Sn\u003Csub>3\u003C\u002Fsub>)[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>2\u003C\u002Fsub>[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH]\u003Csub>2\u003C\u002Fsub>","3.775",{"id":76,"name":77,"entrytype":9,"csystem":35,"ima_formula":78,"mindat_formula":79,"hmin":80,"hmax":49,"dmeas":37,"dcalc":81,"primary_image_id":82},10814,"Kristiansenite","Ca\u003Csub>4\u003C\u002Fsub>Sc\u003Csub>2\u003C\u002Fsub>Sn\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH)\u003Csub>2\u003C\u002Fsub>","Ca\u003Csub>4\u003C\u002Fsub>(Sc\u003Csub>2\u003C\u002Fsub>Sn\u003Csub>2\u003C\u002Fsub>)[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>]\u003Csub>2\u003C\u002Fsub>[Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH]\u003Csub>2\u003C\u002Fsub>",5.5,"3.64",13665,{"id":84,"name":85,"entrytype":9,"csystem":35,"ima_formula":11,"mindat_formula":86,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},498773,"Nybergite","Ca\u003Csub>4\u003C\u002Fsub>Sc\u003Csub>3\u003C\u002Fsub>Sn(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH)\u003Csub>3\u003C\u002Fsub>",[],[89,90],{"id":70,"name":71,"entrytype":9,"csystem":35,"ima_formula":72,"mindat_formula":73,"hmin":11,"hmax":11,"dmeas":11,"dcalc":74,"primary_image_id":11},{"id":76,"name":77,"entrytype":9,"csystem":35,"ima_formula":78,"mindat_formula":79,"hmin":80,"hmax":49,"dmeas":37,"dcalc":81,"primary_image_id":82},[92],{"id":93,"txt":94,"latitude":95,"longitude":96,"country":97},134907,"Szklarska Poręba Huta granite quarry, Szklarska Poręba, Karkonosze County, Lower Silesian Voivodeship, Poland",50.8269276,15.4945857,"Poland",[99,103,108,112,116],{"id":100,"year":29,"html":101,"doi":102},244967,"Hålenius, U., Hatert, F., Pasero, M., Mills, S. J. (2017) New minerals and nomenclature modifications approved in 2017, CNMNC Newsletter No 40. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  81 (6) 1577-1581 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2017.081.096'>doi:10.1180\u002Fminmag.2017.081.096\u003C\u002Fa>","10.1180\u002Fminmag.2017.081.096",{"id":104,"year":105,"html":106,"doi":107},16886779,2021,"Cepedal, Antonia, Fuertes-Fuente, Mercedes, Martin-Izard, Agustín (2021) Occurrence of silesiaite, a new calcium–iron–tin sorosilicate in the calcic skarn of El Valle-Boinás, Asturias, Spain. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  33 (2) 165-174 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-33-165-2021'>doi:10.5194\u002Fejm-33-165-2021\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F33\u002F165\u002F2021\u002Fejm-33-165-2021.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-33-165-2021",{"id":109,"year":110,"html":111,"doi":11},16967323,2022,"(2022) Silesiaite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FSilesiaite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":113,"year":110,"html":114,"doi":115},16143728,"Miyawaki, Ritsuro, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2022) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) – Newsletter 70. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  34 (6) 591-601 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-34-591-2022'>doi:10.5194\u002Fejm-34-591-2022\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F34\u002F591\u002F2022\u002Fejm-34-591-2022.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-34-591-2022",{"id":117,"year":30,"html":118,"doi":119},15839877,"Pieczka, Adam, Zelek-Pogudz, Sylwia, Gołębiowska, Bożena, Stadnicka, Katarzyna M., Kristiansen, Roy (2023) Silesiaite, ideally Ca\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>Sn(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>OH), a new species in the kristiansenite group: crystal chemistry and structure of holotype silesiaite from Szklarska Poręba, Poland, and Sc-free silesiaite from Häiviäntien, Finland. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  87 (2) 271-283 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2023.5'>doi:10.1180\u002Fmgm.2023.5\u003C\u002Fa>","10.1180\u002Fmgm.2023.5",[121,131],{"id":122,"source_url":123,"license_code":124,"credit_html":125,"title":126,"description":127,"author":128,"original_width":129,"original_height":130},22316,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=158068793","CC BY 4.0","Antonia Cepedal, Mercedes Fuertes-Fuente, Agustín Martin-Izard, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=158068793\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Silesiaite in the calcic skarn of El Valle-Boinás, Asturias.png","(a) Microphotography showing the silesiaite (sil) and hydroandradite (had) crystal aggregates surrounding and replacing chalcopyrite (cpy). Apophyllite-(KOH) and babingtonite (bab) appear to be filling the cavity under plain polarized light. (b) The same image under polarized and analysed light. The mineral has anomalous ink blue and leather brown interference colours. (c) Detail of the silesiaite aggregates in which a weak pleochroism from uncoloured to yellowish is observed. (d) The same image under polarized and analysed light. One of the sections has an hourglass zoning and something resembling polysynthetic twins with thin plates. (e) Backscattered electron image that shows the compositional zoning mimicking the optical zoning. Light grey areas are rich in Sn, and dark grey areas are rich in Fe. (f) Secondary electron image of a tiny fragment of the sample. It shows an aggregate of some silesiaite crystals with a tabular habit and an imperfect cleavage of the crystals.","Antonia Cepedal, Mercedes Fuertes-Fuente, Agustín Martin-Izard",2067,2345,{"id":132,"source_url":133,"license_code":124,"credit_html":134,"title":135,"description":136,"author":128,"original_width":137,"original_height":138},22317,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=158068872","Antonia Cepedal, Mercedes Fuertes-Fuente, Agustín Martin-Izard, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=158068872\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Silesiaite in the calcic skarn of El Valle-Boinás, Asturias (d).png","(d) The same image under polarized and analysed light. One of the sections has an hourglass zoning and something resembling polysynthetic twins with thin plates.",1007,758,[],[141,142],"IMA2017-064","Silesiaiet",[144,148,153],{"lang":145,"names":146},"ca",[147],"silesiaïta",{"lang":149,"names":150},"de",[151,152],"IMA 2017-064","Silesiait",{"lang":154,"names":155},"eu",[156],"Silesiaita","Q45959965",{"history":11,"applications":11}]