[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:40169":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":11,"polytypeof":11,"groupid":11,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":11,"ima_formula":15,"elements":16,"sigelements":21,"key_elements":22,"impurities":11,"cim":11,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":25,"publication_year":25,"discovery_year":11,"strunz10ed1":26,"strunz10ed2":27,"strunz10ed3":28,"strunz10ed4":29,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":30,"cclass":31,"spacegroup":32,"spacegroupset":33,"a":34,"b":35,"c":36,"alpha":11,"beta":11,"gamma":11,"aerror":37,"berror":38,"cerror":39,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":40,"z":38,"csmetamict":13,"commentcrystal":11,"twinning":41,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":42,"tlform":43,"hmin":44,"hmax":38,"hardtype":38,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":45,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":46,"commentluster":11,"diapheny":47,"streak":48,"colour":49,"commentcolor":11,"colors":50,"streak_colors":53,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":54,"fracturetype":55,"tenacity":56,"commentbreak":11,"opticaltype":11,"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":57,"opticaln2":11,"opticalnerror":11,"optical2vcalc":11,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":11,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":58,"opticalcomments":59,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":60,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":61,"otheroccurrence":11,"type_specimen_store":62,"description_short":63,"aboutname":64,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":65,"reviewed_at":11,"variety_of":11,"varieties":66,"group_members":67,"associates":68,"confused_with":69,"type_localities":70,"occurrence_total":77,"citations":78,"images":102,"structures":113,"synonyms":120,"language_names":124,"wikidata_qid":142,"texts":143},40169,"1:1:40169:4","bbe6072f-b1f6-498b-967d-be9575e7ba5e","Fassinaite","Fas",0,"mineral",null,511,false,"Pb\u003Csub>2\u003C\u002Fsub>(S\u003Csub>2\u003C\u002Fsub>O\u003Csub>3\u003C\u002Fsub>)(CO\u003Csub>3\u003C\u002Fsub>)","Pb\u003Csub>2\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)(S\u003Csub>2\u003C\u002Fsub>O\u003Csub>3\u003C\u002Fsub>)",[17,18,19,20],"Pb","O","C","S",[17,18,19,20],[17],[24],"APPROVED",2011,"7","J","A","15","Orthorhombic",8,71,"0","16.343","8.760","4.592",1,2,3,657.4,"None observed.","The crystals are acicular to prismatic [010], with a flattened diamond-shaped cross-section. The Austrian crystals are sufficiently well developed to allow determination of some of the crystal forms: the prism {101} is large and dominant, with a flat chisel-shaped {\u003Cem>hk\u003C\u002Fem>0} termination, possibly {110}. Small faces which are possibly {011} are rarely present. Further forms are minute and difficult to measure as they are commonly rounded.","Radiating aggregates of acicular, colourless crystals up to 0.2 mm long.",1.5,"6.084","Adamantine","Transparent,Translucent","White","Colourless, white",[51,52],"colorless","white",[52],"None Observed","Irregular\u002FUneven","brittle","2.13","Very high.","Fassinaite has intense internal reflections, which do not allow satisfactory optical data to be collected; the crystals are length-slow and have very high birefringence.","Straight. Crystals are length-slow.","The mineralization is linked to Mid-Triassic calc-alkaline magmatism. Hydrothermal fluids related to volcanism deposited sulphides, baryte and Fe- and Mn-bearing minerals at the boundary between Ladinic volcanites and limestone\r\nof the Mount Spitz Formation. Supergene minerals including sulphates, carbonates and arsenates of Zn, Pb and Cu are very common.","Museum of Mineralogy of the Department of Geosciences at\r\nthe University of Padova, Italy, under catalogue number MMP M10008.","One of a relatively small group of thiosulphate minerals.\r\n\r\nMay be visually similar to elongate anglesite.","Named after Bruno Fassina (b. 1943) Italian mineral collector, who discovered the mineral at the Trentini mine in 2009.","2025-08-11 12:15:06",[],[],[],[],[71],{"id":72,"txt":73,"latitude":74,"longitude":75,"country":76},28332,"Trentini Mine, Contrada Trentini, Monte Naro - Riolo Valley side, Monte Naro, Torrebelvicino, Vicenza Province, Veneto, Italy",45.7108333,11.305,"Italy",17,[79,83,86,90,94,98],{"id":80,"year":81,"html":82,"doi":11},16138287,2010,"Kolitsch, U.  (2010) Pb2(S2O3)(CO3): The first naturally occurring thiosulphate carbonate and its atomic arrangement. \u003Ci>20th General Meeting of the IMA (IMA2010)\u003C\u002Fi>, abstract in CD of Abstracts. Budapest, Hungary. 489pp.",{"id":84,"year":25,"html":85,"doi":11},16138288,"Nestola, F., Bindi, L., Guastoni, A., Zorzi, F., Nasdala, L. (2011) Pb2(CO3)(S2O3), the first mineral with coexisting carbonate and thiosulfate groups from Trentini mine, Vicenza, Italy. \u003Ci> Geoitalia 2011,\u003C\u002Fi>, abstract in Plinius 37. Turin, Italy,. 308pp.",{"id":87,"year":25,"html":88,"doi":89},244172,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2011) New minerals and nomenclature modifications approved in 2011, CNMNC Newsletter No. 10. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  75 (5) 2549-2561 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2011.075.5.2549'>doi:10.1180\u002Fminmag.2011.075.5.2549\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fuploads\u002FMM75_2549.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.2011.075.5.2549",{"id":91,"year":25,"html":92,"doi":93},244185,"Bindi, L., Nestola, F., Kolitsch, U., Guastoni, A., Zorzi, F. (2011) Fassinaite, Pb\u003Csub>2\u003C\u002Fsub>\u003Csup>2+\u003C\u002Fsup>(S\u003Csub>2\u003C\u002Fsub>O\u003Csub>3\u003C\u002Fsub>)(CO\u003Csub>3\u003C\u002Fsub>), the first mineral with coexisting thiosulphate and carbonate groups: description and crystal structure. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  75 (6) 2721-2732 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2011.075.6.2721'>doi:10.1180\u002Fminmag.2011.075.6.2721\u003C\u002Fa>","10.1180\u002Fminmag.2011.075.6.2721",{"id":95,"year":96,"html":97,"doi":11},16138291,2012,"Kolitsch, U., Bindi, L., Nestola, F., Guastoni, A., Zorzi, F., Poeverlein, R. (2012) Fassinait, ein neues Bleimineral aus Italien, Österreich und Deutschland. \u003Ci>Lapis\u003C\u002Fi>,  37 (1) 52-53",{"id":99,"year":100,"html":101,"doi":11},16964208,2013,"(2013) Fassinaite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Ffassinaite.pdf' class='refpdflink'>\u003C\u002Fa>",[103],{"id":104,"source_url":105,"license_code":106,"credit_html":107,"title":108,"description":109,"author":110,"original_width":111,"original_height":112},8346,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=181847786","CC BY 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=181847786\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fassinaite.jpg","White crystals of the rare thiosulphate mineral fassinaite from Austria (Erasmus adit, Schwarzleo District, Schwarzleograben, Leogang, Salzburg, Austria) on a dark contrasting matrix. Ex. Erich Laskowski collection (USA).","David Hospital",690,568,[114],{"id":115,"url":116,"label":117,"formula":118,"spacegroup":119,"year":25},4349,"\u002Fcif\u002F4349.cif","Bindi 2011","Pb2 S2 C O6","P n m a",[121,122,123],"Fassinaiet","IMA2011-048","Unnamed (Pb Thiosulphate Carbonate)",[125,129,134,138],{"lang":126,"names":127},"ca",[128],"fassinaïta",{"lang":130,"names":131},"de",[132,133],"Fassinait","IMA 2011-048",{"lang":135,"names":136},"eu",[137],"Fassinaita",{"lang":139,"names":140},"it",[141],"fassinaite","Q19833617",{"history":11,"applications":11}]