[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:47916":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":11,"ima_formula":16,"elements":17,"sigelements":23,"key_elements":11,"impurities":11,"cim":11,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":26,"publication_year":27,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":11,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":32,"cclass":33,"spacegroup":33,"spacegroupset":34,"a":35,"b":36,"c":37,"alpha":38,"beta":39,"gamma":40,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":41,"z":42,"csmetamict":14,"commentcrystal":11,"twinning":43,"tranglide":11,"parting":44,"epitaxidescription":11,"morphology":45,"tlform":46,"hmin":47,"hmax":47,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":48,"dmeas2":48,"dcalc":49,"dmeaserror":33,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":50,"commentluster":11,"diapheny":51,"streak":52,"colour":53,"commentcolor":11,"colors":54,"streak_colors":59,"luminescence":11,"uv":60,"cleavage":61,"cleavagetype":62,"fracturetype":63,"tenacity":64,"commentbreak":11,"opticaltype":65,"opticalsign":66,"opticalalpha":67,"opticalalpha2":11,"opticalalphaerror":11,"opticalbeta":68,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":69,"opticalgamma2":11,"opticalgammaerror":11,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":70,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":71,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":72,"rimax":73,"opticaldispersion":74,"opticalpleochroism":75,"opticalpleochorismdesc":76,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":77,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":78,"description_short":79,"aboutname":80,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":81,"reviewed_at":11,"variety_of":11,"varieties":82,"group_members":83,"associates":107,"confused_with":108,"type_localities":109,"occurrence_total":47,"citations":116,"images":134,"structures":145,"synonyms":146,"language_names":149,"wikidata_qid":163,"texts":164},47916,"1:1:47916:3","81763042-33ee-40c8-8a83-0187a2e40696","Ferrorhodonite","Frdn",0,"mineral",null,40297,130,false,"CaMn\u003Csub>3\u003C\u002Fsub>Fe[Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>]","CaMn\u003Csub>3\u003C\u002Fsub>Fe(Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>)",[18,19,20,21,22],"Ca","Fe","Mn","Si","O",[18,19,20,21,22],[25],"APPROVED",2016,2017,"2015","9","D","K","Triclinic",2,"0","6.6766","7.6754","11.8032","105.501","92.275","93.919",580.44,1,"Microtwinning is observed under the microscope; by analogy with rhodonite it is considered as a twinning on (111).","Perfect on (111), i.e. along the twinning plane.","Well-shaped crystals were not observed, single-crystal grains are thick tabular to short prismatic, with rounded edges.","Ferrorhodonite forms granular aggregates composed by thick tabular to short prismatic crystals, with rounded edges,up to 2 cm across.",6,"3.71","3.701","Vitreous","Transparent,Translucent","White","Brown-red, pinkish-brown",[55,56,57,58],"brown","red","pink","white",[58],"Not fluorescent.","Perfect on (201), good on (021) and (210) (according to optical data; indexed by analogy with rhodonite).","Perfect","Step-Like","brittle","Biaxial","+","1.731","1.736","1.745","74","80",1.731,1.745,"r > v, distinct","Non-pleochroic","The mineral is colourless under the microscope.","The IR spectrum is very close to that of Fe-poor rhodonite. Bands of OH groups (in the range 3000–4000 cm−1) are absent.","The type specimens (fragments of the holotype) are deposited in the collection of type specimens (Typmineralsammlung), Mineralogisches Museum Hamburg, catalogue number MMHH-004704, and in the collections of the Fersman Mineralogical Museum of the Russia.","The Fe-substituted equivalent of rhodonite.","Named for being an analogue of rhodonite with predominant Fe\u003Csup>2+\u003C\u002Fsup> (FERROus iron) at the M4 site of the structure.","2025-08-11 12:15:15",[],[84,89,99],{"id":85,"name":86,"entrytype":9,"csystem":11,"ima_formula":11,"mindat_formula":87,"hmin":11,"hmax":11,"dmeas":34,"dcalc":11,"primary_image_id":88},11200,"Fowlerite","(Mn\u003Csup>2+\u003C\u002Fsup>,Zn,Ca)SiO\u003Csub>3\u003C\u002Fsub>",9336,{"id":90,"name":91,"entrytype":9,"csystem":32,"ima_formula":92,"mindat_formula":93,"hmin":94,"hmax":95,"dmeas":96,"dcalc":97,"primary_image_id":98},3407,"Rhodonite","CaMn\u003Csub>3\u003C\u002Fsub>Mn(Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>)","CaMn\u003Csub>3\u003C\u002Fsub>Mn[Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>]",5.5,6.5,"3.57","3.726",30614,{"id":100,"name":101,"entrytype":9,"csystem":32,"ima_formula":102,"mindat_formula":103,"hmin":11,"hmax":11,"dmeas":104,"dcalc":105,"primary_image_id":106},53835,"Vittinkiite","MnMn\u003Csub>3\u003C\u002Fsub>MnSi\u003Csub>5\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>","MnMn\u003Csub>3\u003C\u002Fsub>Mn[Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>]","3.68","3.737",27525,[],[],[110],{"id":111,"txt":112,"latitude":113,"longitude":114,"country":115},23201,"Broken Hill South Mine (BHS Mine; South Mine), Broken Hill, Broken Hill district, Yancowinna Co., New South Wales, Australia",-31.9769444,141.4558333,"Australia",[117,121,125,130],{"id":118,"year":26,"html":119,"doi":120},244816,"Hålenius, U., Hatert, F., Pasero, M., Mills, S. J. (2016) New minerals and nomenclature modifications approved in 2016, CNMNC Newsletter 32. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  80 (5) 915-922 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2016.080.084'>doi:10.1180\u002Fminmag.2016.080.084\u003C\u002Fa>","10.1180\u002Fminmag.2016.080.084",{"id":122,"year":27,"html":123,"doi":124},154160,"Shchipalkina, Nadezhda V., Chukanov, Nikita V., Pekov, Igor V., Aksenov, Sergey M., McCammon, Catherine, Belakovskiy, Dmitry I., Britvin, Sergey N., Koshlyakova, Natalya N., Schäfer, Christof, Scholz, Ricardo, Rastsvetaeva, Ramiza K. (2017) Ferrorhodonite, CaMn\u003Csub>3\u003C\u002Fsub>Fe[Si\u003Csub>5\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>], a new mineral species from Broken Hill, New South Wales, Australia. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  44 (5) 323-334 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-016-0860-3'>doi:10.1007\u002Fs00269-016-0860-3\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FPCM44_323.pdf' class='refpdflink'>\u003C\u002Fa>","10.1007\u002Fs00269-016-0860-3",{"id":126,"year":127,"html":128,"doi":129},245203,2019,"Shchipalkina, Nadezhda V., Pekov, Igor V., Chukanov, Nikita V., Biagioni, Cristian, Pasero, Marco (2019) Crystal chemistry and nomenclature of rhodonite-group minerals. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  83 (6) 829-835 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2019.65'>doi:10.1180\u002Fmgm.2019.65\u003C\u002Fa>","10.1180\u002Fmgm.2019.65",{"id":131,"year":132,"html":133,"doi":11},16964306,2020,"(2020) Ferrorhodonite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fferrorhodonite.pdf' class='refpdflink'>\u003C\u002Fa>",[135],{"id":136,"source_url":137,"license_code":138,"credit_html":139,"title":140,"description":141,"author":142,"original_width":143,"original_height":144},8815,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=73662022","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=73662022\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Ferrorhodonite.jpg","Orange crystal of the mineral of the rhodonite group: ferrorhodonite (IMA 2016-016), from the type locality in Broken Hill (New South Wales, Australia) and only one of the two known localities worldwide in a marix of galena. Ferrorhodonite can be distinguished from rhodonite by its brownish pink color.","David Hospital",863,667,[],[147,148],"Ferrorhodoniet","IMA2016-016",[150,154,159],{"lang":151,"names":152},"ca",[153],"ferrorodonita",{"lang":155,"names":156},"de",[157,158],"Ferrorhodonit","IMA 2016-016",{"lang":160,"names":161},"eu",[162],"Ferrorhodonita","Q26981140",{"history":11,"applications":11}]