[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:471057":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":6,"synid":6,"polytypeof":6,"groupid":11,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":6,"ima_formula":6,"elements":15,"sigelements":19,"key_elements":20,"impurities":6,"cim":6,"ima_status":21,"ima_notes":6,"ima_history":6,"approval_year":6,"publication_year":6,"discovery_year":6,"strunz10ed1":23,"strunz10ed2":24,"strunz10ed3":25,"strunz10ed4":26,"dana8ed1":6,"dana8ed2":6,"dana8ed3":6,"dana8ed4":6,"csystem":27,"cclass":28,"spacegroup":29,"spacegroupset":30,"a":31,"b":6,"c":6,"alpha":6,"beta":6,"gamma":6,"aerror":32,"berror":6,"cerror":6,"alphaerror":6,"betaerror":6,"gammaerror":6,"va3":6,"z":33,"csmetamict":13,"commentcrystal":6,"twinning":6,"tranglide":6,"parting":6,"epitaxidescription":6,"morphology":6,"tlform":34,"hmin":35,"hmax":6,"hardtype":6,"vhnmin":6,"vhnmax":6,"vhnerror":6,"vhng":6,"vhns":6,"commenthard":36,"dmeas":6,"dmeas2":6,"dcalc":37,"dmeaserror":6,"dcalcerror":6,"commentdense":6,"lustre":6,"lustretype":38,"commentluster":6,"diapheny":39,"streak":6,"colour":6,"commentcolor":6,"colors":6,"streak_colors":6,"luminescence":6,"uv":6,"cleavage":40,"cleavagetype":41,"fracturetype":6,"tenacity":42,"commentbreak":6,"opticaltype":6,"opticalsign":6,"opticalalpha":6,"opticalalpha2":6,"opticalalphaerror":6,"opticalbeta":6,"opticalbeta2":6,"opticalbetaerror":6,"opticalgamma":6,"opticalgamma2":6,"opticalgammaerror":6,"opticalomega":6,"opticalomega2":6,"opticalomegaerror":6,"opticalepsilon":6,"opticalepsilon2":6,"opticalepsilonerror":6,"opticaln":6,"opticaln2":6,"opticalnerror":6,"optical2vcalc":6,"optical2vcalc2":6,"optical2vcalcerror":6,"optical2vmeasured":6,"optical2vmeasured2":6,"optical2vmeasurederror":6,"rimin":6,"rimax":6,"opticaldispersion":6,"opticalpleochroism":6,"opticalpleochorismdesc":6,"opticalbirefringence":6,"opticalcomments":6,"opticalcolour":43,"opticalinternal":6,"opticaltropic":6,"opticalanisotropism":6,"opticalbireflectance":6,"opticalextinction":6,"opticalr":6,"specdispm":6,"ir":6,"electrical":6,"magnetism":6,"thermalbehaviour":6,"other":6,"industrial":6,"occurrence":44,"otheroccurrence":6,"type_specimen_store":45,"description_short":46,"aboutname":47,"rock_parent":6,"rock_parent2":6,"rock_root":9,"rock_bgs_code":6,"meteoritical_code":6,"updttime":48,"reviewed_at":6,"variety_of":6,"varieties":49,"group_members":50,"associates":116,"confused_with":117,"type_localities":118,"occurrence_total":12,"citations":125,"images":139,"structures":140,"synonyms":168,"language_names":170,"wikidata_qid":186,"texts":187},471057,"1:1:471057:4",null,"Shiranuiite","Sir",0,"mineral",52869,1,false,"Cu\u003Csup>+\u003C\u002Fsup>(Rh\u003Csup>3+\u003C\u002Fsup>Rh\u003Csup>4+\u003C\u002Fsup>)S\u003Csub>4\u003C\u002Fsub>",[16,17,18],"Cu","Rh","S",[16,17,18],[16,17],[22],"APPROVED","2","D","A","05","Isometric",32,222,"Fd-3m","9.757",2,8,"Isoferroplatinum-based grains are often accompanied by black to gray colored nubs from 20 to 500 μm in size. Shiranuiite and cuprorhodsite occur as dominant minerals of such nubs, although both are indistinguishable based on the occurrence mode and can only be distinguished by chemical analysis.",5,"according to the analogous thiospinel-group minerals","5.78","Metallic","Opaque","estimated to be along the {111} planes according to the isotypic malanite","Poor\u002FIndistinct","brittle","a bluish gray color","The clinopyroxenite mass has a depression near the center, and a small river, approximately 2-3 m wide and 2 km long, passes through this area and joins the Shakain River. PGM can be collected as a placer in this small river. Most of the PGM placer collected was composed of isoferroplatinum-based grains that are irregularly shaped with an average size of less than 1 mm, although grains up to 4 mm were also obtained.","Type material is deposited in the collections of the National Museum of Nature and Science, Amakubo, Tsukuba, Ibaraki 305-0005, Japan, specimen number NSM-M50086","The Rh4+-analogue of ezochiite; the Rh, or rather RhRh-analogue of malanite.\r\n\r\nPossibly a variety of cuprorhodsite:\r\nInstead of weighing the significance of chemical substitution in a PGE-dominant thiospinel, the readership is instead burdened with ac...","This new mineral was named shiranuiite based on a Japanese legend that leads to the ancient name for Kumamoto Prefecture, Kyushu, Japan. In the Nihon Shoki (Chronicles of Japan), the oldest book that records the history of Japan, Emperor Keiko, the 12th emperor of Japan, lost his bearing at sea during a pilgrimage to Kyushu, but was able to land safely because he fortunately saw fire in the distance. He then asked, \"Who lit the fire?\" to which everyone reportedly replied that it was \"The fire that everyone does not know about (= SHIRANUI, in Japanese historical kana orthography)\". From this lore, this area came to be called \"Land of Fire\", now known as Kumamoto Prefecture. Shiranuiite was named in honor of this interesting episode of the locality.","2026-03-12 11:16:32",[],[51,57,66,74,79,84,90,96,102,110],{"id":52,"name":53,"entrytype":9,"csystem":27,"ima_formula":6,"mindat_formula":54,"hmin":55,"hmax":6,"dmeas":6,"dcalc":56,"primary_image_id":6},471225,"Berndlehmannite","Cu(CrV)S\u003Csub>4\u003C\u002Fsub>",3.5,"4.17",{"id":58,"name":59,"entrytype":9,"csystem":27,"ima_formula":60,"mindat_formula":60,"hmin":61,"hmax":62,"dmeas":63,"dcalc":64,"primary_image_id":65},911,"Carrollite","CuCo\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",4.5,5.5,"4.5","4.83",4804,{"id":67,"name":68,"entrytype":9,"csystem":27,"ima_formula":69,"mindat_formula":70,"hmin":62,"hmax":62,"dmeas":71,"dcalc":72,"primary_image_id":73},1186,"Cuproiridsite","Cu(Ir\u003Csup>3+\u003C\u002Fsup>Ir\u003Csup>4+\u003C\u002Fsup>)S\u003Csub>4\u003C\u002Fsub>","(Cu,Fe)Ir\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","0","7.24",6647,{"id":75,"name":76,"entrytype":9,"csystem":27,"ima_formula":77,"mindat_formula":77,"hmin":61,"hmax":35,"dmeas":6,"dcalc":78,"primary_image_id":6},40142,"Cuprokalininite","Cu(Cr\u003Csup>3+\u003C\u002Fsup>Cr\u003Csup>4+\u003C\u002Fsup>)S\u003Csub>4\u003C\u002Fsub>","4.16",{"id":80,"name":81,"entrytype":9,"csystem":27,"ima_formula":82,"mindat_formula":82,"hmin":35,"hmax":6,"dmeas":6,"dcalc":83,"primary_image_id":6},470612,"Ezochiite","Cu\u003Csup>+\u003C\u002Fsup>(Rh\u003Csup>3+\u003C\u002Fsup>Pt\u003Csup>4+\u003C\u002Fsup>)S\u003Csub>4\u003C\u002Fsub>","6.66",{"id":85,"name":86,"entrytype":9,"csystem":27,"ima_formula":87,"mindat_formula":87,"hmin":35,"hmax":35,"dmeas":71,"dcalc":88,"primary_image_id":89},1557,"Fletcherite","CuNi\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","4.76",8970,{"id":91,"name":92,"entrytype":9,"csystem":27,"ima_formula":93,"mindat_formula":94,"hmin":35,"hmax":35,"dmeas":71,"dcalc":95,"primary_image_id":6},1563,"Florensovite","Cu(Cr\u003Csub>1.5\u003C\u002Fsub>Sb\u003Csub>0.5\u003C\u002Fsub>)S\u003Csub>4\u003C\u002Fsub>","(Cu,Zn)Cr\u003Csub>1.5\u003C\u002Fsub>Sb\u003Csub>0.5\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","4.28",{"id":97,"name":98,"entrytype":9,"csystem":27,"ima_formula":99,"mindat_formula":99,"hmin":35,"hmax":35,"dmeas":71,"dcalc":100,"primary_image_id":101},2551,"Malanite","Cu\u003Csup>1+\u003C\u002Fsup>(Ir\u003Csup>3+\u003C\u002Fsup>Pt\u003Csup>4+\u003C\u002Fsup>)S\u003Csub>4\u003C\u002Fsub>","7.46",15212,{"id":103,"name":104,"entrytype":9,"csystem":105,"ima_formula":106,"mindat_formula":106,"hmin":107,"hmax":107,"dmeas":71,"dcalc":108,"primary_image_id":109},3408,"Rhodostannite","Tetragonal","Cu\u003Csup>1+\u003C\u002Fsup>(Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>Sn\u003Csup>4+\u003C\u002Fsup>\u003Csub>1.5\u003C\u002Fsub>)S\u003Csub>4\u003C\u002Fsub>",4,"4.79",20862,{"id":111,"name":112,"entrytype":9,"csystem":105,"ima_formula":113,"mindat_formula":113,"hmin":107,"hmax":107,"dmeas":71,"dcalc":114,"primary_image_id":115},4004,"Toyohaite","Ag\u003Csup>1+\u003C\u002Fsup>(Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>0.5\u003C\u002Fsub>Sn\u003Csup>4+\u003C\u002Fsup>\u003Csub>1.5\u003C\u002Fsub>)S\u003Csub>4\u003C\u002Fsub>","7.25",24449,[],[],[119],{"id":120,"txt":121,"latitude":122,"longitude":123,"country":124},312048,"Haraigawa, Misato, Shimomashiki District, Kumamoto Prefecture, Japan",32.5725896,130.7904738,"Japan",[126,129,134],{"id":127,"year":6,"html":128,"doi":6},17250137,"Nishio-Hamane, D., Tanaka, T., and Shinmachi, T.: Shiranuiite, IMA 2023-072a, in: CNMNC Newsletter 78, Eur. J. Mineral., 36, https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-36-361-2024, 2024.",{"id":130,"year":131,"html":132,"doi":133},17436987,2024,"NISHIO-HAMANE, Daisuke, SAITO, Katsuyuki (2024) Ezochiite, Cu+(Rh3+Pt4+)S4, a new mineral in the thiospinel group from Hokkaido, Japan. \u003Ci>Journal of Mineralogical and Petrological Sciences\u003C\u002Fi>,  119 (1). 240304 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2465\u002Fjmps.240304'>doi:10.2465\u002Fjmps.240304\u003C\u002Fa>","10.2465\u002Fjmps.240304",{"id":135,"year":136,"html":137,"doi":138},18502320,2025,"Cabri, Louis J.; McDonald, Andrew M. (2025) Ezochiite and shiranuiite are cuprorhodsite and are not new mineral species. \u003Ci>American Mineralogist\u003C\u002Fi>,  110 (6). 941-944 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2024-9517'>doi:10.2138\u002Fam-2024-9517\u003C\u002Fa>","10.2138\u002Fam-2024-9517",[],[141,148,153,158,163],{"id":142,"url":143,"label":144,"formula":145,"spacegroup":146,"year":147},12690,"\u002Fcif\u002F12690.cif","Riedel 1981 · Cu Rh2 S4","Cu Rh2 S4","F d 3 m",1981,{"id":149,"url":150,"label":151,"formula":152,"spacegroup":146,"year":147},12691,"\u002Fcif\u002F12691.cif","Riedel 1981 · (Cu.9 Fe.1) Rh2 S4","(Cu.9 Fe.1) Rh2 S4",{"id":154,"url":155,"label":156,"formula":157,"spacegroup":146,"year":147},12692,"\u002Fcif\u002F12692.cif","Riedel 1981 · (Cu.8 Fe.2) Rh2 S4","(Cu.8 Fe.2) Rh2 S4",{"id":159,"url":160,"label":161,"formula":162,"spacegroup":146,"year":147},12693,"\u002Fcif\u002F12693.cif","Riedel 1981 · (Cu.7 Fe.3) Rh2 S4","(Cu.7 Fe.3) Rh2 S4",{"id":164,"url":165,"label":166,"formula":167,"spacegroup":146,"year":147},12694,"\u002Fcif\u002F12694.cif","Riedel 1981 · (Cu.6 Fe.4) Rh2 S4","(Cu.6 Fe.4) Rh2 S4",[169],"Shiranuiiet",[171,175,179,182],{"lang":172,"names":173},"ca",[174],"shiranuiïta",{"lang":176,"names":177},"de",[178],"Shiranuiit",{"lang":180,"names":181},"it",[7],{"lang":183,"names":184},"ja",[185],"不知火鉱","Q125693289",{"history":6,"applications":6}]