[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:7269":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":14,"elements":15,"sigelements":18,"key_elements":19,"impurities":11,"cim":11,"ima_status":20,"ima_notes":11,"ima_history":11,"approval_year":22,"publication_year":23,"discovery_year":11,"strunz10ed1":24,"strunz10ed2":25,"strunz10ed3":26,"strunz10ed4":27,"dana8ed1":28,"dana8ed2":28,"dana8ed3":28,"dana8ed4":28,"csystem":29,"cclass":30,"spacegroup":30,"spacegroupset":28,"a":31,"b":32,"c":33,"alpha":34,"beta":35,"gamma":36,"aerror":37,"berror":37,"cerror":38,"alphaerror":39,"betaerror":40,"gammaerror":41,"va3":11,"z":42,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":43,"epitaxidescription":11,"morphology":11,"tlform":44,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":28,"vhnmax":28,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":28,"dmeas2":28,"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":55,"luminescence":11,"uv":11,"cleavage":56,"cleavagetype":57,"fracturetype":11,"tenacity":58,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":28,"opticalalpha2":28,"opticalalphaerror":11,"opticalbeta":28,"opticalbeta2":28,"opticalbetaerror":11,"opticalgamma":28,"opticalgamma2":28,"opticalgammaerror":11,"opticalomega":28,"opticalomega2":28,"opticalomegaerror":11,"opticalepsilon":28,"opticalepsilon2":28,"opticalepsilonerror":11,"opticaln":28,"opticaln2":28,"opticalnerror":11,"optical2vcalc":28,"optical2vcalc2":28,"optical2vcalcerror":11,"optical2vmeasured":28,"optical2vmeasured2":28,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":59,"opticalinternal":11,"opticaltropic":60,"opticalanisotropism":61,"opticalbireflectance":11,"opticalextinction":11,"opticalr":62,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":63,"otheroccurrence":11,"type_specimen_store":64,"description_short":65,"aboutname":66,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":67,"reviewed_at":11,"variety_of":11,"varieties":68,"group_members":69,"associates":70,"confused_with":71,"type_localities":72,"occurrence_total":79,"citations":80,"images":115,"structures":182,"synonyms":183,"language_names":185,"wikidata_qid":236,"texts":237},7269,"1:1:7269:0","c7d47a17-89bc-4168-afe2-b560388d5475","Rheniite","Rhn",0,"mineral",null,523,false,"ReS\u003Csub>2\u003C\u002Fsub>",[16,17],"Re","S",[16,17],[16],[21],"APPROVED",2004,2005,"2","E","B","35","0","Triclinic",2,"6.470","6.368","6.401","105.0","91.59","118.90",5,7,1,9,6,4,"With pseudohexagonal symmetry.","Millimetric, wedge-shaped crystals that are dark red translucent.","7.598","Metallic","Translucent","Gray-black","Silvery-white, black, red translucent",[51,52,53,54],"white","black","gray","red",[53,52],"Pefect on {001}","Perfect","elastic","White with slight pink hue","Anisotropic","Strong","(43.0,46.0) 400,\r\n(41.2,44.9) 420,\r\n(39.8,44.1) 440,\r\n(39.3,44.0) 460,\r\n(39.1,44.1) 470,\r\n(39.0,44.0) 480,\r\n(38.6,43.7) 500,\r\n(38.1,43.3) 520,\r\n(37.7,42.9) 540,\r\n(37.6,42.8) 546,\r\n(37.7,42.9) 560,\r\n(37.7,42.3) 580,\r\n(37.6,42.2) 589,\r\n(37.4,42.1) 600,\r\n(37.2,42.1) 620,\r\n(37.3,42.3) 640,\r\n(37.3,42.4) 650,\r\n(37.2,42.4) 660,\r\n(37.0,41.9) 680,\r\n(36.4,41.1) 700","High temperature fumarole","Fersman Mineralogical Museum, Russian Academy of Sciences, Moscow, Russia.","One of a very few rhenium-dominant minerals. Compare, e.g., rhenium, tarkianite, dzhezkazganite, and 'UM1986-51-S:Re'.","Named for its rhenium content.","2025-11-02 20:37:31",[],[],[],[],[73],{"id":74,"txt":75,"latitude":76,"longitude":77,"country":78},10264,"Kudriavy volcano, Iturup Island, Kurilsky District, Kuril Islands, Sakhalin Oblast, Russia",45.3812917,148.8171639,"Russia",10,[81,85,88,91,95,98,101,105,109,112],{"id":82,"year":83,"html":84,"doi":11},16131128,1994,"Kelty, S.P., Ruppert, A.F., Chianelli, R.R., Ren, J., Whangbo, M-H. (1994) Journal of the American Chemical Society: 116: 7857-7863.",{"id":86,"year":83,"html":87,"doi":11},16131129,"Murray, H.H., Kelty, S.P., Chianelli, R.R., Day, C.S. (1994) Inorganic Chemistry: 33: 4418-4420.",{"id":89,"year":83,"html":90,"doi":11},16131130,"Korzhinsky, M.A., Tkachenko, S.I., Shmulovich, K.I., Taran, Y.A., Steinberg, G.S. (1994) Nature: 369: 51-20.",{"id":92,"year":93,"html":94,"doi":11},16131133,2001,"www.cnt.ru (n.d.) \u003Ca target='_blank' rel='nofollow' href='http:\u002F\u002Fwww.cnt.ru\u002Fusers\u002Fyakushev\u002Frhenium\u002F'>http:\u002F\u002Fwww.cnt.ru\u002Fusers\u002Fyakushev\u002Frhenium\u002F\u003C\u002Fa>",{"id":96,"year":23,"html":97,"doi":11},15976534,"Canadian Mineralogist (2005) 43, 834.",{"id":99,"year":23,"html":100,"doi":11},16131132,"Znamensky, V.S., Korzhinsky, M.A., Steinberg, G.S., Trachenko, S.I., Yakushev, A.I., Laputina, I.P., Bryzgalov, I.A., Samotoin, N.D., Magazina, L.O., Kuzmina, O.V., Organova, N.I., Rassulov, V.A., Chaplygin, I.V. (2005) Rheniite, ReS2, the natural rhenium disulphide from fumaroles of of Kudryavy volcano, Iturup Island, Kurile Islands. (Russian with English abstract) Zapiski Vserossiyskogo Mineralogicheskogo Obshchestva (Proceedings of the Russian Mineralogical Society): 134(5): 32–40.",{"id":102,"year":103,"html":104,"doi":11},17631621,2007,"(2007) New Minerals From Former Soviet Union Countries 1998-2006. \u003Ci>Mineralogical Almanac\u003C\u002Fi> Vol. 11",{"id":106,"year":107,"html":108,"doi":11},16131134,2021,"www.youtube.com (n.d.) \u003Ca target='_blank' rel='nofollow' href='https:\u002F\u002Fwww.youtube.com\u002Fwatch?v=1ftfKT46PNg'>https:\u002F\u002Fwww.youtube.com\u002Fwatch?v=1ftfKT46PNg\u003C\u002Fa>",{"id":110,"year":107,"html":111,"doi":11},16131135,"Ibáñez-Insa, J., Woźniak, T., Oliva, R., Popescu, C., Hernández, S., López-Vidrier, J. (2021): Structural and High-Pressure Properties of Rheniite (ReS\u003Csub>2\u003C\u002Fsub>) and (Re,Mo)S\u003Csub>2\u003C\u002Fsub>. Minerals: 11: 207.",{"id":113,"year":107,"html":114,"doi":11},16966981,"(2021) Rheniite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FRheniite.pdf' class='refpdflink'>\u003C\u002Fa>",[116,123,133,141,148,155,161,168,176],{"id":117,"source_url":118,"license_code":119,"credit_html":120,"title":7,"description":11,"author":11,"original_width":121,"original_height":122},30606,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F170031","CC BY-SA 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F170031\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",1000,750,{"id":124,"source_url":125,"license_code":126,"credit_html":127,"title":128,"description":129,"author":130,"original_width":131,"original_height":132},20805,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10124294","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10124294\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-34295.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRheniite\" class=\"extiw\" title=\"en:Rheniite\">Rheniite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kudriavy (Kudryavyi) volcano, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FIturup\" class=\"extiw\" title=\"en:Iturup\">Iturup Island\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKuril_Islands\" class=\"extiw\" title=\"en:Kuril Islands\">Kuril Islands\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSakhalin_Oblast\" class=\"extiw\" title=\"en:Sakhalin Oblast\">Sakhalinskaya Oblast'\u003C\u002Fa>, Far-Eastern Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-10264.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Rheniite is the only known mineral with Rhenium as its primary metallic constituent and as such is a fascinating species. It occurs at a volcanic vent in this remote area of Russia, and scientists have to climb down into hot crevasses to find the stuff. That being said, it is usually pretty ugly and massive material in terms of specimen appeal on the macro level. THIS piece, brought to my attention by my friend Dmitriy Belakovskiy of the Fersman Museum, has rheniite draped liberally on one side of the specimen and actual hardened rock made from the bubbly lava on the other! This shows the origins of the material so well, compared to most rather chunky specimens. Even aside from the lava, it is a really rich specimen with LOTS of bright microcrystalline rheniite. 8.9 x 7.8 x 7.7 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",600,581,{"id":134,"source_url":135,"license_code":126,"credit_html":136,"title":137,"description":138,"author":130,"original_width":139,"original_height":140},20809,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153955","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153955\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-183985.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRheniite\" class=\"extiw\" title=\"en:Rheniite\">Rheniite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kudriavy (Kudryavyi) volcano, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FIturup\" class=\"extiw\" title=\"en:Iturup\">Iturup Island\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKuril_Islands\" class=\"extiw\" title=\"en:Kuril Islands\">Kuril Islands\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSakhalin_Oblast\" class=\"extiw\" title=\"en:Sakhalin Oblast\">Sakhalinskaya Oblast'\u003C\u002Fa>, Far-Eastern Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-10264.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 6.3 x 5.8 x 4.5 cm.\u003C\u002Fdd>\n\u003Cdd>Rheniite is the only known mineral with Rhenium as its primary metallic constituent and as such is a fascinating species. It occurs at a volcanic vent in this remote area of Russia. This is a really rich specimen with lots of silvery bright microcrystalline rheniite.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",374,321,{"id":142,"source_url":143,"license_code":126,"credit_html":144,"title":145,"description":146,"author":130,"original_width":131,"original_height":147},20806,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10144286","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10144286\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-140355.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRheniite\" class=\"extiw\" title=\"en:Rheniite\">Rheniite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kudriavy (Kudryavyi) volcano, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FIturup\" class=\"extiw\" title=\"en:Iturup\">Iturup Island\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKuril_Islands\" class=\"extiw\" title=\"en:Kuril Islands\">Kuril Islands\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSakhalin_Oblast\" class=\"extiw\" title=\"en:Sakhalin Oblast\">Sakhalinskaya Oblast'\u003C\u002Fa>, Far-Eastern Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-10264.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.5 x 4.2 x 3.4 cm.\u003C\u002Fdd>\n\u003Cdd>Rheniite is the only known mineral with Rhenium as its primary metallic constituent and as such is a fascinating species. It occurs at a volcanic vent in this remote area of Russia, and scientists have to climb down into hot crevasses to find the stuff. This is a REALLY RICH specimen with LOTS of silvery bright microcrystalline rheniite.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",531,{"id":149,"source_url":150,"license_code":126,"credit_html":151,"title":152,"description":146,"author":130,"original_width":153,"original_height":154},20807,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10144287","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10144287\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-140357.jpg",488,362,{"id":156,"source_url":157,"license_code":126,"credit_html":158,"title":159,"description":138,"author":130,"original_width":160,"original_height":131},20808,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153954","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153954\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-183984.jpg",529,{"id":162,"source_url":163,"license_code":126,"credit_html":164,"title":165,"description":166,"author":130,"original_width":122,"original_height":167},20810,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159762","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10159762\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-204178.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRheniite\" class=\"extiw\" title=\"en:Rheniite\">Rheniite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kudriavy (Kudryavyi) volcano, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FIturup\" class=\"extiw\" title=\"en:Iturup\">Iturup Island\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKuril_Islands\" class=\"extiw\" title=\"en:Kuril Islands\">Kuril Islands\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSakhalin_Oblast\" class=\"extiw\" title=\"en:Sakhalin Oblast\">Sakhalinskaya Oblast'\u003C\u002Fa>, Far-Eastern Region, Russia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-10264.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 3.9 x 3.7 x 3.3 cm.\u003C\u002Fdd>\n\u003Cdd>Rheniite is the only known mineral with Rhenium as its primary metallic constituent and as such is a fascinating species. It occurs at a volcanic vent in this remote area of Russia, and scientists have to climb down into hot crevasses to find the stuff. This is a really rich specimen with lots of silvery bright microcrystalline rheniite filling the 3-dimensional vug.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",649,{"id":169,"source_url":170,"license_code":126,"credit_html":171,"title":172,"description":173,"author":130,"original_width":174,"original_height":175},20811,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10467141","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10467141\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-tr507c.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRheniite\" class=\"extiw\" title=\"en:Rheniite\">Rheniite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Kudryaviy Volcano, Hurup Island, Kuriles, Russia\u003C\u002Fdd>\n\u003Cdd>Size: small cabinet, 8.9 x 7.8 x 7.7 cm\n\u003Cdl>\u003Cdt>Rheniite on lava\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>Rheniite is the only known mineral with Rhenium as its primary metallic constituent and as such is a fascinating species. It occurs at a volcanic vent in this remote area of Russia, and scientists have to climb down into hot crevasses to find the stuff. That being said, it is usually pretty ugly and massive material in terms of specimen appeal on the macro level. THIS piece, brought to my attention by my friend Dmitriy Belakovskiy of the Fersman Museum, has rheniite draped liberally on one side of the specimen and actual hardened rock made from the bubbly lava on the other! This shows the origins of the material so well, compared to most rather chunky specimens. Even aside from the lava, it is a really rich specimen with LOTS of bright microcrystalline rheniite.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",400,294,{"id":177,"source_url":178,"license_code":126,"credit_html":179,"title":180,"description":173,"author":130,"original_width":174,"original_height":181},20812,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10467142","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10467142\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Rheniite-tr507d.jpg",300,[],[184],"IMA1999-004a",[186,190,194,198,201,206,209,213,217,221,224,228,232],{"lang":187,"names":188},"ca",[189],"reniïta",{"lang":191,"names":192},"cs",[193],"Rheniit",{"lang":195,"names":196},"de",[197,193],"IMA 1999-004a",{"lang":199,"names":200},"de-ch",[193],{"lang":202,"names":203},"es",[204,205],"Reniíta","Rheniita",{"lang":207,"names":208},"eu",[205],{"lang":210,"names":211},"it",[212],"rheniite",{"lang":214,"names":215},"ja",[216],"レニウム鉱",{"lang":218,"names":219},"nl",[220],"rheniiet",{"lang":222,"names":223},"pl",[193],{"lang":225,"names":226},"ru",[227],"Рениит",{"lang":229,"names":230},"ta",[231],"இரேணைட்டு",{"lang":233,"names":234},"zh",[235],"輝錸礦","Q411587",{"history":11,"applications":11}]