[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:470834":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":6,"synid":6,"polytypeof":6,"groupid":6,"weighting":11,"nolocadd":12,"blacklisted":12,"mindat_formula":13,"mindat_formula_note":6,"ima_formula":6,"elements":14,"sigelements":18,"key_elements":19,"impurities":20,"cim":6,"ima_status":21,"ima_notes":6,"ima_history":24,"approval_year":25,"publication_year":6,"discovery_year":6,"strunz10ed1":26,"strunz10ed2":27,"strunz10ed3":28,"strunz10ed4":6,"dana8ed1":6,"dana8ed2":6,"dana8ed3":6,"dana8ed4":6,"csystem":29,"cclass":30,"spacegroup":31,"spacegroupset":32,"a":33,"b":34,"c":35,"alpha":6,"beta":36,"gamma":6,"aerror":37,"berror":37,"cerror":37,"alphaerror":6,"betaerror":37,"gammaerror":6,"va3":6,"z":38,"csmetamict":12,"commentcrystal":6,"twinning":6,"tranglide":6,"parting":39,"epitaxidescription":6,"morphology":6,"tlform":40,"hmin":6,"hmax":6,"hardtype":6,"vhnmin":6,"vhnmax":6,"vhnerror":6,"vhng":6,"vhns":6,"commenthard":6,"dmeas":6,"dmeas2":6,"dcalc":41,"dmeaserror":6,"dcalcerror":6,"commentdense":6,"lustre":6,"lustretype":42,"commentluster":6,"diapheny":43,"streak":44,"colour":45,"commentcolor":6,"colors":46,"streak_colors":48,"luminescence":6,"uv":6,"cleavage":6,"cleavagetype":49,"fracturetype":50,"tenacity":51,"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":52,"opticalcolour":53,"opticalinternal":45,"opticaltropic":6,"opticalanisotropism":54,"opticalbireflectance":55,"opticalextinction":6,"opticalr":56,"specdispm":6,"ir":6,"electrical":6,"magnetism":6,"thermalbehaviour":6,"other":6,"industrial":6,"occurrence":57,"otheroccurrence":6,"type_specimen_store":58,"description_short":59,"aboutname":60,"rock_parent":6,"rock_parent2":6,"rock_root":9,"rock_bgs_code":6,"meteoritical_code":6,"updttime":61,"reviewed_at":6,"variety_of":6,"varieties":62,"group_members":63,"associates":64,"confused_with":65,"type_localities":74,"occurrence_total":81,"citations":82,"images":97,"structures":98,"synonyms":99,"language_names":101,"wikidata_qid":110,"texts":111},470834,"1:1:470834:2",null,"Paramolybdomenite","Pmdm",0,"mineral",7,false,"PbSeO\u003Csub>3\u003C\u002Fsub>",[15,16,17],"Pb","Se","O",[15,16,17],[15,16],"S",[22,23],"APPROVED","PENDING_PUBLICATION","IMA No. 2023-025",2023,"4","J","F","Monoclinic",5,14,"P21\u002Fc ","8.997","8.159","9.032","103.33",1,8,"none","tabular to lamellar crystals up to 0.1 × 0.05 × 0.01 mm and their clusters up to 0.15 mm\r\n\r\nThe crystals demonstrate different signs of the skeletal growth: they are surrounded by fringed aggregates of acicular or columnar tiny subindividuals grown on lateral faces and are typically cavernous, \"waffle-like\"","6.743","Adamantine","Transparent","yellowish","bright yellow",[47],"yellow",[47],"None Observed","Irregular\u002FUneven","brittle","Porosity of paramolybdomenite crystals (Fig. 1) and high values of refractive indices prevented its optical study in transmitted light.","grey","anisotropism is strong, from brownish-yellow to dark brown","Bireflectance is very weak","(11.6,13.9) 470, \r\n(11.2,11.4) 546, \r\n(10.9,11.1) 589, \r\n(10.6,10.7) 650","it is a supergene mineral formed in the weathering zone of the deposits of volcanic fumaroles extinct for a long time.","collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration number 6007\u002F1","Paramolybdomenite is a natural analogue of synthetic α-PbSeO3.\r\n\r\nIn the structure of paramolybdomenite the [Pb2+O9] polyhedra are cross-connected via common edges and are connected via common corners with [Se4+O3] groups to form a quasiframework. Sele...","It was named paramolybdomenite (Cyrillic: парамолибдоменит) due to the dimorphism with molybdomenite, which name originates from the Greek μόλυβδος for \"lead\" and μήυη for \"moon\", because the chemical element selenium is named for the moon.","2026-01-11 12:44:46",[],[],[],[66],{"id":67,"name":68,"entrytype":9,"csystem":29,"ima_formula":69,"mindat_formula":13,"hmin":70,"hmax":70,"dmeas":71,"dcalc":72,"primary_image_id":73},2733,"Molybdomenite","PbSe\u003Csup>4+\u003C\u002Fsup>O\u003Csub>3\u003C\u002Fsub>",3.5,"7.07","7.12",16537,[75],{"id":76,"txt":77,"latitude":78,"longitude":79,"country":80},333762,"Western paleo-fumarole field, Mountain 1004, Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia",55.6717807,160.2310753,"Russia",2,[83,87,92],{"id":84,"year":25,"html":85,"doi":86},16627056,"Bosi, Ferdinando; Hatert, Frédéric; Pasero, Marco; Mills, Stuart J. (2023) Newsletter 74. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  87 (5). 783-787 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2023.54'>doi:10.1180\u002Fmgm.2023.54\u003C\u002Fa>","10.1180\u002Fmgm.2023.54",{"id":88,"year":89,"html":90,"doi":91},17447439,2024,"Zhang, Jingnan; Yang, Hexiong; Gibbs, Ronald B. (2024) Molybdomenite-P21\u002Fc, Polymorphous with Molybdomenite and the Natural Analogue of Synthetic α-PbSe4+O3, from the El Dragón Mine, Potosí, Bolivia. \u003Ci>The Canadian Journal of Mineralogy and Petrology\u003C\u002Fi>,  62 (4). 643-652 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002F2400004'>doi:10.3749\u002F2400004\u003C\u002Fa>","10.3749\u002F2400004",{"id":93,"year":94,"html":95,"doi":96},19122791,2025,"Pekov, Igor V.; Britvin, Sergey N.; Agakhanov, Atali A.; Vigasina, Marina F.; Turchkova, Anna G.; Zhegunov, Pavel S. (2025) Paramolybdomenite, PbSeO\u003Csub>3\u003C\u002Fsub>, a new mineral dimorphous with molybdomenite from the Tolbachik volcano, Kamchatka, Russia. \u003Ci>Mineralogical Magazine\u003C\u002Fi>, 1-22 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2025.10166'>doi:10.1180\u002Fmgm.2025.10166\u003C\u002Fa>","10.1180\u002Fmgm.2025.10166",[],[],[100],"Paramolybdomeniet",[102,106],{"lang":103,"names":104},"ca",[105],"paramolibdomenita",{"lang":107,"names":108},"de",[109],"Paramolybdomenit","Q122943409",{"history":6,"applications":6}]