[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:43899":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":21,"key_elements":22,"impurities":23,"cim":11,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":26,"publication_year":27,"discovery_year":11,"strunz10ed1":28,"strunz10ed2":29,"strunz10ed3":30,"strunz10ed4":31,"dana8ed1":32,"dana8ed2":32,"dana8ed3":32,"dana8ed4":32,"csystem":33,"cclass":34,"spacegroup":35,"spacegroupset":36,"a":37,"b":38,"c":39,"alpha":11,"beta":11,"gamma":40,"aerror":41,"berror":42,"cerror":43,"alphaerror":11,"betaerror":11,"gammaerror":44,"va3":45,"z":43,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":46,"tlform":47,"hmin":48,"hmax":48,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":49,"dmeas2":49,"dcalc":50,"dmeaserror":43,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":51,"commentluster":11,"diapheny":52,"streak":53,"colour":54,"commentcolor":11,"colors":55,"streak_colors":59,"luminescence":11,"uv":11,"cleavage":60,"cleavagetype":61,"fracturetype":11,"tenacity":62,"commentbreak":63,"opticaltype":64,"opticalsign":65,"opticalalpha":66,"opticalalpha2":11,"opticalalphaerror":42,"opticalbeta":11,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":67,"opticalgamma2":11,"opticalgammaerror":68,"opticalomega":11,"opticalomega2":11,"opticalomegaerror":11,"opticalepsilon":11,"opticalepsilon2":11,"opticalepsilonerror":11,"opticaln":11,"opticaln2":11,"opticalnerror":11,"optical2vcalc":11,"optical2vcalc2":11,"optical2vcalcerror":11,"optical2vmeasured":11,"optical2vmeasured2":11,"optical2vmeasurederror":11,"rimin":69,"rimax":70,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":71,"opticalbirefringence":11,"opticalcomments":72,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":73,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":74,"industrial":11,"occurrence":75,"otheroccurrence":11,"type_specimen_store":76,"description_short":77,"aboutname":78,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":79,"reviewed_at":11,"variety_of":11,"varieties":80,"group_members":81,"associates":82,"confused_with":83,"type_localities":84,"occurrence_total":42,"citations":91,"images":104,"structures":105,"synonyms":112,"language_names":115,"wikidata_qid":133,"texts":134},43899,"1:1:43899:9","7f813db0-ce5f-4e87-b649-c91dbdbf5555","Parawulffite","Pwlf",0,"mineral",null,32,false,"K\u003Csub>5\u003C\u002Fsub>Na\u003Csub>3\u003C\u002Fsub>Cu\u003Csub>8\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>",[16,17,18,19,20],"Cu","Na","O","K","S",[16,17,18,19,20],[16],"Rb, Cs",[25],"APPROVED",2013,2014,"7","B","C","60","0","Monoclinic",5,12,"P2\u002Fc "," 13.904"," 4.9765"," 23.586"," 90.209",1,3,2,6,1631.98,"Imperfect prismatic crystals up to 0.4 × 0.2 mm, in clusters and crusts; [010] elongation often observed; commonly curved, blocky character.","Crude crystals or irregularly shaped grains.",2.5,"3.35","3.32","Vitreous","Transparent","Light green","Dark green or deep emerald-green",[56,57,58],"green","blue","colorless",[56],"One parallel to elongation, second coplanar with (010).","Perfect","brittle","Laminated fracture","Biaxial","+","1.585","1.717",4,1.585,1.717,"Z = very strong, deep emerald-green; X = very pale green, almost colourless.","Absorption: Z > X.\r\n\r\nThe perfect cleavage parallel to the elongation (causing laminated fracturing) and the very strong pleochroism prevented measurement of β and 2V values.","[cm\u003Csup>-1\u003C\u002Fsup>]: 1212s, 1202s, 1149s, 1116s (asymmetric stretching of sulfate), 1036s, 1006s, 981s [symmetric stretching of sulfate), 690, 665, 642, 618, 572, 550 (bending of sulfate),  503, 450 [lattice modes: stretching of shorter bonds in Cu-center","Slowly dissolves in room temperature water.","Incrustations on basalt scoria and on hematite.","Type material is deposited in the collections of the Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia, registration number 4386\u002F1.","Related to wulffite both chemically and structurally. One of four K-Na-Cu sulfate minerals beside euchlorine, piypite, and wulffite.\r\n\r\nStructure details: (1) the heteropolyhedral quasi-framework of Cu–O–S, along [010], and Na(1)O6 octahedra chains ; (...","After its relation to wulffite. Para, after the greek παρά, beside and wulffite (which is named in honor of the Russian crystallographer Georgiy Viktorovich Wulff (1863–1925)).","2025-08-11 12:15:10",[],[],[],[],[85],{"id":86,"txt":87,"latitude":88,"longitude":89,"country":90},2656,"Yadovitaya fumarole, Second scoria cone, Northern Breakthrough (North Breach), Great Fissure eruption (Main Fracture), Tolbachik Volcanic field, Milkovsky District, Kamchatka Krai, Russia",55.8333333,160.3333333,"Russia",[92,96,100],{"id":93,"year":26,"html":94,"doi":95},244456,"Williams, P. A., Hatert, F., Pasero, M., Mills, S. J. (2013) New minerals and nomenclature modifications approved in 2013. CNMNC Newsletter No.17. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  77 (7) 2997-3005 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2013.077.7.09'>doi:10.1180\u002Fminmag.2013.077.7.09\u003C\u002Fa>","10.1180\u002Fminmag.2013.077.7.09",{"id":97,"year":27,"html":98,"doi":99},65210,"Pekov, I. V., Zubkova, N. V., Yapaskurt, V. O., Belakovskiy, D. I., Chukanov, N. V., Lykova, I. S., Savelyev, D. P., Sidorov, E. G., Pushcharovsky, D. Y. (2014) Wulffite, K\u003Csub>3\u003C\u002Fsub>NaCu\u003Csub>4\u003C\u002Fsub>O\u003Csub>2\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>, and parawulffite, K\u003Csub>5\u003C\u002Fsub>Na\u003Csub>3\u003C\u002Fsub>Cu\u003Csub>8\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>(SO\u003Csub>4\u003C\u002Fsub>)\u003Csub>8\u003C\u002Fsub>, two new minerals from fumarole sublimates of the Tolbachik Volcano, Kamchatka, Russia. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  52 (4) 699-716 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.1400018'>doi:10.3749\u002Fcanmin.1400018\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM52_699.pdf' class='refpdflink'>\u003C\u002Fa>","10.3749\u002Fcanmin.1400018",{"id":101,"year":102,"html":103,"doi":11},16966577,2016,"(2016) Parawulffite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fparawulffite.pdf' class='refpdflink'>\u003C\u002Fa>",[],[106],{"id":107,"url":108,"label":109,"formula":110,"spacegroup":111,"year":27},10436,"\u002Fcif\u002F10436.cif","Pekov 2014","Na2.95 K4.75 Rb.25 Cs.14 Cu7.95 Zn.04 S8 O36","P 1 2\u002Fc 1",[113,114],"IMA2013-036","Parawulffiet",[116,120,125,129],{"lang":117,"names":118},"ca",[119],"parawulffita",{"lang":121,"names":122},"de",[123,124],"IMA 2013-036","Parawulffit",{"lang":126,"names":127},"eu",[128],"Parawulffita",{"lang":130,"names":131},"it",[132],"parawulffite","Q19861154",{"history":11,"applications":11}]