[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2874":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":16,"ima_formula":17,"elements":18,"sigelements":25,"key_elements":26,"impurities":27,"cim":28,"ima_status":29,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":31,"discovery_year":32,"strunz10ed1":33,"strunz10ed2":34,"strunz10ed3":34,"strunz10ed4":35,"dana8ed1":36,"dana8ed2":37,"dana8ed3":38,"dana8ed4":39,"csystem":40,"cclass":41,"spacegroup":42,"spacegroupset":43,"a":44,"b":45,"c":46,"alpha":45,"beta":45,"gamma":45,"aerror":47,"berror":11,"cerror":48,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":49,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":50,"hmin":47,"hmax":47,"hardtype":11,"vhnmin":45,"vhnmax":45,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":51,"dmeas2":51,"dcalc":52,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":53,"lustretype":54,"commentluster":55,"diapheny":56,"streak":57,"colour":58,"commentcolor":11,"colors":59,"streak_colors":62,"luminescence":11,"uv":63,"cleavage":64,"cleavagetype":65,"fracturetype":11,"tenacity":11,"commentbreak":66,"opticaltype":67,"opticalsign":68,"opticalalpha":45,"opticalalpha2":45,"opticalalphaerror":11,"opticalbeta":45,"opticalbeta2":45,"opticalbetaerror":11,"opticalgamma":45,"opticalgamma2":45,"opticalgammaerror":11,"opticalomega":69,"opticalomega2":45,"opticalomegaerror":70,"opticalepsilon":71,"opticalepsilon2":45,"opticalepsilonerror":70,"opticaln":45,"opticaln2":45,"opticalnerror":11,"optical2vcalc":45,"optical2vcalc2":45,"optical2vcalcerror":11,"optical2vmeasured":45,"optical2vmeasured2":45,"optical2vmeasurederror":11,"rimin":72,"rimax":73,"opticaldispersion":11,"opticalpleochroism":74,"opticalpleochorismdesc":75,"opticalbirefringence":11,"opticalcomments":76,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":77,"description_short":78,"aboutname":79,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":80,"reviewed_at":11,"variety_of":11,"varieties":81,"group_members":82,"associates":117,"confused_with":118,"type_localities":119,"occurrence_total":47,"citations":126,"images":146,"structures":157,"synonyms":158,"language_names":162,"wikidata_qid":192,"texts":193},2874,"1:1:2874:1","c4d2e9a8-a9a0-4a51-858b-181cfeb698cb","Nelenite","Nln",0,"mineral",null,39517,286,false,"(Mn,Fe)\u003Csub>16\u003C\u002Fsub>(Si\u003Csub>12\u003C\u002Fsub>O\u003Csub>30\u003C\u002Fsub>)(OH)\u003Csub>14\u003C\u002Fsub>[As\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>O\u003Csub>6\u003C\u002Fsub>(OH)\u003Csub>3\u003C\u002Fsub>]","In the type material, Fe substitutes for Mn up to 5.8 of the 16 octahedrally coordinated cations.","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>16\u003C\u002Fsub>As\u003Csup>3+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>Si\u003Csub>12\u003C\u002Fsub>O\u003Csub>36\u003C\u002Fsub>(OH)\u003Csub>17\u003C\u002Fsub>",[19,20,21,22,23,24],"As","Fe","Mn","Si","O","H",[19,21,22,23,24],[19],",Zn,Mg,Ca,H2O,","17.7.13",[30],"APPROVED",1984,"1984","9","E","15","72","4","1b","3","Trigonal",13,99,"R-3m ","13.418","0","85.48",5,8,2,"Coarse granular, to 4.5 cm; massive","3.46","3.45","Vitreous, Resinous","Vitreous,Resinous,Dull","Vitreous on cleavages, resinous and duller on fractures.","Transparent","Light brown","Light to medium brown",[60,61],"brown","colorless",[60],"None","Parallel to {0001}","Perfect","Cleavage plates are flat and highly lustrous, and it is this quality and appearance of the cleavage that immediately distinguishes nelenite from the other members of the friedelite group, which have cleavage fragments with slightly or grossly warped and curved surfaces.","Uniaxial","-","1.718",4,"1.700",1.7,1.718,"Visible","with e = colourless and w = light brown.","May appear biaxial.","Holotype material is deposited in the National Museum of\r\nNatural History (Smithsonian Institution), Washington, D.C., USA, under catalog no. C6219. Co-type samples are in the Smithsonian Institution under catalog no. R7824 and at Harvard University, Cambridge, Massachusetts, USA under catalog no. H 92791-a.","Formerly known as ferroschallerite (note: \"ferroschallerite\" with Mn>Fe is Fe-bearing schallerite).","Named in 1984 by Pete J. Dunn and Donald R. Peacor in honor of Joseph A. Nelen (28 Aug 1923 - 7 Jun 2005), chemist at the Smithsonian Institution, Washington, D.C., USA, for his contributions contributions \"to the chemistry of minerals, in particular his analytical studies of the complex arsenosilicates of manganese which are found at Franklin and Sterling Hill.\"  The material was earlier known as ferroschallerite.","2025-12-10 09:54:37",[],[83,92,98,105,111],{"id":84,"name":85,"entrytype":9,"csystem":86,"ima_formula":87,"mindat_formula":88,"hmin":70,"hmax":47,"dmeas":89,"dcalc":90,"primary_image_id":91},1609,"Friedelite","Monoclinic","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>8\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>(OH)\u003Csub>10\u003C\u002Fsub>","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>8\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>(OH,Cl)\u003Csub>10\u003C\u002Fsub>","3.04","3.066",9425,{"id":93,"name":94,"entrytype":9,"csystem":86,"ima_formula":95,"mindat_formula":96,"hmin":47,"hmax":47,"dmeas":45,"dcalc":45,"primary_image_id":97},2613,"Mcgillite","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>8\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>(OH)\u003Csub>8\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>","(Mn,Fe)\u003Csub>8\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>(OH)\u003Csub>8\u003C\u002Fsub>Cl\u003Csub>2\u003C\u002Fsub>",15699,{"id":99,"name":100,"entrytype":9,"csystem":40,"ima_formula":101,"mindat_formula":102,"hmin":103,"hmax":103,"dmeas":45,"dcalc":45,"primary_image_id":104},1525,"Pyrosmalite-(Fe)","Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>8\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>(OH)\u003Csub>10\u003C\u002Fsub>","Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>8\u003C\u002Fsub>Si\u003Csub>6\u003C\u002Fsub>O\u003Csub>15\u003C\u002Fsub>(OH,Cl)\u003Csub>10\u003C\u002Fsub>",4.5,20328,{"id":106,"name":107,"entrytype":9,"csystem":40,"ima_formula":88,"mindat_formula":88,"hmin":70,"hmax":103,"dmeas":108,"dcalc":109,"primary_image_id":110},2491,"Pyrosmalite-(Mn)","3.06","3.14",3975,{"id":112,"name":113,"entrytype":9,"csystem":40,"ima_formula":17,"mindat_formula":114,"hmin":103,"hmax":47,"dmeas":115,"dcalc":52,"primary_image_id":116},3557,"Schallerite","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>16\u003C\u002Fsub>As\u003Csub>3\u003C\u002Fsub>Si\u003Csub>12\u003C\u002Fsub>O\u003Csub>36\u003C\u002Fsub>(OH)\u003Csub>17\u003C\u002Fsub>","3.37",21721,[],[],[120],{"id":121,"txt":122,"latitude":123,"longitude":124,"country":125},3960,"Trotter Mine, Franklin Mine, Franklin, Sussex County, New Jersey, USA",41.1177778,-74.5875,"USA",[127,130,134,138,142],{"id":128,"year":31,"html":129,"doi":11},16901124,"Dunn, Pete J., Peacor, Donald R., Simmons, William B. (1984) Lennilenapeite, the Mg-analogue of stilpnomelane, and chemical data on other stilpnomelane species from Franklin, New Jersey. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  22 (2) 259-263 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM22_259.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":131,"year":31,"html":132,"doi":133},3625,"Dunn, Pete J., Peacor, Donald R. (1984) Nelenite, a manganese arsenosilicate of the friedelite group, polymorphous with schallerite, from Franklin, New Jersey. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  48 (347) 271-275 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1984.048.347.13'>doi:10.1180\u002Fminmag.1984.048.347.13\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_48\u002F48-347-271.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1984.048.347.13",{"id":135,"year":136,"html":137,"doi":11},528143,1985,"Dunn, Pete J., Fleischer, Michael, Langley, Richard H., Shigley, James E., Zilczer, Janet A. (1985) New mineral names. \u003Ci>American Mineralogist\u003C\u002Fi>,  70 (7-8) 871-881 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM70\u002FAM70_871.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":139,"year":140,"html":141,"doi":11},17080552,1995,"Dunn, Pete J. (1995) \u003Ci>Franklin and Sterling Hill, New Jersey: The world's most magnificent mineral deposits\u003C\u002Fi> Vol. 4. The Franklin-Ogdensburg Mineralogical Society.",{"id":143,"year":144,"html":145,"doi":11},16966252,2001,"(2001) Nelenite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fnelenite.pdf' class='refpdflink'>\u003C\u002Fa>",[147],{"id":148,"source_url":149,"license_code":150,"credit_html":151,"title":152,"description":153,"author":154,"original_width":155,"original_height":156},17529,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10160977","CC BY-SA 3.0","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10160977\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Nelenite-213099.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNelenite\" class=\"extiw\" title=\"en:Nelenite\">Nelenite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Trotter Mine (Lehigh Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFranklin\" class=\"extiw\" title=\"en:Franklin\">Franklin\u003C\u002Fa>, Franklin Mining District, Sussex County, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNew_Jersey\" class=\"extiw\" title=\"en:New Jersey\">New Jersey\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3960.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.0 x 2.8 x 1.7 cm.\u003C\u002Fdd>\n\u003Cdd>Nelenite is a very rare silicate found in only two localities worldwide, both in the United States and this specimen is from the Type Locality - the Trotter Mine at Franklin, New Jersey. Brown nelenite is richly dispersed on both sides of the matrix, which includes metallic, black franklinite. Ex. George Elling Collection, a noted Franklin\u002FSterling Hill collector.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",700,531,[],[159,160,161],"Ferroschallerite","IMA1982-011","Neleniet",[163,168,172,177,181,185,188],{"lang":164,"names":165},"ar",[166,167],"نيلينايت","نيلينيت",{"lang":169,"names":170},"ca",[171],"nelenita",{"lang":173,"names":174},"de",[175,176],"IMA 1982-011","Nelenit",{"lang":178,"names":179},"eu",[180],"Nelenita",{"lang":182,"names":183},"fr",[184],"nelenite",{"lang":186,"names":187},"it",[7],{"lang":189,"names":190},"ta",[160,191],"நெலனைட்டு","Q3874416",{"history":11,"applications":11}]