[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3089":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":15,"elements":16,"sigelements":22,"key_elements":23,"impurities":11,"cim":11,"ima_status":24,"ima_notes":11,"ima_history":11,"approval_year":26,"publication_year":27,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":34,"dana8ed3":35,"dana8ed4":36,"csystem":37,"cclass":38,"spacegroup":38,"spacegroupset":39,"a":40,"b":41,"c":42,"alpha":43,"beta":44,"gamma":45,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":46,"z":47,"csmetamict":13,"commentcrystal":11,"twinning":48,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":49,"tlform":50,"hmin":51,"hmax":51,"hardtype":11,"vhnmin":39,"vhnmax":39,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":52,"dmeas2":11,"dcalc":53,"dmeaserror":47,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":54,"commentluster":11,"diapheny":55,"streak":56,"colour":57,"commentcolor":11,"colors":58,"streak_colors":61,"luminescence":11,"uv":62,"cleavage":11,"cleavagetype":63,"fracturetype":11,"tenacity":64,"commentbreak":65,"opticaltype":66,"opticalsign":67,"opticalalpha":68,"opticalalpha2":39,"opticalalphaerror":11,"opticalbeta":69,"opticalbeta2":39,"opticalbetaerror":11,"opticalgamma":70,"opticalgamma2":39,"opticalgammaerror":11,"opticalomega":39,"opticalomega2":39,"opticalomegaerror":11,"opticalepsilon":39,"opticalepsilon2":39,"opticalepsilonerror":11,"opticaln":39,"opticaln2":39,"opticalnerror":11,"optical2vcalc":71,"optical2vcalc2":39,"optical2vcalcerror":11,"optical2vmeasured":72,"optical2vmeasured2":39,"optical2vmeasurederror":11,"rimin":73,"rimax":74,"opticaldispersion":75,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":76,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":77,"industrial":11,"occurrence":78,"otheroccurrence":11,"type_specimen_store":79,"description_short":11,"aboutname":80,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":81,"reviewed_at":11,"variety_of":11,"varieties":82,"group_members":83,"associates":84,"confused_with":95,"type_localities":96,"occurrence_total":47,"citations":103,"images":114,"structures":125,"synonyms":132,"language_names":138,"wikidata_qid":155,"texts":156},3089,"1:1:3089:8","1896d1f2-8522-46e5-b520-9ed9acd45a14","Parafransoletite","Pfsl",0,"mineral",null,36,false,"Ca\u003Csub>3\u003C\u002Fsub>Be\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>3\u003C\u002Fsub>OH)\u003Csub>2\u003C\u002Fsub>·4H\u003Csub>2\u003C\u002Fsub>O","Ca\u003Csub>3\u003C\u002Fsub>Be\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>2\u003C\u002Fsub>(PO\u003Csub>3\u003C\u002Fsub>OH)\u003Csub>2\u003C\u002Fsub> · 4H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20,21],"Be","Ca","O","P","H",[17,18,19,20,21],[17],[25],"APPROVED",1989,1992,"1989","8","C","A","05","40","5","2","1","Triclinic",2,"0","7.32","7.69","7.06","94.9","96.82","101.86",385.48,1,"Simple contact twinning on {010} is common.","Thin individual spear-shaped blades, sheaf- and bowtie-like aggregates, and compact radial sprays. Similar to collinsite in appearance and notably distinct from fransoletite. Most crystals are composite with slightly rounded faces tapering to a pointed termination. Individual crystals are flattened on {010} and elongate parallel to [100]. Forms include \u003Cmi>{010}, {011}, {13_1}, {_131}, and {14_4}\u003C\u002Fmi>. Doubly terminated crystals are common and seemingly exhibit centrosymmetric development of crystal forms.","Thin individual spear-shaped blades up to 0.4 x 0.1 x 0.04 mm, as sheaf- and bowtie-like aggregates, and as compact radial sprays to 2 mm in diameter. It is similar to collinsite in appearance and notably distinct from fransoletite.",2.5,"2.54","2.27","Vitreous,Silky","Transparent,Translucent","White","Colorless, white",[59,60],"colorless","white",[60],"Not fluorescent.","None Observed","brittle","'Even' fracture.","Biaxial","+","1.562","1.564","1.588","34","33",1.562,1.588,"strong","θ = 85°; ψ = –13°; φ = 98°.","Dissolves readily in cold 1:1 HCl.","Granite pegmatite.","Natural History Museum, Los Angeles, California, USA, number 35696.\r\nNational Museum of Natural History, Washington, D.C., USA, number 168432.","Named for its dimorphous relationship with fransoletite.","2026-04-06 18:42:49",[],[],[85],{"id":86,"name":87,"entrytype":9,"csystem":88,"ima_formula":89,"mindat_formula":90,"hmin":91,"hmax":91,"dmeas":92,"dcalc":93,"primary_image_id":94},1383,"Englishite","Monoclinic","K\u003Csub>3\u003C\u002Fsub>Na\u003Csub>2\u003C\u002Fsub>Ca\u003Csub>10\u003C\u002Fsub>Al\u003Csub>15\u003C\u002Fsub>(OH)\u003Csub>7\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>21\u003C\u002Fsub> · 26H\u003Csub>2\u003C\u002Fsub>O","K\u003Csub>3\u003C\u002Fsub>Na\u003Csub>2\u003C\u002Fsub>Ca\u003Csub>10\u003C\u002Fsub>Al\u003Csub>15\u003C\u002Fsub>(PO\u003Csub>4\u003C\u002Fsub>)\u003Csub>21\u003C\u002Fsub>(OH)\u003Csub>7\u003C\u002Fsub>·26H\u003Csub>2\u003C\u002Fsub>O",3,"2.65","2.69",7842,[],[97],{"id":98,"txt":99,"latitude":100,"longitude":101,"country":102},4122,"Tip Top Mine, Fourmile, Custer Mining District, Custer County, South Dakota, USA",43.7155556,-103.6694444,"USA",[104,107,110],{"id":105,"year":27,"html":106,"doi":11},529326,"Kampf, Anthony R., Dunn, Pete J., Foord, Eugene E. (1992) Parafransoletite, a new dimorph of fransoletite from the Tip Top Pegmatite, Custer, South Dakota. \u003Ci>American Mineralogist\u003C\u002Fi>,  77 (7-8) 843-847 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM77\u002FAM77_843.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":108,"year":27,"html":109,"doi":11},529327,"Kampf, Anthony R. (1992) Beryllophosphate chains in the structures of fransoletite, parafransoletite, and ehrleite and some general comments on beryllophosphate linkages. \u003Ci>American Mineralogist\u003C\u002Fi>,  77 (7-8) 848-856 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM77\u002FAM77_848.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":111,"year":112,"html":113,"doi":11},16966533,2005,"(2005) Parafransoletite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fparafransoletite.pdf' class='refpdflink'>\u003C\u002Fa>",[115],{"id":116,"source_url":117,"license_code":118,"credit_html":119,"title":120,"description":121,"author":122,"original_width":123,"original_height":124},18644,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130251032","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=130251032\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Parafransoletite.jpg","Compact radial sprays of white microcrystals of the extremely rare Ca-Be-phosphate mineral parafransoletite from the type and only known locality worldwide in the Tip Top mine (Tip Top Mine, Fourmile, Custer County, South Dakota, United States of America). Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",656,537,[126],{"id":127,"url":128,"label":129,"formula":130,"spacegroup":131,"year":27},10376,"\u002Fcif\u002F10376.cif","Kampf 1992","Ca3 Be2 P4 O20 H10","P -1",[133,134,135,136,137],"IMA1989-049","Parafransoleit","Parafransoleita","Parafransoleite","Parafransoletiet",[139,143,148,152],{"lang":140,"names":141},"ca",[142],"parafransoletita",{"lang":144,"names":145},"de",[146,147],"IMA 1989-049","Parafransoletit",{"lang":149,"names":150},"eu",[151],"Parafransoletita",{"lang":153,"names":154},"it",[7],"Q3895107",{"history":11,"applications":11}]