[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1338":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":21,"key_elements":11,"impurities":11,"cim":22,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":25,"publication_year":25,"discovery_year":26,"strunz10ed1":27,"strunz10ed2":28,"strunz10ed3":29,"strunz10ed4":30,"dana8ed1":31,"dana8ed2":32,"dana8ed3":33,"dana8ed4":34,"csystem":35,"cclass":36,"spacegroup":37,"spacegroupset":38,"a":39,"b":40,"c":41,"alpha":38,"beta":42,"gamma":38,"aerror":43,"berror":44,"cerror":36,"alphaerror":11,"betaerror":45,"gammaerror":11,"va3":46,"z":11,"csmetamict":13,"commentcrystal":47,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":48,"tlform":49,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":38,"vhnmax":38,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":38,"dmeas2":38,"dcalc":50,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":51,"commentluster":11,"diapheny":52,"streak":53,"colour":54,"commentcolor":11,"colors":55,"streak_colors":58,"luminescence":11,"uv":59,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":60,"opticalsign":61,"opticalalpha":62,"opticalalpha2":38,"opticalalphaerror":11,"opticalbeta":63,"opticalbeta2":38,"opticalbetaerror":11,"opticalgamma":64,"opticalgamma2":38,"opticalgammaerror":11,"opticalomega":38,"opticalomega2":38,"opticalomegaerror":11,"opticalepsilon":38,"opticalepsilon2":38,"opticalepsilonerror":11,"opticaln":38,"opticaln2":38,"opticalnerror":11,"optical2vcalc":38,"optical2vcalc2":38,"optical2vcalcerror":11,"optical2vmeasured":38,"optical2vmeasured2":38,"optical2vmeasurederror":11,"rimin":65,"rimax":66,"opticaldispersion":67,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":68,"electrical":11,"magnetism":11,"thermalbehaviour":69,"other":70,"industrial":11,"occurrence":71,"otheroccurrence":72,"type_specimen_store":73,"description_short":74,"aboutname":75,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":76,"reviewed_at":11,"variety_of":11,"varieties":77,"group_members":78,"associates":79,"confused_with":80,"type_localities":81,"occurrence_total":88,"citations":89,"images":150,"structures":170,"synonyms":171,"language_names":174,"wikidata_qid":234,"texts":235},1338,"1:1:1338:9","70bc81b4-739e-45a8-aa9a-ef438d186a94","Dypingite","Dyp",0,"mineral",null,1568,false,"Mg\u003Csub>5\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>·5H\u003Csub>2\u003C\u002Fsub>O","Mg\u003Csub>5\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub> · 5H\u003Csub>2\u003C\u002Fsub>O",[17,18,19,20],"Mg","O","C","H",[17,18,19,20],"11.3.9",[24],"APPROVED",1970,"1961","5","D","A","05","16b","7","2","1","Monoclinic",4,9,"0","8.8593","8.3846","32.655","97.801",2,5,8,2402.7,"Space group and unit cell determined by Sednev-Lugovets et al. (2025). Dehydrated material has the following unit-cell parameters: 8.8317(2), 8.3734(1), 30.041(9), 98.040(2), 2198.4(8).","Forms reniform, botryoidal, oolitic or globular aggregates of radially-divergent acicular to flaky crystals, up to 0.5 mm in size.","Globular aggregates often showing a radiating structure, occurring as a thin surface alteration product on serpentine, resembling hydromagnesite","2.15","Pearly","Translucent","White","White, pale pink",[56,57],"white","pink",[56],"Fluorescent (light blue) with LW\u002FMW\u002FSW and phosphorescent (yellow-green).  The strongest response is with MW.","Biaxial","+","1.508","1.51","1.516",1.508,1.516,"none","Infrared absorption spectrum is very similar to hydromagnesite.  Absorption bands at 3650 cm-1 (OH-); 3510 and 3450 cm-1 (water); 1480, 1420, 1120 (CO32- stretching); 880, 850, 800 (CO32- bending). Bands at 1020 and 940 are characteristic.","Heating to 150 °C, causes dypingite to convert to hydromagnesite.\r\n\r\nDTA curve is very similar to hydromagnesite.  However, dypingite shows two pronounced endothermic peaks at 55 and 125 C.","Easily dissolved in cold dilute HCl with effervescence.","Serpentine-magnesite-deposit in Precambrian rocks","Weathered ultramafic rocks (esp. serpentinites).\r\nDump material and excavations at various ore deposits.\r\nCave assemblages.\r\nSlag material.\r\nBiologially induced by cyanobacteria (Power et al. 2007).","Natural History Museum, Oslo, Norway.","Higher hydrate counterpart of hydromagnesite, chemically very similar to giorgiosite. Also a lower hydrate when compared to 'UM1973-06-CO:MgH'.\r\n\r\nAt the type locality dypingite occurs as a surface alteration product on serpentine; it may be confused w...","Named in 1970 by Gunnar Raade after the type locality, the Dypingdal serpentine-magnesite deposit, Snarum, Modum, Buskerud, Norway. The name is pronounced 'dip-ing-ite'.","2026-04-08 16:47:29",[],[],[],[],[82],{"id":83,"txt":84,"latitude":85,"longitude":86,"country":87},2510,"Dypingdal serpentine-magnesite deposit, Snarum, Modum, Buskerud, Norway",60.064613,9.87591,"Norway",55,[90,93,98,103,107,112,117,122,126,131,136,141,145],{"id":91,"year":25,"html":92,"doi":11},525465,"Raade, Gunnar (1970) Dypingite, a new hydrous basic carbonate of magnesium, from Norway. \u003Ci>American Mineralogist\u003C\u002Fi>,  55 (9-10) 1457-1465 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM55\u002FAM55_1457.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":94,"year":95,"html":96,"doi":97},88411,1973,"Suzuki, Jujin, Ito, Masahiro (1973)  A new magnesium carbonate hydrate mineral, Mg\u003Csub>5\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>·8H\u003Csub>2\u003C\u002Fsub>O,from Yoshikawa, Aichi Prefecture, Japan. \u003Ci>The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists\u003C\u002Fi>,  68 (11) 353-361 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2465\u002Fganko1941.68.353'>doi:10.2465\u002Fganko1941.68.353\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.jstage.jst.go.jp\u002Farticle\u002Fganko1941\u002F68\u002F11\u002F68_11_353\u002F_pdf' class='refpdflink'>\u003C\u002Fa>","10.2465\u002Fganko1941.68.353",{"id":99,"year":100,"html":101,"doi":102},3651,1984,"Canterford, J. H., Tsambourakis, G., Lambert, B. (1984) Some observations on the properties of dypingite, Mg\u003Csub>5\u003C\u002Fsub>(CO\u003Csub>3\u003C\u002Fsub>)\u003Csub>4\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>·5H\u003Csub>2\u003C\u002Fsub>O, and related minerals. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  48 (348) 437-442 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1984.048.348.15'>doi:10.1180\u002Fminmag.1984.048.348.15\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_48\u002F48-348-437.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1984.048.348.15",{"id":104,"year":105,"html":106,"doi":11},16964053,2005,"(2005) Dypingite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fdypingite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":108,"year":109,"html":110,"doi":111},677866,2007,"Power, Ian M, Wilson, Siobhan A, Thom, James M, Dipple, Gregory M, Southam, Gordon (2007) Biologically induced mineralization of dypingite by cyanobacteria from an alkaline wetland near Atlin, British Columbia, Canada. \u003Ci>Geochemical Transactions\u003C\u002Fi>,  8 (13). 1-16 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1186\u002F1467-4866-8-13'>doi:10.1186\u002F1467-4866-8-13\u003C\u002Fa>","10.1186\u002F1467-4866-8-13",{"id":113,"year":114,"html":115,"doi":116},16941660,2008,"Frost, Ray L., Bahfenne, Silmarilly, Graham, Jessica, Reddy, B. Jagannadha (2008) The structure of selected magnesium carbonate minerals – A near infrared and mid-infrared spectroscopic study. \u003Ci>Polyhedron\u003C\u002Fi>,  27 (9) 2069-2076 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.poly.2008.03.019'>doi:10.1016\u002Fj.poly.2008.03.019\u003C\u002Fa>","10.1016\u002Fj.poly.2008.03.019",{"id":118,"year":119,"html":120,"doi":121},2430023,2009,"Frost, Ray L., Bahfenne, Silmarilly, Graham, Jessica (2009) Raman spectroscopic study of the magnesium-carbonate minerals-artinite and dypingite. \u003Ci>Journal of Raman Spectroscopy\u003C\u002Fi>, 40 (8). 855-860 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fjrs.2152'>doi:10.1002\u002Fjrs.2152\u003C\u002Fa>","10.1002\u002Fjrs.2152",{"id":123,"year":124,"html":125,"doi":11},12992160,2012,"Raade, Gunnar (2012) Dypingite, my first mineral - forty-two years later, in \u003Ci>Kongsberg Mineralsymposium 2012\u003C\u002Fi>. \u003Ci>Norsk Bergverksmuseum Skrifter\u003C\u002Fi>,  49. 53-63 \u003Ca target='_blank' href='http:\u002F\u002Fwww.nags.net\u002FMineralsymposium\u002F2012\u002F2012-Raade.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":127,"year":128,"html":129,"doi":130},13735299,2022,"Yamamoto, Gen-ichiro; Kyono, Atsushi; Okada, Satoru (2022) Thermal decomposition process of dypingite Mg5(CO3)4(OH)2·5H2O. \u003Ci>Materials Letters\u003C\u002Fi>,  308. 131125 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.matlet.2021.131125'>doi:10.1016\u002Fj.matlet.2021.131125\u003C\u002Fa>","10.1016\u002Fj.matlet.2021.131125",{"id":132,"year":133,"html":134,"doi":135},17638424,2023,"Lu, Yang, Sednev-Lugovets, Anton, Carvalho, Patricia, Guzik, Matylda, Dunkel, Kristina, Austrheim, Håkon, Friis, Henrik (2023) Dypingite series defined by the content of molecular H\u003Csub>2\u003C\u002Fsub>O. \u003Ci>Goldschmidt2023 abstracts\u003C\u002Fi>, European Association of Geochemistry.  \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.7185\u002Fgold2023.17096'>doi:10.7185\u002Fgold2023.17096\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fgoldschmidtabstracts.info\u002F2023\u002F17096.pdf' class='refpdflink'>\u003C\u002Fa>","10.7185\u002Fgold2023.17096",{"id":137,"year":138,"html":139,"doi":140},19284941,2025,"Lu, Yang; Sednev-Lugovets, Anton; Carvalho, Patricia; Guzik, Matylda N.; Dayaghi, Amir Masoud; Dunkel, Kristina; Austrheim, Håkon; Lin, Zhiyong; Friis, Henrik (2025) Dypingite as a hydration series with reversible change of H2O content. \u003Ci>American Mineralogist\u003C\u002Fi>.  \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2024-9603'>doi:10.2138\u002Fam-2024-9603\u003C\u002Fa>","10.2138\u002Fam-2024-9603",{"id":142,"year":138,"html":143,"doi":144},19284938,"Sednev-Lugovets, Anton; Lu, Yang; Vistad, Ørnulv; Carvalho, Patricia Almeida; Missyul, Alexander; Austrheim, Håkon; Friis, Henrik; Guzik, Matylda N. (2025) The crystal structure of dypingite: understanding the long-range disorder. \u003Ci>Journal of Applied Crystallography\u003C\u002Fi>,  58 (6). 1908-1919 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs1600576725007915'>doi:10.1107\u002Fs1600576725007915\u003C\u002Fa>","10.1107\u002Fs1600576725007915",{"id":146,"year":147,"html":148,"doi":149},19818182,2026,"Sednev-Lugovets, Anton; Lu, Yang; Vistad, Ørnulv; Carvalho, Patricia Almeida; Missyul, Alexander; Austrheim, Håkon; Friis, Henrik; Guzik, Matylda N. (2026) The crystal structure of dypingite: understanding the long-range disorder. Corrigendum. \u003Ci>Journal of Applied Crystallography\u003C\u002Fi>,  59 (2). 705 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs1600576726002438'>doi:10.1107\u002Fs1600576726002438\u003C\u002Fa>","10.1107\u002Fs1600576726002438",[151,160],{"id":152,"source_url":153,"license_code":154,"credit_html":155,"title":156,"description":157,"author":158,"original_width":159,"original_height":159},28529,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1956331","Public domain","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1956331\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Yoshikawaite on serpentine Hydrous basic magnesium carbonate Yoshikawa - Shinoshira shi - Aichi Prefecture Japan 1940.jpg","These mineral images are free to use how you wish.","Dave Dyet http:\u002F\u002Fwww.shutterstone.com http:\u002F\u002Fwww.dyet.com",800,{"id":161,"source_url":162,"license_code":163,"credit_html":164,"title":165,"description":166,"author":167,"original_width":168,"original_height":169},7548,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=66166537","CC BY-SA 4.0","Joan Rosell, from rosellminerals.com, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=66166537\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","RM1631-Dypingita-hidromagnesita-brucita-gualba.jpg",":Estéticos y brillantes agregados de cristales foliáceos, formando rosetas, de intenso color blanco, aunque son incoloros, de dypingita. Se acompañan de gavillas de cristales aplanados de hidromagnesita, entre translúcidos a transparentes, incoloros (recuerdan al aragonito). Todos ellos se disponen sobre una matriz de roca recubierta de una capa con formas botroidales, de color azul a gris, de brucita. Una pieza catalana de las que hoy día cuesta encontrar, con especies poco habituales y con calidad.\n\u003Cdl>\u003Cdd>From: Pedrera de l'Àngel, Montseny massif, Gualba, Barcelona, Catalunya, España\u003C\u002Fdd>\n\u003Cdd>Medidas: 8.5 x 7.0 x 6.0 cm.\u003C\u002Fdd>\n\u003Cdd>Encontrado en 1970's.\u003C\u002Fdd>\n\u003Cdd>Ex. L. Daunis (Barcelona)\u003C\u002Fdd>\n\u003Cdd>Ejemplar con análisis\u003C\u002Fdd>\u003C\u002Fdl>","Joan Rosell, from rosellminerals.com",872,1260,[],[172,173],"IMA1970-011","Yoshikawaite",[175,179,183,188,192,196,199,203,207,210,215,220,223,226,230],{"lang":176,"names":177},"af",[178],"Dypingiet",{"lang":180,"names":181},"ca",[182],"dypingita",{"lang":184,"names":185},"de",[186,187],"Dypingit","IMA 1970-011",{"lang":189,"names":190},"eu",[191],"Dypingita",{"lang":193,"names":194},"fr",[195],"dypingite",{"lang":197,"names":198},"it",[7],{"lang":200,"names":201},"nb",[202],"dypingitt",{"lang":204,"names":205},"nl",[206],"dypingiet",{"lang":208,"names":209},"nn",[202],{"lang":211,"names":212},"ta",[213,214],"டைபிங்கைட்டு","நீரேறிய மக்னீசியம் கார்பனேட்டு",{"lang":216,"names":217},"zh",[218,219],"球碳镁石","碱式碳酸镁",{"lang":221,"names":222},"zh-cn",[219],{"lang":224,"names":225},"zh-hans",[219],{"lang":227,"names":228},"zh-hant",[229],"鹼式碳酸鎂",{"lang":231,"names":232},"zh-tw",[233],"球碳鎂石","Q3716911",{"history":11,"applications":11}]