[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:55329":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":22,"impurities":11,"cim":11,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":25,"publication_year":26,"discovery_year":11,"strunz10ed1":27,"strunz10ed2":28,"strunz10ed3":29,"strunz10ed4":11,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":30,"cclass":31,"spacegroup":32,"spacegroupset":33,"a":34,"b":11,"c":35,"alpha":11,"beta":11,"gamma":11,"aerror":36,"berror":11,"cerror":37,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":38,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":39,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":11,"vhnmax":11,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":11,"dmeas2":11,"dcalc":40,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":41,"commentluster":11,"diapheny":11,"streak":42,"colour":43,"commentcolor":44,"colors":45,"streak_colors":48,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":11,"opticalalpha2":11,"opticalalphaerror":11,"opticalbeta":11,"opticalbeta2":11,"opticalbetaerror":11,"opticalgamma":11,"opticalgamma2":11,"opticalgammaerror":11,"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":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":11,"opticalanisotropism":11,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":49,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":50,"otheroccurrence":51,"type_specimen_store":52,"description_short":53,"aboutname":54,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":55,"reviewed_at":11,"variety_of":11,"varieties":56,"group_members":57,"associates":58,"confused_with":59,"type_localities":67,"occurrence_total":12,"citations":74,"images":102,"structures":103,"synonyms":104,"language_names":107,"wikidata_qid":117,"texts":118},55329,"1:1:55329:8","2af8fdc4-5667-472c-a7e0-b9bd7c78d1b6","Parahibbingite","Phib",0,"mineral",null,3,false,"Fe\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>3\u003C\u002Fsub>Cl","Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>3\u003C\u002Fsub>Cl",[17,18,19,20],"Cl","Fe","O","H",[17,18,19,20],[17],[24],"APPROVED",2021,2022,"3","D","A","Trigonal",13,99,"R-3m ","6.9362","14.673",4,1,6,"Fine-grained coatings, reaction rims, and aggregates hosted by talc. Also as short, tiny veinlets parallel to the cleavage of cummingtonite. The maximum size of individual aggregates is 100 µm; individual grains are usually less than a few microns in diameter.","3.24","Vitreous","Greyish (synthetic)","Light-blue grey (synthetic)","Covered by a reddish-brown rim of akageneite.",[46,47],"blue","gray",[47],"Unstable in air.","Late hydrothermal alteration of pyroxenite. Fine-grained reaction rims on the contact of orthopyroxene phenocrysts and talc, inside a drill core.","weathering of iron meteorites","Collections of the Mineralogical Museum, Comenius University, Ilkovičova 6, Bratislava 84215, Slovakia, catalogue number 7601","A dimorph of hibbingite.\r\n\r\nVery unstable when in contact with air, oxidizing to iron oxyhydroxides such as akaganéite in just a few hours.","Named for being the β-polymorph of Fe2(OH)3Cl, where the γ-polymorph is \u003Cm>hibbingite\u003C\u002Fm>.","2025-08-11 12:15:23",[],[],[],[60],{"id":61,"name":62,"entrytype":9,"csystem":63,"ima_formula":15,"mindat_formula":15,"hmin":11,"hmax":11,"dmeas":64,"dcalc":65,"primary_image_id":66},1896,"Hibbingite","Orthorhombic","0","3.04",11378,[68],{"id":69,"txt":70,"latitude":71,"longitude":72,"country":73},264837,"Karee Mine, Rustenburg, Rustenburg Local Municipality, Bojanala Platinum District Municipality, North West, South Africa",-25.6713889,27.4713889,"South Africa",[75,79,83,87,91,94,98],{"id":76,"year":77,"html":78,"doi":11},16143359,1964,"Oswald, H.R., Feitknecht, W. (1964) Über die Hydroxidhalogenide Me2(OH)3Cl, -Br, -J zweiwertiget Metalle (Me = Mg, Ni, Co, Cu, Fe, Mn). Helvetica Chimica Acta, 47, 272–289. [synthetic]",{"id":80,"year":81,"html":82,"doi":11},16143360,1995,"Buchwald, V.F., and Koch, C.B. (1995) Hibbingite (β-Fe2(OH)3Cl), a chlorine-rich corrosion product in meteorites and ancient iron objects. Meteoritics, 30(5), 493-493.",{"id":84,"year":85,"html":86,"doi":11},16143361,2008,"Rémazeilles, C., Refait, P. (2008) Formation, fast oxidation and thermodynamic data of Fe(II) hydrochlorides. Corrosion Science, 50, 856-864.",{"id":88,"year":25,"html":89,"doi":90},16082666,"Miyawaki, Ritsuro, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2021) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) – Newsletter 59. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  33 (1) 139-143 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-33-139-2021'>doi:10.5194\u002Fejm-33-139-2021\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F33\u002F139\u002F2021\u002Fejm-33-139-2021.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-33-139-2021",{"id":92,"year":26,"html":93,"doi":11},16966537,"(2022) Parahibbingite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fhandbookofmineralogy.org\u002Fpdfs\u002FParahibbingite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":95,"year":26,"html":96,"doi":97},15193012,"Koděra, Peter, Majzlan, Juraj, Pollok, Kilian, Kiefer, Stefan, Šimko, František, Scholtzová, Eva, Luptáková, Jarmila, Cawthorn, Grant (2022) Ferrous hydroxychlorides hibbingite [γ-Fe2(OH)3Cl] and parahibbingite [β-Fe2(OH)3Cl] as a concealed sink of Cl and H2O in ultrabasic and granitic systems. \u003Ci>American Mineralogist\u003C\u002Fi>, 107 (5) 826-841 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2022-8011'>doi:10.2138\u002Fam-2022-8011\u003C\u002Fa>","10.2138\u002Fam-2022-8011",{"id":99,"year":26,"html":100,"doi":101},15620445,"Margheri, Simone, Bindi, Luca, Bonazzi, Paola, Holtstam, Dan (2022) Structural and spectroscopic study of well-developed crystals of parahibbingite, β-Fe\u003Csub>2\u003C\u002Fsub>(OH)\u003Csub>3\u003C\u002Fsub>Cl, formed from terrestrial weathering of the Muonionalusta iron meteorite. \u003Ci>Mineralogical Magazine\u003C\u002Fi>, 86 (6) 891-896 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fmgm.2022.108'>doi:10.1180\u002Fmgm.2022.108\u003C\u002Fa>","10.1180\u002Fmgm.2022.108",[],[],[105,106],"IMA2020-038a","Parahibbingiet",[108,112],{"lang":109,"names":110},"ca",[111],"parahibbingita",{"lang":113,"names":114},"de",[115,116],"IMA 2020-038a","Parahibbingit","Q105580321",{"history":11,"applications":11}]