[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:4228":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":15,"ima_formula":16,"elements":17,"sigelements":21,"key_elements":11,"impurities":22,"cim":23,"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":33,"dana8ed3":34,"dana8ed4":35,"csystem":36,"cclass":37,"spacegroup":38,"spacegroupset":39,"a":40,"b":41,"c":42,"alpha":43,"beta":43,"gamma":43,"aerror":44,"berror":45,"cerror":46,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":37,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":47,"hmin":11,"hmax":11,"hardtype":11,"vhnmin":43,"vhnmax":43,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":43,"dmeas2":43,"dcalc":48,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":11,"commentluster":11,"diapheny":49,"streak":11,"colour":50,"commentcolor":51,"colors":52,"streak_colors":11,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":11,"tenacity":11,"commentbreak":11,"opticaltype":55,"opticalsign":11,"opticalalpha":43,"opticalalpha2":43,"opticalalphaerror":11,"opticalbeta":56,"opticalbeta2":43,"opticalbetaerror":11,"opticalgamma":43,"opticalgamma2":43,"opticalgammaerror":11,"opticalomega":43,"opticalomega2":43,"opticalomegaerror":11,"opticalepsilon":43,"opticalepsilon2":43,"opticalepsilonerror":11,"opticaln":43,"opticaln2":43,"opticalnerror":11,"optical2vcalc":43,"optical2vcalc2":43,"optical2vcalcerror":11,"optical2vmeasured":43,"optical2vmeasured2":43,"optical2vmeasurederror":11,"rimin":57,"rimax":57,"opticaldispersion":58,"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":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":59,"otheroccurrence":11,"type_specimen_store":60,"description_short":61,"aboutname":62,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":63,"reviewed_at":11,"variety_of":11,"varieties":64,"group_members":65,"associates":66,"confused_with":67,"type_localities":96,"occurrence_total":103,"citations":104,"images":219,"structures":238,"synonyms":266,"language_names":269,"wikidata_qid":331,"texts":332},4228,"1:1:4228:0","198bd3f1-e769-4134-942d-4d898ebd6294","Wadsleyite","Wds",0,"mineral",null,25,false,"Mg\u003Csub>4\u003C\u002Fsub>O(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)","Although the formula is typically written as β-Mg\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub> to emphasize its polymorphic relationship to forsterite, wadsleyite is actually a sorosilicate and not a member of the olivine group. This formula format also better illustrates where hydration of the bridging O occurs in \"hydrous wadsleyite\".","Mg\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>",[18,19,20],"Mg","Si","O",[18,19,20],",Cr,Mn,Ni,Ca,Zn,","14.21.3",[25],"APPROVED",1982,1983,"9","B","E","02","51","3","4","1","Orthorhombic",8,57,"Imma ","5.70","11.71","8.24","0",2,7,4,"Fine-grained aggregates with a grain size of 5 µm.","3.84","Transparent","Light grayish brown","Color of polycrystalline aggregates.",[53,54],"brown","gray","Biaxial","1.76",1.76,"r > v","Found in vein in the Peace River meteorite, believed to have formed from an extraterrestrial shock event.","Department of Geology, University of Alberta, Edmonton, Canada.","The orthorhombic, high-pressure polymorph of Ringwoodite and Forsterite (a member of the Olivine group of minerals). Initially found in the Peace River meteorite (from Alberta, Canada), it is thought to be formed from the transformation of Olivine duri...","It was proposed by Ringwood and Major (1970), who first made synthetic material, that if it was ever found in nature, it should be named after A.D. Wadsley.\r\n\r\nNamed by G.D. Price, A. Putnis, S.O. Agrell, and D.G.W. Smith in 1982 in honor of David Arthur Wadsley (1 August 1918, Hobart, Tasmania, Australia - 6 January 1969 Canberra, Australian Capital Territory, Australia), Australian solid-state chemist and crystallographer, former research scientist of the Commonwealth Scientific and Industrial Research Organization (CSIRO), Australia, for his significant contributions to crystallography, including the concept of crystallographic shearing.","2025-08-11 12:14:24",[],[],[],[68,73,80,84,88],{"id":69,"name":70,"entrytype":9,"csystem":36,"ima_formula":71,"mindat_formula":72,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},53233,"Asimowite","Fe\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>","Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>4\u003C\u002Fsub>O(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>7\u003C\u002Fsub>)",{"id":74,"name":75,"entrytype":9,"csystem":36,"ima_formula":76,"mindat_formula":76,"hmin":45,"hmax":45,"dmeas":77,"dcalc":78,"primary_image_id":79},1584,"Forsterite","Mg\u003Csub>2\u003C\u002Fsub>(SiO\u003Csub>4\u003C\u002Fsub>)","3.275","3.271",29729,{"id":81,"name":82,"entrytype":9,"csystem":36,"ima_formula":11,"mindat_formula":83,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},471230,"Ohtaniite"," Mg\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>0.5\u003C\u002Fsub>◻\u003Csub>0.5\u003C\u002Fsub>)Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>8\u003C\u002Fsub>",{"id":85,"name":86,"entrytype":9,"csystem":36,"ima_formula":16,"mindat_formula":16,"hmin":11,"hmax":11,"dmeas":11,"dcalc":87,"primary_image_id":11},54351,"Poirierite","3.326",{"id":89,"name":90,"entrytype":9,"csystem":91,"ima_formula":92,"mindat_formula":93,"hmin":11,"hmax":11,"dmeas":43,"dcalc":94,"primary_image_id":95},3421,"Ringwoodite","Isometric","SiMg\u003Csub>2\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>","(Mg,Fe\u003Csup>2+\u003C\u002Fsup>)\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>","3.9",20946,[97],{"id":98,"txt":99,"latitude":100,"longitude":101,"country":102},31451,"Peace River meteorite, Peace River, Alberta, Canada",56.1333333,-117.9333333,"Canada",16,[105,109,113,117,120,123,126,130,134,139,144,148,152,156,160,164,168,172,177,181,185,190,194,197,201,206,211,215],{"id":106,"year":107,"html":108,"doi":11},16127669,1966,"Ringwood, A.F., Major, A. (1966) Synthesis of Mg\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>-Fe\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub> spinel solid solutions. Earth and Planetary Science Letters: 1: 241-245.",{"id":110,"year":111,"html":112,"doi":11},16127670,1968,"Akimoto, S. (1968) High-pressure transformations in Co\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub> olivine and some geohysical implications. Physics of the Earth and Planetary Interiors: 1: 498-504.",{"id":114,"year":115,"html":116,"doi":11},16127671,1970,"Ringwood, A.F., Major, A. (1970) The system Mg\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>-Fe\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub> at high pressures and temperatures. Physics of the Earth and Planetary Interiors: 3: 89-108.",{"id":118,"year":115,"html":119,"doi":11},16127672,"Akimoto, S. (1970) High pressure synthesis of a \"modified\" spinel and some geophysical implications. Physics of the Earth and Planetary Interiors: 3: 189-195.",{"id":121,"year":27,"html":122,"doi":11},527828,"Dunn, P.J.; Grice, J.D.; Fleischer, M.; Pabst, A. (1983) New mineral names. \u003Ci>American Mineralogist\u003C\u002Fi>,  68 (9-10). 1038-1041 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM68\u002FAM68_1038.pdf?reftype=.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":124,"year":27,"html":125,"doi":11},16127673,"Price, G.D., Putnis, A., Agrell, S.O., Smith, D.G.W. (1983) Wadsleyite, natural ß-(Mg,Fe)\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub> from the Peace River meteorite. The Canadian Mineralogist: 21: 29-35.",{"id":127,"year":128,"html":129,"doi":11},16127674,1996,"Kudoh, Y., Inoue, T., Arashi, H. (1996) Structure and crystal chemistry of hydrous wadsleyite Mg\u003Csub>1.75\u003C\u002Fsub>SiH\u003Csub>0.5\u003C\u002Fsub>O\u003Csub>4\u003C\u002Fsub>: possible hydrous magnesium silicate in the mantle transition zone. Physics and Chemistry of Minerals: 23: 461-469.",{"id":131,"year":128,"html":132,"doi":133},393468,"Reynard, Bruno; Takir, Fouzia; Guyot, Francois; Gwanmesia, Gabriel D.; Liebermann, Robert C.; Gillet, Philippe (1996) High-temperature Raman spectroscopic and X-ray diffraction study of β–Mg\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>: Insights into its high-temperature thermodynamic properties and the β– to α–phase-transformation mechanism and kinetics. \u003Ci>American Mineralogist\u003C\u002Fi>,  81 (5). 585-594 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-1996-5-605'>doi:10.2138\u002Fam-1996-5-605\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol81\u002FAM81_585.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-1996-5-605",{"id":135,"year":136,"html":137,"doi":138},393587,1997,"Smyth, Joseph R.; Kawamoto, Tatsuhiko; Jacobsen, Stephen D.; Swope, R. Jeffrey; Hervig, Richard L.; Holloway, John R. (1997) Crystal structure of monoclinic hydrous wadsleyite β-(Mg,Fe)\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>. \u003Ci>American Mineralogist\u003C\u002Fi>,  82 (3). 270-275 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-1997-3-404'>doi:10.2138\u002Fam-1997-3-404\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol82\u002FAM82_270.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-1997-3-404",{"id":140,"year":141,"html":142,"doi":143},917578,1998,"Sinogeikin, S. V., Katsura, T., Bass, J. D. (1998) Sound velocities and elastic properties of Fe-bearing wadsleyite and ringwoodite. \u003Ci>Journal of Geophysical Research: Solid Earth\u003C\u002Fi>,  103. 20819-20825 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1029\u002F98jb01819'>doi:10.1029\u002F98jb01819\u003C\u002Fa>","10.1029\u002F98jb01819",{"id":145,"year":146,"html":147,"doi":11},16968043,2001,"(2001) Wadsleyite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fwadsleyite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":149,"year":150,"html":151,"doi":11},16127678,2005,"Demouchy, S., Deloule, E., Frost, D.J., Keppler, H. (2005) Pressure and temperature-dependence of water solubility in Fe-free wadsleyite. American Mineralogist: 90: 1084-1091.",{"id":153,"year":154,"html":155,"doi":11},16127679,2006,"Kleppe, A.K., Jephcoat, A.P., Smyth, J.R. (2006) High-pressure Raman spectroscopic studies of hydrous wadsleyite II. American Mineralogist: 91: 1102-1109.",{"id":157,"year":158,"html":159,"doi":11},16127681,2008,"Nishihara, Y., Shinmei, T., Karato, S.I. (2008) Effect of chemical environment on the hydrogen-related defect chemistry in wadsleyite. American Mineralogist: 93: 831-843.",{"id":161,"year":158,"html":162,"doi":163},396003,"Holl, C. M.; Smyth, J. R.; Jacobsen, S. D.; Frost, D. J. (2008) Effects of hydration on the structure and compressibility of wadsleyite, β-(Mg\u003Csub>2\u003C\u002Fsub>SiO\u003Csub>4\u003C\u002Fsub>). \u003Ci>American Mineralogist\u003C\u002Fi>,  93 (4). 598-607 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2008.2620'>doi:10.2138\u002Fam.2008.2620\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol93\u002FAM93_598.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2008.2620",{"id":165,"year":166,"html":167,"doi":11},16127682,2009,"Tschauner, O., Asimow, P.D., et al. (2009) Ultrafast growth of wadsleyite in shock-produced melts and its implications for early solar system impact processes. PNAS 2009: 0905751106v1-pnas.0905751106.",{"id":169,"year":170,"html":171,"doi":11},16127683,2011,"Sano-Furukawa, A., Kuribayashi, T., Komatsu, K., Yagi, T., Ohtani, E. (2011) Investigation of hydrogen sites of wadsleyite: a neutron diffraction study. Physics of The Earth and Planetary Interiors: 189: 56-62.",{"id":173,"year":174,"html":175,"doi":176},396852,2012,"Trots, D. M., Kurnosov, A., Ballaran, T. B., Frost, D. J. (2012) High-temperature structural behaviors of anhydrous wadsleyite and forsterite. \u003Ci>American Mineralogist\u003C\u002Fi>,  97 (10) 1582-1590 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2012.3992'>doi:10.2138\u002Fam.2012.3992\u003C\u002Fa>","10.2138\u002Fam.2012.3992",{"id":178,"year":179,"html":180,"doi":11},16127685,2013,"Blanchard, M., Roberge, M., Balan, E., Fiquet, G., Bureau, H. (2013) Infrared signatures of OH-defects in wadsleyite: A first-principles study. American Mineralogist: 98: 2132-2143.",{"id":182,"year":183,"html":184,"doi":11},16127686,2014,"Yang, X., Keppler, H., Dubrovinsky, L., Kurnosov, A. (2014) In-situ infrared spectra of hydroxyl in wadsleyite and ringwoodite at high pressure and high temperature. American Mineralogist: 99: 724-729.",{"id":186,"year":187,"html":188,"doi":189},397691,2015,"Kawazoe, Takaaki, Buchen, Johannes, Marquardt, Hauke (2015) Synthesis of large wadsleyite single crystals by solid-state recrystallization. \u003Ci>American Mineralogist\u003C\u002Fi>,  100 (10) 2336-2339 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2015-5400'>doi:10.2138\u002Fam-2015-5400\u003C\u002Fa>","10.2138\u002Fam-2015-5400",{"id":191,"year":192,"html":193,"doi":11},16127688,2016,"Kawazoe, T., Chaudhari, A., Smyth, J.R., McCammon, C. (2016) Coupled substitution of Fe\u003Csup>3+\u003C\u002Fsup> and H\u003Csup>+\u003C\u002Fsup> for Si in wadsleyite: a study by polarized infrared and Mössbauer spectroscopies and single-crystal X-ray diffraction. American Mineralogist: 101: 1236-1239.",{"id":195,"year":192,"html":196,"doi":11},16127689,"Zhang, L., Smyth, J.R., Allaz, J., Kawazoe, T., Jacobsen, S.D., Jin, Z. (2016) Transition Metals in the Transition Zone: Crystal Chemistry of Minor Element Substitution in Wadsleyite. American Mineralogist: 101: 2322-2330.",{"id":198,"year":199,"html":200,"doi":11},16127690,2020,"Gwanmesia, G.D.; Whitaker, M.L.; Dai, L.; James, A.; Chen, H.; Triplett, R.S.; Cai, N. (2020) The Elastic Properties of β-Mg2SiO4 Containing 0.73 wt.% of H\u003Csub>2\u003C\u002Fsub>O to 10 GPa and 600 K by Ultrasonic Interferometry with Synchrotron X-Radiation. Minerals 10, 209.",{"id":202,"year":203,"html":204,"doi":205},12999906,2021,"Martinek, Loïs, Bolfan-Casanova, Nathalie (2021) Water quantification in olivine and wadsleyite by Raman spectroscopy and study of errors and uncertainties. \u003Ci>American Mineralogist\u003C\u002Fi>, 106 (4) 570-580 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2021-7264'>doi:10.2138\u002Fam-2021-7264\u003C\u002Fa>","10.2138\u002Fam-2021-7264",{"id":207,"year":208,"html":209,"doi":210},15192973,2022,"Wang, Wenzhong, Wu, Zhongqing (2022) A first-principles study of water in wadsleyite and ringwoodite: Implication for the 520 km discontinuity. \u003Ci>American Mineralogist\u003C\u002Fi>,  107 (7) 1361-1368 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2021-7929'>doi:10.2138\u002Fam-2021-7929\u003C\u002Fa>","10.2138\u002Fam-2021-7929",{"id":212,"year":213,"html":214,"doi":11},16960820,2023,"Ledoux, Estelle, Krug, Matthias, Gay, Jeffrey, Chantel, Julien, Hilairet, Nadège, Bykov, Maxim, Bykova, Elena, Aprilis, Georgios, Svitlyk, Volodymyr, Garbarino, Gaston, others (2023) In-situ study of microstructures induced by the olivine to wadsleyite transformation at conditions of the 410 km depth discontinuity. \u003Ci>American Mineralogist\u003C\u002Fi>,  108 (12) 2283-2293",{"id":216,"year":213,"html":217,"doi":218},16944557,"Miyajima, Nobuyoshi, Buchen, Johannes, Kawazoe, Takaaki (2023) Twinning in hydrous wadsleyite: Symmetry relations, origin, and consequences. \u003Ci>American Mineralogist\u003C\u002Fi>,  108 (11) 2096-2104 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2022-8596'>doi:10.2138\u002Fam-2022-8596\u003C\u002Fa>","10.2138\u002Fam-2022-8596",[220,230],{"id":221,"source_url":222,"license_code":223,"credit_html":224,"title":225,"description":226,"author":227,"original_width":228,"original_height":229},27707,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=94273166","CC BY-SA 4.0","Zwymmmm, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=94273166\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fe-bearing hydrous wadsleyite .jpg","This is a wadsleyite sample with Fe#=9.4 and 0.14% water contents","Zwymmmm",351,269,{"id":231,"source_url":232,"license_code":223,"credit_html":233,"title":234,"description":235,"author":227,"original_width":236,"original_height":237},27708,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=94612219","Zwymmmm, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=94612219\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hydrous Fe-bearing Wadsleyite.jpg","This is a hydrous Fe-bearing wadsleyite sample under a polarized microscope",584,450,[239,245,251,257,262],{"id":240,"url":241,"label":242,"formula":243,"spacegroup":244,"year":174},14309,"\u002Fcif\u002F14309.cif","Trots 2012","Mg2 Si O4","I m m a",{"id":246,"url":247,"label":248,"formula":249,"spacegroup":250,"year":158},14313,"\u002Fcif\u002F14313.cif","Holl 2008 · Mg1.864 O4.129 Si H.258","Mg1.864 O4.129 Si H.258","I 1 2\u002Fm 1",{"id":252,"url":253,"label":254,"formula":255,"spacegroup":256,"year":158},14314,"\u002Fcif\u002F14314.cif","Holl 2008 · Mg1.89 O4.092 Si H.183","Mg1.89 O4.092 Si H.183","I 1 m m a 1",{"id":258,"url":259,"label":260,"formula":261,"spacegroup":256,"year":158},14315,"\u002Fcif\u002F14315.cif","Holl 2008 · Mg1.961 O4.03 Si H.059","Mg1.961 O4.03 Si H.059",{"id":263,"url":264,"label":265,"formula":243,"spacegroup":256,"year":158},14316,"\u002Fcif\u002F14316.cif","Holl 2008 · Mg2 Si O4",[267,268],"IMA1982-012","Wadsleyiet",[270,274,279,283,286,290,293,296,301,305,310,316,322,325,328],{"lang":271,"names":272},"ca",[273],"wadsleyita",{"lang":275,"names":276},"de",[277,278],"IMA 1982-012","Wadsleyit",{"lang":280,"names":281},"es",[282],"Wadsleyita",{"lang":284,"names":285},"eu",[282],{"lang":287,"names":288},"fa",[289],"وادسلیت",{"lang":291,"names":292},"fr",[7],{"lang":294,"names":295},"it",[7],{"lang":297,"names":298},"ja",[299,300],"ウォズリアイト","ウォズレアイト",{"lang":302,"names":303},"mk",[304],"вадслеит",{"lang":306,"names":307},"ru",[308,309],"Вадслеит","Уэдслиит",{"lang":311,"names":312},"uk",[313,314,315],"вадсліїт","ведсліїт","Уедсліїт",{"lang":317,"names":318},"zh",[319,320,321],"似尖晶橄欖石","瓦兹利石","瓦茲利石",{"lang":323,"names":324},"zh-cn",[320],{"lang":326,"names":327},"zh-hans",[320],{"lang":329,"names":330},"zh-hant",[321],"Q4017643",{"history":11,"applications":11}]