[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:2425":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":11,"ima_formula":16,"elements":17,"sigelements":22,"key_elements":11,"impurities":23,"cim":24,"ima_status":25,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":28,"discovery_year":29,"strunz10ed1":30,"strunz10ed2":31,"strunz10ed3":32,"strunz10ed4":33,"dana8ed1":34,"dana8ed2":35,"dana8ed3":36,"dana8ed4":37,"csystem":38,"cclass":39,"spacegroup":40,"spacegroupset":41,"a":42,"b":41,"c":43,"alpha":41,"beta":41,"gamma":41,"aerror":44,"berror":11,"cerror":45,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":46,"csmetamict":14,"commentcrystal":47,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":48,"tlform":11,"hmin":49,"hmax":49,"hardtype":50,"vhnmin":41,"vhnmax":41,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":51,"dmeas2":51,"dcalc":52,"dmeaserror":50,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":53,"commentluster":11,"diapheny":54,"streak":55,"colour":56,"commentcolor":11,"colors":57,"streak_colors":61,"luminescence":11,"uv":62,"cleavage":63,"cleavagetype":11,"fracturetype":64,"tenacity":65,"commentbreak":66,"opticaltype":67,"opticalsign":68,"opticalalpha":69,"opticalalpha2":70,"opticalalphaerror":11,"opticalbeta":71,"opticalbeta2":41,"opticalbetaerror":11,"opticalgamma":72,"opticalgamma2":73,"opticalgammaerror":11,"opticalomega":41,"opticalomega2":41,"opticalomegaerror":11,"opticalepsilon":41,"opticalepsilon2":41,"opticalepsilonerror":11,"opticaln":41,"opticaln2":41,"opticalnerror":11,"optical2vcalc":41,"optical2vcalc2":74,"optical2vcalcerror":11,"optical2vmeasured":75,"optical2vmeasured2":76,"optical2vmeasurederror":11,"rimin":77,"rimax":78,"opticaldispersion":79,"opticalpleochroism":80,"opticalpleochorismdesc":11,"opticalbirefringence":81,"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":11,"otheroccurrence":82,"type_specimen_store":11,"description_short":83,"aboutname":84,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":85,"reviewed_at":11,"variety_of":11,"varieties":86,"group_members":96,"associates":185,"confused_with":186,"type_localities":191,"occurrence_total":202,"citations":203,"images":317,"structures":453,"synonyms":481,"language_names":486,"wikidata_qid":542,"texts":543},2425,"1:1:2425:5","06b6c13a-2ac9-4385-8e15-060c27a57f95","Lizardite","Lz",0,"mineral",null,11135,4525,false,"Mg\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>","Mg\u003Csub>3\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>",[18,19,20,21],"Mg","Si","O","H",[18,19,20,21],"Al, Ni, Fe","14.4.8",[26,27],"APPROVED","GRANDFATHERED",1951,"1949","9","E","D","15","71","1","2b","2","Trigonal",11,82,"0","5.325","7.259",5,7,2,"Pseudo-orthorhombic. Space group either P31m (1A polytype) with above cell parameters, or P63cm (2H1 polytype), with a = 5.318(4) c = 14.541(7) Å, Z = 4.","Trigonal plates to truncated trigonal pyramids.",2.5,3,"2.55","2.57","Resinous,Waxy,Greasy","Translucent","white","green, brown, light yellow to white",[58,59,60,55],"green","brown","yellow",[55],"Not known to be fluorescent in UV","Rarely observed","Irregular\u002FUneven,Conchoidal,Sub-Conchoidal","flexible","crystals and scales can be easily bent","Biaxial","-","1.541","1.5625","1.565","1.553","1.568","86","37","61",1.541,1.568,"weak to distinct","Non-pleochroic","0.009","It is typically a product of retrograde metamorphism, replacing \u003Cm>olivine\u003C\u002Fm>, \u003Cm>orthopyroxene\u003C\u002Fm> (\u003Cm>enstatite\u003C\u002Fm>), or other minerals in ultramafic igneous rocks.","Lizardite is volumetrically the most common serpentine subgroup species. It is typically a product of retrograde metamorphism, replacing olivine and orthopyroxene (enstatite) in ultramafic igneous rocks and some magnesian skarns.\r\n\r\nCan contain nickel ...","Named in 1956 by Eric James William Whittaker and Jack Zussman for the type location which lies within the area of Cornwall known as the Lizard peninsula. The locality itself being at Eastern Cliff, Kennack, Ruan - Grade, Lizard Peninsula, Cornwall, England, UK. The mineral had been previously described from here by Midgely (1951).","2026-04-16 13:50:59",[87,92],{"id":88,"name":89,"entrytype":46,"csystem":11,"ima_formula":11,"mindat_formula":90,"hmin":11,"hmax":11,"dmeas":41,"dcalc":11,"primary_image_id":91},77,"Al-lizardite","Mg\u003Csub>3\u003C\u002Fsub>((Si,Al)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>",30109,{"id":93,"name":94,"entrytype":46,"csystem":11,"ima_formula":11,"mindat_formula":95,"hmin":11,"hmax":11,"dmeas":11,"dcalc":11,"primary_image_id":11},39965,"Nickel-bearing Lizardite","(Mg,Ni)\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>",[97,105,114,120,127,134,138,145,153,162,170,178],{"id":98,"name":99,"entrytype":9,"csystem":100,"ima_formula":101,"mindat_formula":101,"hmin":49,"hmax":50,"dmeas":102,"dcalc":103,"primary_image_id":104},197,"Amesite","Triclinic","Mg\u003Csub>2\u003C\u002Fsub>Al(AlSiO\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>","2.77","2.7",1100,{"id":106,"name":107,"entrytype":9,"csystem":108,"ima_formula":16,"mindat_formula":15,"hmin":109,"hmax":110,"dmeas":111,"dcalc":112,"primary_image_id":113},260,"Antigorite","Monoclinic",3.5,4,"2.5","2.52",1581,{"id":115,"name":116,"entrytype":9,"csystem":108,"ima_formula":117,"mindat_formula":117,"hmin":49,"hmax":49,"dmeas":41,"dcalc":118,"primary_image_id":119},639,"Berthierine","(Fe\u003Csup>2+\u003C\u002Fsup>,Fe\u003Csup>3+\u003C\u002Fsup>,Al)\u003Csub>3\u003C\u002Fsub>(Si,Al)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","3.06",3130,{"id":121,"name":122,"entrytype":9,"csystem":108,"ima_formula":123,"mindat_formula":123,"hmin":49,"hmax":50,"dmeas":124,"dcalc":125,"primary_image_id":126},774,"Brindleyite","(Ni,Al)\u003Csub>3\u003C\u002Fsub>(Si,Al)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","3.17","3.16",3943,{"id":128,"name":129,"entrytype":9,"csystem":108,"ima_formula":130,"mindat_formula":130,"hmin":50,"hmax":109,"dmeas":131,"dcalc":132,"primary_image_id":133},913,"Caryopilite","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","2.83","2.788",4818,{"id":135,"name":136,"entrytype":9,"csystem":108,"ima_formula":16,"mindat_formula":15,"hmin":49,"hmax":49,"dmeas":41,"dcalc":41,"primary_image_id":137},975,"Chrysotile",5708,{"id":139,"name":140,"entrytype":9,"csystem":38,"ima_formula":141,"mindat_formula":142,"hmin":109,"hmax":109,"dmeas":143,"dcalc":41,"primary_image_id":144},1158,"Cronstedtite","(Fe\u003Csup>2+\u003C\u002Fsup>,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>3\u003C\u002Fsub>(Si,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","Fe\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>((Si,Fe\u003Csup>3+\u003C\u002Fsup>)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>","3.34",29554,{"id":146,"name":147,"entrytype":9,"csystem":108,"ima_formula":148,"mindat_formula":149,"hmin":109,"hmax":110,"dmeas":150,"dcalc":151,"primary_image_id":152},1588,"Fraipontite","(Zn,Al)\u003Csub>3\u003C\u002Fsub>(Si,Al)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","(Zn,Al)\u003Csub>3\u003C\u002Fsub>((Si,Al)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>","3.08","3.49",9339,{"id":154,"name":155,"entrytype":9,"csystem":156,"ima_formula":157,"mindat_formula":158,"hmin":110,"hmax":159,"dmeas":160,"dcalc":161,"primary_image_id":11},39763,"Guidottiite","Hexagonal","Mn\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>(SiFe\u003Csup>3+\u003C\u002Fsup>)O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","Mn\u003Csub>2\u003C\u002Fsub>Fe\u003Csup>3+\u003C\u002Fsup>(Fe\u003Csup>3+\u003C\u002Fsup>SiO\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>",4.5,"3.33","3.264",{"id":163,"name":164,"entrytype":9,"csystem":156,"ima_formula":165,"mindat_formula":166,"hmin":49,"hmax":49,"dmeas":167,"dcalc":168,"primary_image_id":169},2180,"Kellyite","(Mn\u003Csup>2+\u003C\u002Fsup>,Mg,Al)\u003Csub>3\u003C\u002Fsub>(Si,Al)\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","Mn\u003Csup>2+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Al(AlSiO\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>","3.07","3.11",13109,{"id":171,"name":172,"entrytype":9,"csystem":173,"ima_formula":174,"mindat_formula":174,"hmin":46,"hmax":49,"dmeas":175,"dcalc":176,"primary_image_id":177},2882,"Népouite","Orthorhombic","Ni\u003Csub>3\u003C\u002Fsub>Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>(OH)\u003Csub>4\u003C\u002Fsub>","3.24","3.26",17559,{"id":179,"name":180,"entrytype":9,"csystem":108,"ima_formula":174,"mindat_formula":181,"hmin":11,"hmax":11,"dmeas":182,"dcalc":183,"primary_image_id":184},3139,"Pecoraite","Ni\u003Csub>3\u003C\u002Fsub>(Si\u003Csub>2\u003C\u002Fsub>O\u003Csub>5\u003C\u002Fsub>)(OH)\u003Csub>4\u003C\u002Fsub>","3.084","3.47",18965,[],[187,188,189,190],{"id":106,"name":107,"entrytype":9,"csystem":108,"ima_formula":16,"mindat_formula":15,"hmin":109,"hmax":110,"dmeas":111,"dcalc":112,"primary_image_id":113},{"id":128,"name":129,"entrytype":9,"csystem":108,"ima_formula":130,"mindat_formula":130,"hmin":50,"hmax":109,"dmeas":131,"dcalc":132,"primary_image_id":133},{"id":135,"name":136,"entrytype":9,"csystem":108,"ima_formula":16,"mindat_formula":15,"hmin":49,"hmax":49,"dmeas":41,"dcalc":41,"primary_image_id":137},{"id":146,"name":147,"entrytype":9,"csystem":108,"ima_formula":148,"mindat_formula":149,"hmin":109,"hmax":110,"dmeas":150,"dcalc":151,"primary_image_id":152},[192,198],{"id":193,"txt":194,"latitude":195,"longitude":196,"country":197},1354,"Eastern Cliff, Kennack Cove (Kennack Sands), Kennack, Grade-Ruan, Cornwall, England, UK",50.0060152,-5.1607188,"UK",{"id":199,"txt":200,"latitude":11,"longitude":11,"country":201},3769,"North shore of Lake Superior, Minnesota, USA","USA",432,[204,207,210,215,219,223,227,231,236,240,244,248,253,258,263,267,272,277,282,287,292,297,302,307,312],{"id":205,"year":11,"html":206,"doi":11},18590236,"Caruso, L.J. and Chernosky, J.V. (1979) The stability of lizardite. The Canadian Mineralogist, 17 (4), 757–769.",{"id":208,"year":28,"html":209,"doi":11},16147331,"Midgley, H.G. (1951): A serpentine mineral from Kennack Cove, Lizard, Cornwall. Mineralogical Magazine 29, 526-530.",{"id":211,"year":212,"html":213,"doi":214},3941,1956,"Whittaker, E. J. W., Zussman, J. (1956) The characterization of serpentine minerals by X-ray diffraction. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  31 (233) 107-126 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1956.031.233.01'>doi:10.1180\u002Fminmag.1956.031.233.01\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_31\u002F31-233-107.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1956.031.233.01",{"id":216,"year":217,"html":218,"doi":11},524866,1968,"Page, Norman J. (1968) Chemical differences among the serpentine \"polymorphs\". \u003Ci>American Mineralogist\u003C\u002Fi>,  53 (1-2) 201-215 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM53\u002FAM53_201.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":220,"year":221,"html":222,"doi":11},525414,1970,"Whittaker, E. J. W., Wicks, F. J. (1970) Chemical differences among the serpentine \"polymorphs\": A discussion. \u003Ci>American Mineralogist\u003C\u002Fi>,  55 (5-6) 1025-1047 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM55\u002FAM55_1025.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":224,"year":225,"html":226,"doi":11},16100833,1975,"Wicks, F.J. and Whittaker, E.J.W. (1975) A reappraisal of the structures of the serpentine minerals. Canadian Mineralogist: 13(3): 227-243.",{"id":228,"year":229,"html":230,"doi":11},15959345,1976,"Cressey, B.A. and Zussman, J. (1976): Electron microscopic studies of serpentinites. Canadian Mineralogist 14, 307-313. https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol14\u002FCM14_307.pdf",{"id":232,"year":233,"html":234,"doi":235},3245,1981,"Bayliss, Peter (1981) Unit cell data of serpentine group minerals. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  44 (334) 153-156 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1981.044.334.06'>doi:10.1180\u002Fminmag.1981.044.334.06\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_44\u002F44-334-153.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1981.044.334.06",{"id":237,"year":238,"html":239,"doi":11},16115460,1982,"Mellini, M. (1982) The crystal structure of lizardite 1\u003Ci>T\u003C\u002Fi>: hydrogen bonds and polytypism. American Mineralogist: 67: 587-598. https:\u002F\u002Frruff.geo.arizona.edu\u002Fdoclib\u002Fam\u002Fvol67\u002FAM67_587.pdf",{"id":241,"year":242,"html":243,"doi":11},528347,1987,"Mellini, Marcello, Zanazzi, Pier Francesco (1987) Crystal structures of lizardite-\u003Ci>1T\u003C\u002Fi> and lizardite-\u003Ci>2H1\u003C\u002Fi> from Coli, Italy. \u003Ci>American Mineralogist\u003C\u002Fi>,  72 (9-10). 943-948 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM72\u002FAM72_943.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":245,"year":246,"html":247,"doi":11},529741,1994,"Mellini, Marcello, Viti, Cecilia (1994) Crystal structure of lizardite-1\u003Ci>T\u003C\u002Fi> from Elba, Italy. \u003Ci>American Mineralogist\u003C\u002Fi>,  79 (11-12). 1194-1198 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM79\u002FAM79_1194.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":249,"year":250,"html":251,"doi":252},393519,1996,"Gregorkiewitz, M., Lebech, B., Mellini, M., Viti, C. (1996) Hydrogen positions and thermal expansion in lizardite-1\u003Ci>T\u003C\u002Fi> from Elba; a low-temperature study using Rietveld refinement of neutron diffraction data. \u003Ci>American Mineralogist\u003C\u002Fi>,  81 (9). 1111-1116 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-1996-9-1008'>doi:10.2138\u002Fam-1996-9-1008\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol81\u002FAM81_1111.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-1996-9-1008",{"id":254,"year":255,"html":256,"doi":257},393664,1997,"Brigatti, Maria Franca, Galli, Ermanno, Medici, Luca, Poppi, Luciano (1997) Crystal structure refinement of aluminian lizardite-2H2. \u003Ci>American Mineralogist\u003C\u002Fi>,  82 (9) 931-935 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-1997-9-1010'>doi:10.2138\u002Fam-1997-9-1010\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol82\u002FAM82_931.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam-1997-9-1010",{"id":259,"year":260,"html":261,"doi":262},127660,1998,"Benco, L̆ubomír, Smrčok, L̆ubomír (1998) Hartree-Fock study of pressure-induced strengthening of hydrogen bonding in lizardite-1T. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  10 (3) 483-490 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002Fejm\u002F10\u002F3\u002F0483'>doi:10.1127\u002Fejm\u002F10\u002F3\u002F0483\u003C\u002Fa>","10.1127\u002Fejm\u002F10\u002F3\u002F0483",{"id":264,"year":265,"html":266,"doi":11},16965640,2001,"(2001) Lizardite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Flizardite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":268,"year":269,"html":270,"doi":271},394486,2002,"Balan, Etienne, Saitta, A. Marco, Mauri, Francesco, Lemaire, Céline, Guyot, François (2002) First-principles calculation of the infrared spectrum of lizardite. \u003Ci>American Mineralogist\u003C\u002Fi>,  87 (10) 1286-1290 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2002-1003'>doi:10.2138\u002Fam-2002-1003\u003C\u002Fa>","10.2138\u002Fam-2002-1003",{"id":273,"year":274,"html":275,"doi":276},63842,2003,"Rinaudo, C., Gastaldi, D., Belluso, E. (2003) Characterization of chrysotile, antigorite and lizardite by FT-Raman spectroscopy. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  41 (4). 883-890 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.41.4.883'>doi:10.2113\u002Fgscanmin.41.4.883\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol41\u002FCM41_883.pdf' class='refpdflink'>\u003C\u002Fa>","10.2113\u002Fgscanmin.41.4.883",{"id":278,"year":279,"html":280,"doi":281},153083,2004,"Auzende, A.-L., Daniel, I., Reynard, B., Lemaire, C., Guyot, F. (2004) High-pressure behaviour of serpentine minerals: a Raman spectroscopic study. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  31 (5) 269-277 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-004-0384-0'>doi:10.1007\u002Fs00269-004-0384-0\u003C\u002Fa>","10.1007\u002Fs00269-004-0384-0",{"id":283,"year":284,"html":285,"doi":286},64219,2005,"Wicks, F. J., Chatfield, E. J. (2005) Scrolling of thin crystals of lizardite: an expression of internal stress. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  43 (6). 1993-2004 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.43.6.1993'>doi:10.2113\u002Fgscanmin.43.6.1993\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol43\u002FCM43_1993.pdf' class='refpdflink'>\u003C\u002Fa>","10.2113\u002Fgscanmin.43.6.1993",{"id":288,"year":289,"html":290,"doi":291},153297,2006,"Hilairet, N., Daniel, I., Reynard, B. (2006) P–V Equations of State and the relative stabilities of serpentine varieties. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  33 (8) 629-637 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fs00269-006-0111-0'>doi:10.1007\u002Fs00269-006-0111-0\u003C\u002Fa>","10.1007\u002Fs00269-006-0111-0",{"id":293,"year":294,"html":295,"doi":296},396480,2010,"Viti, C. (2010) Serpentine minerals discrimination by thermal analysis. \u003Ci>American Mineralogist\u003C\u002Fi>,  95 (4) 631-638 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2010.3366'>doi:10.2138\u002Fam.2010.3366\u003C\u002Fa>","10.2138\u002Fam.2010.3366",{"id":298,"year":299,"html":300,"doi":301},16100861,2020,"SAKAGUCHI, Ilona, KOUKETSU, Yui, MICHIBAYASHI, Katsuyoshi, WALLIS, Simon R. (2020) Attenuated total reflection infrared (ATR–IR) spectroscopy of antigorite, chrysotile, and lizardite. \u003Ci>Journal of Mineralogical and Petrological Sciences\u003C\u002Fi>,  115 (4). 303-312 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2465\u002Fjmps.190807'>doi:10.2465\u002Fjmps.190807\u003C\u002Fa>","10.2465\u002Fjmps.190807",{"id":303,"year":304,"html":305,"doi":306},17069006,2021,"Fritsch, Emmanuel, Balan, Etienne, Petit, Sabine, Juillot, Farid (2021) Structural, textural, and chemical controls on the OH stretching vibrations in serpentine-group minerals. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  33 (4) 447-462 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-33-447-2021'>doi:10.5194\u002Fejm-33-447-2021\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F33\u002F447\u002F2021\u002Fejm-33-447-2021.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-33-447-2021",{"id":308,"year":309,"html":310,"doi":311},12999734,2022,"Zhang, Hui, Zarzycki, Piotr, Gilbert, Benjamin, Banfield, Jillian F. (2022) Polytypism in semi-disordered lizardite and amesite by low-dose HAADF-STEM. \u003Ci>American Mineralogist\u003C\u002Fi>, 107 (2) 221-232 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2021-7867'>doi:10.2138\u002Fam-2021-7867\u003C\u002Fa>","10.2138\u002Fam-2021-7867",{"id":313,"year":314,"html":315,"doi":316},17180326,2024,"Ji, Shichao, Huang, Fang, Wang, Shaoze, Gupta, Priyantan, Seyfried, William, Zhang, Hejia, Chu, Xu, Cao, Wentao, ZhangZhou, J (2024) Identifying serpentine minerals by their chemical compositions with machine learning. \u003Ci>American Mineralogist\u003C\u002Fi>,  109 (2) 315-324 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2022-8688'>doi:10.2138\u002Fam-2022-8688\u003C\u002Fa>","10.2138\u002Fam-2022-8688",[318,328,338,346,356,366,376,381,386,392,397,402,407,416,424,433,439,445],{"id":319,"source_url":320,"license_code":321,"credit_html":322,"title":323,"description":324,"author":325,"original_width":326,"original_height":327},64811,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=4772055","CC BY-SA 4.0","Piotr Sosnowski, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=4772055\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Marmur 2.jpg","Marmur z mineralizacja serpentynitową reprezentowana przez lizardyt, K. Rędziny, Dolny lsk","Piotr Sosnowski",1506,862,{"id":329,"source_url":330,"license_code":331,"credit_html":332,"title":333,"description":334,"author":335,"original_width":336,"original_height":337},14666,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646314","Public domain","John Krygier, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646314\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lizardite-362595.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLizardite\" class=\"extiw\" title=\"en:Lizardite\">Lizardite\u003C\u002Fa> (Dimensions: 1.25\" x 1\" x 1\")\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Montville, Morris County, New Jersey, USA\u003C\u002Fdd>\n\u003Cdd>Gold-green lizardite from Montville NJ. From a collection assembled in the 1960s by Dr. James R. Mason of Chester VT.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","John Krygier",1024,768,{"id":339,"source_url":340,"license_code":321,"credit_html":341,"title":342,"description":343,"author":325,"original_width":344,"original_height":345},64812,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=4779811","Piotr Sosnowski, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=4779811\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mamrur z lizardytem.jpg","Marmur dolomitowy z mineralizacją serpentynitową reprezentowaną przez lizardyt, Rędziny, Dolny Śląsk",1344,857,{"id":347,"source_url":348,"license_code":349,"credit_html":350,"title":351,"description":352,"author":353,"original_width":354,"original_height":355},64814,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=20231294","CC BY-SA 3.0","Zio, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=20231294\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lizardit.jpg","Lizardite (green) with Magnesite (white) and Hematite (black) from Uppland (Sweden)","Zio",2904,3248,{"id":357,"source_url":358,"license_code":359,"credit_html":360,"title":361,"description":362,"author":363,"original_width":364,"original_height":365},14670,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168134134","CC BY 4.0","Animalculum, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168134134\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lizardite, Musee de Mineralogie, Paris, 2025.jpg","Lizardite from Modum, Buskerud, Norway in Musee de Mineralogie, Paris","Animalculum",1757,2343,{"id":367,"source_url":368,"license_code":369,"credit_html":370,"title":371,"description":372,"author":373,"original_width":374,"original_height":375},3719,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9951751","CC BY 3.0","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9951751\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Stichtite- Lizardite.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FStichtite\" class=\"extiw\" title=\"en:Stichtite\">Stichtite\u003C\u002Fa> and lizardite \n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality:  Stichtite Hill, Dundas mineral field, Zeehan District, Tasmania, Australia\u003C\u002Fdd>\n\u003Cdd>Size :15 × 14 cm.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Didier Descouens",2936,3056,{"id":91,"source_url":377,"license_code":321,"credit_html":378,"title":7,"description":11,"author":11,"original_width":379,"original_height":380},"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F164347","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F164347\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",1000,906,{"id":382,"source_url":383,"license_code":321,"credit_html":384,"title":7,"description":11,"author":11,"original_width":385,"original_height":379},30110,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F164345","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F164345\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",901,{"id":387,"source_url":388,"license_code":331,"credit_html":389,"title":390,"description":391,"author":335,"original_width":336,"original_height":337},14667,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646770","John Krygier, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646770\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lizardite, Chrysotile-288580.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLizardite\" class=\"extiw\" title=\"en:Lizardite\">Lizardite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FChrysotile\" class=\"extiw\" title=\"en:Chrysotile\">Chrysotile\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Dimensions: close-up: 1\" wide, entire specimen 3.5\" x 2\" x 2\"\u003C\u002Fdd>\n\u003Cdd>Locality: Gordon's Crystalline Limestone Quarry, Montville, Morris Co., New Jersey, USA\u003C\u002Fdd>\n\u003Cdd>Vivid, deep green and bronze lizardite. The first child photo shows the entire specimen, with a nicely contrastive streak of pearly chrysotile cutting across it. The second child photo shows the reverse side of the specimen. An old collection specimen with a tag dated 1916 from the John Weigand collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",{"id":393,"source_url":394,"license_code":321,"credit_html":395,"title":7,"description":11,"author":11,"original_width":379,"original_height":396},30111,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F164346","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F164346\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",866,{"id":398,"source_url":399,"license_code":331,"credit_html":400,"title":401,"description":391,"author":335,"original_width":336,"original_height":337},14668,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646775","John Krygier, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646775\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lizardite, Chrysotile-288582.jpg",{"id":403,"source_url":404,"license_code":331,"credit_html":405,"title":406,"description":391,"author":335,"original_width":336,"original_height":337},14669,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646777","John Krygier, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=23646777\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lizardite, Chrysotile-288581.jpg",{"id":408,"source_url":409,"license_code":349,"credit_html":410,"title":411,"description":412,"author":413,"original_width":414,"original_height":415},4317,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=64334500","Giorgio Bortolozzi, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=64334500\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cafetite, Lizardite-529436.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCafetite\" class=\"extiw\" title=\"en:Cafetite\">Cafetite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLizardite\" class=\"extiw\" title=\"en:Lizardite\">Lizardite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Base 0,7 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Val di Serra Quarry, Pilcante, Ala, Lagarina Valley, Trento Province, Trentino-Alto Adige (Trentino-Südtirol), Italy\u003C\u002Fdd>\n\u003Cdd>Original description: Collection and photo Giorgio Bortolozzi\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Giorgio Bortolozzi",721,700,{"id":417,"source_url":418,"license_code":349,"credit_html":419,"title":420,"description":421,"author":413,"original_width":422,"original_height":423},4318,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=64334733","Giorgio Bortolozzi, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=64334733\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cafetite, Lizardite, Calcite-529437.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCafetite\" class=\"extiw\" title=\"en:Cafetite\">Cafetite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLizardite\" class=\"extiw\" title=\"en:Lizardite\">Lizardite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCalcite\" class=\"extiw\" title=\"en:Calcite\">Calcite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Base 4 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Val di Serra Quarry, Pilcante, Ala, Lagarina Valley, Trento Province, Trentino-Alto Adige (Trentino-Südtirol), Italy\u003C\u002Fdd>\n\u003Cdd>Original description: Collection and photo Giorgio Bortolozzi\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",625,511,{"id":425,"source_url":426,"license_code":349,"credit_html":427,"title":428,"description":429,"author":430,"original_width":431,"original_height":432},919,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50402143","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50402143\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Althausite-Hematite-Lizardite-704015.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAlthausite\" class=\"extiw\" title=\"en:Althausite\">Althausite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHematite\" class=\"extiw\" title=\"en:Hematite\">Hematite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLizardite\" class=\"extiw\" title=\"en:Lizardite\">Lizardite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Overntjern Quarry, Overntjern, Modum, Buskerud, Norway\u003C\u002Fdd>\n\u003Cdd>Dimensions: 8.0 cm x 4.0 cm x 3.0 cm\u003C\u002Fdd>\n\u003Cdd>Dark reddish brown, subhedral crystals of althausite to 3cm in a serpentine-talc matrix with dark gray subhedral hematite crystals and aggregates to 2cm. A very good example for the species. Ex. Paulo Matioli collection. Photos by Tom and Melissa Campbell.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",1498,791,{"id":434,"source_url":435,"license_code":349,"credit_html":436,"title":437,"description":429,"author":430,"original_width":336,"original_height":438},920,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50941833","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50941833\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Althausite-Hematite-Lizardite-704016.jpg",557,{"id":440,"source_url":441,"license_code":349,"credit_html":442,"title":443,"description":429,"author":430,"original_width":336,"original_height":444},921,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50941834","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=50941834\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Althausite-Hematite-Lizardite-704017.jpg",544,{"id":446,"source_url":447,"license_code":349,"credit_html":448,"title":449,"description":450,"author":413,"original_width":451,"original_height":452},4316,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=64334379","Giorgio Bortolozzi, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=64334379\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Kassite, Cafetite, Lizardite-529446.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FKassite\" class=\"extiw\" title=\"en:Kassite\">Kassite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCafetite\" class=\"extiw\" title=\"en:Cafetite\">Cafetite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLizardite\" class=\"extiw\" title=\"en:Lizardite\">Lizardite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Base 2 mm\u003C\u002Fdd>\n\u003Cdd>Locality: Val di Serra Quarry, Pilcante, Ala, Lagarina Valley, Trento Province, Trentino-Alto Adige (Trentino-Südtirol), Italy\u003C\u002Fdd>\n\u003Cdd>Original description: Light yellow kassite's spherules with orange-yellow tabular cafetite in lizardite matrix. Collection and photo Giorgio Bortolozzi\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",693,599,[454,461,466,471,476],{"id":455,"url":456,"label":457,"formula":458,"spacegroup":459,"year":460},7829,"\u002Fcif\u002F7829.cif","Laurora 2011 · Si1.896 Al.209 Fe.105 Mg2.787 O9 H4","Si1.896 Al.209 Fe.105 Mg2.787 O9 H4","P 3 1 m",2011,{"id":462,"url":463,"label":464,"formula":465,"spacegroup":459,"year":460},7830,"\u002Fcif\u002F7830.cif","Laurora 2011 · Si1.886 Al.162 Fe.18 Mg2.694 O9 H4","Si1.886 Al.162 Fe.18 Mg2.694 O9 H4",{"id":467,"url":468,"label":469,"formula":470,"spacegroup":459,"year":460},7831,"\u002Fcif\u002F7831.cif","Laurora 2011 · Si1.924 Al.151 Fe.174 Mg2.745 O9 H4","Si1.924 Al.151 Fe.174 Mg2.745 O9 H4",{"id":472,"url":473,"label":474,"formula":475,"spacegroup":459,"year":460},7832,"\u002Fcif\u002F7832.cif","Laurora 2011 · Si1.888 Al.223 Fe.141 Mg2.742 O9 H4","Si1.888 Al.223 Fe.141 Mg2.742 O9 H4",{"id":477,"url":478,"label":479,"formula":480,"spacegroup":459,"year":460},7833,"\u002Fcif\u002F7833.cif","Laurora 2011 · Si1.882 Al.235 Fe.147 Mg2.733 O9 H4","Si1.882 Al.235 Fe.147 Mg2.733 O9 H4",[482,483,484,485],"Lizardiet","Scyelit","Scyelita","Scyelite",[487,491,495,498,502,505,509,512,516,520,523,527,530,533,537],{"lang":488,"names":489},"az",[490],"Lizardit",{"lang":492,"names":493},"ca",[494],"lizardita",{"lang":496,"names":497},"de",[490],{"lang":499,"names":500},"eu",[501],"Lizardita",{"lang":503,"names":504},"fr",[7],{"lang":506,"names":507},"he",[508],"ליזרדיט",{"lang":510,"names":511},"it",[7],{"lang":513,"names":514},"ja",[515],"リザード閃石",{"lang":517,"names":518},"pl",[519],"Lizardyt",{"lang":521,"names":522},"pt",[7],{"lang":524,"names":525},"ru",[526],"лизардит",{"lang":528,"names":529},"sl",[490],{"lang":531,"names":532},"sr",[526],{"lang":534,"names":535},"uk",[536],"Лізардит",{"lang":538,"names":539},"zh",[540,541],"板蛇纹石","蜥蛇紋石","Q2856416",{"history":11,"applications":11}]