[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:11467":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":15,"elements":16,"sigelements":20,"key_elements":21,"impurities":11,"cim":11,"ima_status":22,"ima_notes":11,"ima_history":11,"approval_year":24,"publication_year":25,"discovery_year":11,"strunz10ed1":26,"strunz10ed2":27,"strunz10ed3":28,"strunz10ed4":29,"dana8ed1":30,"dana8ed2":30,"dana8ed3":30,"dana8ed4":30,"csystem":31,"cclass":32,"spacegroup":33,"spacegroupset":30,"a":34,"b":30,"c":35,"alpha":30,"beta":30,"gamma":30,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":36,"z":37,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":38,"tlform":39,"hmin":40,"hmax":40,"hardtype":11,"vhnmin":30,"vhnmax":30,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":30,"dmeas2":30,"dcalc":41,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":42,"commentluster":11,"diapheny":11,"streak":43,"colour":44,"commentcolor":11,"colors":45,"streak_colors":47,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":48,"fracturetype":49,"tenacity":50,"commentbreak":11,"opticaltype":51,"opticalsign":11,"opticalalpha":30,"opticalalpha2":30,"opticalalphaerror":11,"opticalbeta":30,"opticalbeta2":30,"opticalbetaerror":11,"opticalgamma":30,"opticalgamma2":30,"opticalgammaerror":11,"opticalomega":30,"opticalomega2":30,"opticalomegaerror":11,"opticalepsilon":30,"opticalepsilon2":30,"opticalepsilonerror":11,"opticaln":30,"opticaln2":30,"opticalnerror":11,"optical2vcalc":30,"optical2vcalc2":30,"optical2vcalcerror":11,"optical2vmeasured":30,"optical2vmeasured2":30,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":52,"opticalpleochorismdesc":11,"opticalbirefringence":53,"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":54,"otheroccurrence":11,"type_specimen_store":55,"description_short":56,"aboutname":57,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":58,"reviewed_at":11,"variety_of":11,"varieties":59,"group_members":60,"associates":95,"confused_with":96,"type_localities":98,"occurrence_total":121,"citations":122,"images":174,"structures":175,"synonyms":176,"language_names":179,"wikidata_qid":199,"texts":200},11467,"1:1:11467:3","8d65515d-9b55-4ec1-b4b3-d64049a0c14f","Reidite","Rei",0,"mineral",null,39501,25,false,"Zr(SiO\u003Csub>4\u003C\u002Fsub>)",[17,18,19],"Si","Zr","O",[17,18,19],[18],[23],"APPROVED",2001,2002,"9","A","D","45","0","Tetragonal",23,136,"4.738","10.506",235.84,4,"skeletal crystals up to 10 µm in length and 0.3 µm in width; also lamellar intergrowths in host zircon crystals.","skeletal crystals replacing zircon. The crystals are up to 10 µm in length and 0.3 µm in width.",7.5,"5.2","Adamantine","white","Colourless",[46,43],"colorless",[43],"None Observed","Irregular\u002FUneven","brittle","Uniaxial","Non-pleochroic","0.015","In upper Eocene impact ejecta layer, probably from the Chesapeake Bay impact structure.","Holotype material is deposited at the Smithsonian Institution (National Museum of Natural History), Washington, D.C., catalog number NMNH 173504.","A high-pressure polymorph of zircon with a scheelite-type structure.\r\n\r\nThe presence of reidite in shocked zircon (in which it may occur as micron-sized lamellae) is evidence of shock pressures in excess of ∼30 GPa.","Named in 2002 by Billy P. Glass, Shaobin Liu, and Peter B. Leavens in honor of Alan Forrest Reid (26 March 1931, Gisborne, New Zealand - 17 January 2013, Adelaide, Australia), Commonwealth Scientific and Industrial Research Organisation (CSIRO), who first produced the phase in high-pressure laboratory experiments in 1969. At CSIRO he was, at different times, Director of Minerals, Energy and Construction; Director of CSIRO's Institute of Energy and Earth Resources; and Chief of the Division of Mineral Engineering. He also analyzed Apollo lunar samples and codescribed the mineral tranquillityite.","2025-11-08 16:57:51",[],[61,70,76,81,89],{"id":62,"name":63,"entrytype":9,"csystem":31,"ima_formula":64,"mindat_formula":65,"hmin":66,"hmax":67,"dmeas":68,"dcalc":30,"primary_image_id":69},1106,"Coffinite","U(SiO\u003Csub>4\u003C\u002Fsub>) · nH\u003Csub>2\u003C\u002Fsub>O","U(SiO\u003Csub>4\u003C\u002Fsub>)·nH\u003Csub>2\u003C\u002Fsub>O",5,6,"5.1",6047,{"id":71,"name":72,"entrytype":9,"csystem":31,"ima_formula":73,"mindat_formula":73,"hmin":40,"hmax":40,"dmeas":30,"dcalc":74,"primary_image_id":75},1792,"Hafnon","Hf(SiO\u003Csub>4\u003C\u002Fsub>)","6.97",10681,{"id":77,"name":78,"entrytype":9,"csystem":31,"ima_formula":79,"mindat_formula":79,"hmin":11,"hmax":11,"dmeas":11,"dcalc":80,"primary_image_id":11},38899,"Stetindite-(Ce)","Ce(SiO\u003Csub>4\u003C\u002Fsub>)","5.03",{"id":82,"name":83,"entrytype":9,"csystem":31,"ima_formula":84,"mindat_formula":84,"hmin":85,"hmax":85,"dmeas":86,"dcalc":87,"primary_image_id":88},3946,"Thorite","Th(SiO\u003Csub>4\u003C\u002Fsub>)",4.5,"6.70","4.40",24127,{"id":90,"name":91,"entrytype":9,"csystem":31,"ima_formula":15,"mindat_formula":15,"hmin":40,"hmax":40,"dmeas":92,"dcalc":93,"primary_image_id":94},4421,"Zircon","4.6","4.714",31046,[],[97],{"id":90,"name":91,"entrytype":9,"csystem":31,"ima_formula":15,"mindat_formula":15,"hmin":40,"hmax":40,"dmeas":92,"dcalc":93,"primary_image_id":94},[99,105,110,115],{"id":100,"txt":101,"latitude":102,"longitude":103,"country":104},33076,"Deep Sea Drilling Project Site 612, Upper continental slope of New Jersey, Atlantic Ocean",38.8166667,-72.7833333,"Atlantic Ocean",{"id":106,"txt":107,"latitude":108,"longitude":109,"country":104},33077,"Ocean Drilling Program Hole 903C, Upper continental slope of New Jersey, Atlantic Ocean",38.9333333,-72.8166667,{"id":111,"txt":112,"latitude":113,"longitude":114,"country":104},33078,"Ocean Drilling Program Hole 904A, Upper continental slope of New Jersey, Atlantic Ocean",38.8666667,-72.7666667,{"id":116,"txt":117,"latitude":118,"longitude":119,"country":120},33079,"Bath Cliff, Saint John Parish, Barbados",13.1912396,-59.4820349,"Barbados",20,[123,128,132,137,142,147,152,156,160,164,169],{"id":124,"year":125,"html":126,"doi":127},361606,1969,"Reid, A.F., Ringwood, A.E. (1969) Newly observed high pressure transformations in Mn3O4, CaAl2O4, and ZrSiO4. \u003Ci>Earth and Planetary Science Letters\u003C\u002Fi>,  6 (3) 205-208 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002F0012-821x(69)90091-0'>doi:10.1016\u002F0012-821x(69)90091-0\u003C\u002Fa>","10.1016\u002F0012-821x(69)90091-0",{"id":129,"year":25,"html":130,"doi":131},394580,"Glass, Billy P., Liu, Shaobin, Leavens, Peter B. (2002) Reidite: An impact-produced high-pressure polymorph of zircon found in marine sediments. \u003Ci>American Mineralogist\u003C\u002Fi>,  87 (4) 562-565 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2002-0420'>doi:10.2138\u002Fam-2002-0420\u003C\u002Fa>","10.2138\u002Fam-2002-0420",{"id":133,"year":134,"html":135,"doi":136},63824,2003,"Mandarino, Joseph A. (2003) New minerals. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  41 (3) 803-828 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2113\u002Fgscanmin.41.3.803'>doi:10.2113\u002Fgscanmin.41.3.803\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fcm\u002Fvol41\u002FCM41_803.pdf' class='refpdflink'>\u003C\u002Fa>","10.2113\u002Fgscanmin.41.3.803",{"id":138,"year":139,"html":140,"doi":141},243574,2004,"Gucsik, A., Zhang, M., Koeberl, C., Salje, E. K. H., Redfern, S. A. T., Pruneda, J. M. (2004) Infrared and Raman spectra of ZrSiO\u003Csub>4\u003C\u002Fsub> experimentally shocked at high pressures. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  68 (5) 801-811 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002F0026461046850220'>doi:10.1180\u002F0026461046850220\u003C\u002Fa>","10.1180\u002F0026461046850220",{"id":143,"year":144,"html":145,"doi":146},333108,2008,"GLASS, Billy P., FRIES, Marc (2008) Micro-Raman spectroscopic study of fine-grained, shock-metamorphosed rock fragments from the Australasian microtektite layer. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  43 (9) 1487-1496 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1945-5100.2008.tb01023.x'>doi:10.1111\u002Fj.1945-5100.2008.tb01023.x\u003C\u002Fa>","10.1111\u002Fj.1945-5100.2008.tb01023.x",{"id":148,"year":149,"html":150,"doi":151},333915,2013,"Chen, Ming, Yin, Feng, Li, Xiaodong, Xie, Xiande, Xiao, Wansheng, Tan, Dayong (2013) Natural occurrence of reidite in the Xiuyan crater of China. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  48 (5) 796-805 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fmaps.12106'>doi:10.1111\u002Fmaps.12106\u003C\u002Fa>","10.1111\u002Fmaps.12106",{"id":153,"year":154,"html":155,"doi":11},16133327,2015,"en.wikipedia.org (2015) \u003Ca target='_blank' rel='nofollow' href='https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FReidite'>https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FReidite\u003C\u002Fa>",{"id":157,"year":154,"html":158,"doi":159},142577,"Reddy, S.M., Johnson, T.E., Fischer, S., Rickard, W.D.A., Taylor, R.J.M. (2015) Precambrian reidite discovered in shocked zircon from the Stac Fada impactite, Scotland. \u003Ci>Geology\u003C\u002Fi>,  43 (10) 899-902 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1130\u002Fg37066.1'>doi:10.1130\u002Fg37066.1\u003C\u002Fa>","10.1130\u002Fg37066.1",{"id":161,"year":162,"html":163,"doi":11},16966957,2021,"(2021) Reidite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002FReidite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":165,"year":166,"html":167,"doi":168},15598244,2022,"Gao, Yue, Zheng, Zhi, Zhao, Xia, Liu, Yuegao, Chen, Jiangzhi, Li, Yan, Xiong, Mengjun, Zu, Xiaotao, Mei, Shenghua (2022) In Situ Raman Spectroscopy and DFT Studies of the Phase Transition from Zircon to Reidite at High P–T Conditions. \u003Ci>Minerals\u003C\u002Fi>, 12 (12) 1618 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin12121618'>doi:10.3390\u002Fmin12121618\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F12\u002F12\u002F1618\u002Fpdf?version=1671603831' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin12121618",{"id":170,"year":171,"html":172,"doi":173},19172249,2025,"Roddatis, Vladimir; Kovaleva, Elizaveta; Syczewski, Marcin D.; Schreiber, Anja; Wirth, Richard (2025) Nanoscale mapping of ZrSiO4 phases in naturally shocked zircon using electron energy loss spectroscopy. \u003Ci>American Mineralogist\u003C\u002Fi>,  110 (11). 1728-1736 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2024-9455'>doi:10.2138\u002Fam-2024-9455\u003C\u002Fa>","10.2138\u002Fam-2024-9455",[],[],[177,178],"IMA2001-013","Reidiet",[180,184,189,193,196],{"lang":181,"names":182},"ca",[183],"reidita",{"lang":185,"names":186},"de",[187,188],"IMA 2001-013","Reidit",{"lang":190,"names":191},"eu",[192],"Reidita",{"lang":194,"names":195},"it",[7],{"lang":197,"names":198},"pt",[7],"Q3932203",{"history":11,"applications":11}]