[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:3296":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":14,"elements":15,"sigelements":19,"key_elements":20,"impurities":11,"cim":21,"ima_status":22,"ima_notes":24,"ima_history":26,"approval_year":11,"publication_year":27,"discovery_year":28,"strunz10ed1":29,"strunz10ed2":30,"strunz10ed3":31,"strunz10ed4":32,"dana8ed1":33,"dana8ed2":29,"dana8ed3":34,"dana8ed4":35,"csystem":36,"cclass":37,"spacegroup":38,"spacegroupset":39,"a":40,"b":39,"c":41,"alpha":39,"beta":39,"gamma":39,"aerror":42,"berror":11,"cerror":43,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":42,"csmetamict":13,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":44,"tlform":11,"hmin":45,"hmax":45,"hardtype":11,"vhnmin":39,"vhnmax":39,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":46,"dmeas2":46,"dcalc":47,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":48,"commentluster":11,"diapheny":49,"streak":50,"colour":51,"commentcolor":11,"colors":52,"streak_colors":57,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":11,"fracturetype":58,"tenacity":59,"commentbreak":11,"opticaltype":60,"opticalsign":11,"opticalalpha":39,"opticalalpha2":39,"opticalalphaerror":11,"opticalbeta":39,"opticalbeta2":39,"opticalbetaerror":11,"opticalgamma":39,"opticalgamma2":39,"opticalgammaerror":11,"opticalomega":39,"opticalomega2":39,"opticalomegaerror":11,"opticalepsilon":39,"opticalepsilon2":39,"opticalepsilonerror":11,"opticaln":39,"opticaln2":39,"opticalnerror":11,"optical2vcalc":39,"optical2vcalc2":39,"optical2vcalcerror":11,"optical2vmeasured":39,"optical2vmeasured2":39,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":61,"opticalpleochorismdesc":62,"opticalbirefringence":11,"opticalcomments":63,"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":64,"industrial":11,"occurrence":11,"otheroccurrence":11,"type_specimen_store":65,"description_short":66,"aboutname":67,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":68,"reviewed_at":11,"variety_of":11,"varieties":69,"group_members":77,"associates":78,"confused_with":79,"type_localities":89,"occurrence_total":96,"citations":97,"images":170,"structures":181,"synonyms":188,"language_names":190,"wikidata_qid":206,"texts":207},3296,"1:1:3296:0","f578c40b-1196-4897-b458-825d7d822ddd","Pseudorutile","Pdrt",0,"mineral",null,56,false,"Fe\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>Ti\u003Csup>4+\u003C\u002Fsup>\u003Csub>3\u003C\u002Fsub>O\u003Csub>9\u003C\u002Fsub>",[16,17,18],"Fe","Ti","O",[16,17,18],[17],"7.9.18",[23],"APPROVED",[25],"REDEFINED","Redefined 1994 s.p.: Grey et al. (1994).",1966,"1994","4","C","B","25","8","2","1","Hexagonal",19,120,"0","14.375","4.615",6,3,"thin, irregular plates having fibrous texture; fine-grained, massive.",5.5,"3.8","4.82","Metallic,Sub-Metallic","Opaque","Reddish brown","Dark steel-gray on fresh fractures, light brown to black",[53,54,55,56],"gray","brown","black","red",[56,54],"Sub-Conchoidal","brittle","Uniaxial","Weak","very weak in reds","n = ∼2.62","magnetic","Museum Victoria, Melbourne, Australia, M42789.","Closely related to kleberite. Chemically, but not structurally, the Fe analogue of machiite and schreyerite. The Fe analogue of (the Mn dominant) UM2004-26-O:FeMnTi.\r\nCompare the chemically similar carmichaelite.\r\n\r\nSee also Arizonite (of Palmer).","Named for the relation to rutile.","2025-11-21 18:32:26",[70],{"id":71,"name":72,"entrytype":73,"csystem":11,"ima_formula":11,"mindat_formula":74,"hmin":75,"hmax":76,"dmeas":39,"dcalc":11,"primary_image_id":11},7138,"Hydroxylian Pseudorutile",2,"FeTi\u003Csub>6\u003C\u002Fsub>O\u003Csub>13\u003C\u002Fsub>&middot;4H\u003Csub>2\u003C\u002Fsub>O ?",4,4.5,[],[],[80],{"id":81,"name":82,"entrytype":9,"csystem":83,"ima_formula":84,"mindat_formula":85,"hmin":11,"hmax":11,"dmeas":86,"dcalc":87,"primary_image_id":88},10804,"Kleberite","Monoclinic","Fe\u003Csup>3+\u003C\u002Fsup>Ti\u003Csub>6\u003C\u002Fsub>O\u003Csub>11\u003C\u002Fsub>(OH)\u003Csub>5\u003C\u002Fsub>","FeTi\u003Csub>6\u003C\u002Fsub>O\u003Csub>11\u003C\u002Fsub>(OH)\u003Csub>5\u003C\u002Fsub>","3.28","3.91",13430,[90],{"id":91,"txt":92,"latitude":93,"longitude":94,"country":95},12491,"South Neptune Island, South Australia, Australia",-35.3333333,136.1166667,"Australia",30,[98,103,107,111,115,120,125,129,134,138,143,147,151,156,161,165],{"id":99,"year":100,"html":101,"doi":102},4081208,1959,"KARKHANAVALA, M. D., MOMIN, A. C. (1959) Subsolidus Reactions in the System Fe2O3- TiO2. \u003Ci>Journal of the American Ceramic Society\u003C\u002Fi>, 42 (8). 399-402 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1151-2916.1959.tb13600.x'>doi:10.1111\u002Fj.1151-2916.1959.tb13600.x\u003C\u002Fa>","10.1111\u002Fj.1151-2916.1959.tb13600.x",{"id":104,"year":27,"html":105,"doi":106},2541396,"TEUFER, G.; TEMPLE, A. K. (1966) Pseudorutile—a New Mineral Intermediate between Ilmenite and Rutile in the Natural Alteration of Ilmenite. \u003Ci>Nature\u003C\u002Fi>,  211 (5045). 179-181 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1038\u002F211179b0'>doi:10.1038\u002F211179b0\u003C\u002Fa>","10.1038\u002F211179b0",{"id":108,"year":109,"html":110,"doi":11},16120754,1971,"Larrett, M.J.W., Spencer, W.G. (1971) Contributions to Australasian Mineralogy, 3. \"Pseudorutile\" from South Neptune Island, South Australia. Amdel Bulletin: 12: 74-80.",{"id":112,"year":113,"html":114,"doi":11},526543,1975,"Grey, Ian E., Reid, Alan F. (1975) The structure of pseudorutile and its role in the natural alteration of ilmenite. \u003Ci>American Mineralogist\u003C\u002Fi>,  60 (9-10) 898-906 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM60\u002FAM60_898.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":116,"year":117,"html":118,"doi":119},3110,1980,"Wort, M. J., Jones, M. P. (1980) X-ray diffraction and magnetic studies of altered ilmenite and pseudorutile. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  43 (329) 659-663 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1980.043.329.16'>doi:10.1180\u002Fminmag.1980.043.329.16\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_43\u002F43-329-659.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1980.043.329.16",{"id":121,"year":122,"html":123,"doi":124},15874,1991,"Melcher, F. (1991) Fe-Ti-Oxide assemblages in the basal parts of the Central Alpine Brenner Mesozoic, Tyrol\u002FAustria. \u003Ci>Mineralogy and Petrology\u003C\u002Fi>,  44 (3) 197-212 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf01166963'>doi:10.1007\u002Fbf01166963\u003C\u002Fa>","10.1007\u002Fbf01166963",{"id":126,"year":122,"html":127,"doi":128},239541,"Mücke, A.; Bhadra Chaudhuri, J.N. (1991) The continuous alteration of ilmenite through pseudorutile to leucoxene. \u003Ci>Ore Geology Reviews\u003C\u002Fi>,  6 (1). 25-44 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002F0169-1368(91)90030-b'>doi:10.1016\u002F0169-1368(91)90030-b\u003C\u002Fa>","10.1016\u002F0169-1368(91)90030-b",{"id":130,"year":131,"html":132,"doi":133},2083,1994,"Grey, Ian E., Watts, John A., Bayliss, Peter (1994) Mineralogical nomenclature: pseudorutile revalidated and neotype given. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  58 (393) 597-600 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1994.058.393.07'>doi:10.1180\u002Fminmag.1994.058.393.07\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_58\u002F58-393-597.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1994.058.393.07",{"id":135,"year":136,"html":137,"doi":11},16119383,1995,"American Mineralogist (1995): 80: 1077.",{"id":139,"year":140,"html":141,"doi":142},243442,2003,"Tetsopgang, S., Koyanagi, J., Enami, M., Kihara, K. (2003) Hydroxylian pseudorutile in an adamellite from the Nkambe area, Cameroon. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  67 (3) 509-516 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002F0026461036730113'>doi:10.1180\u002F0026461036730113\u003C\u002Fa>","10.1180\u002F0026461036730113",{"id":144,"year":140,"html":145,"doi":146},243460,"Grey, I. E., Li, C. (2003) Hydroxylian pseudorutile derived from picroilmenite in the Murray Basin, southeastern Australia. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  67 (4) 733-747 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002F0026461036740130'>doi:10.1180\u002F0026461036740130\u003C\u002Fa>","10.1180\u002F0026461036740130",{"id":148,"year":149,"html":150,"doi":11},16966843,2005,"(2005) Pseudorutile. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fpseudorutile.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":152,"year":153,"html":154,"doi":155},396369,2010,"Grey, I. E., Bordet, P., Wilson, N. C., Townend, R., Bastow, T. J., Brunelli, M. (2010) A new Al-rich hydroxylian pseudorutile from Kalimantan, Indonesia. \u003Ci>American Mineralogist\u003C\u002Fi>,  95 (1) 161-170 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2010.3330'>doi:10.2138\u002Fam.2010.3330\u003C\u002Fa>","10.2138\u002Fam.2010.3330",{"id":157,"year":158,"html":159,"doi":160},65043,2012,"Medaris, L. G., Fournelle, J. H. (2012) Pseudorutile in the Baraboo Range, Wisconsin: first recognition as a metamorphic mineral. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  50 (5) 1165-1172 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3749\u002Fcanmin.50.5.1165'>doi:10.3749\u002Fcanmin.50.5.1165\u003C\u002Fa>","10.3749\u002Fcanmin.50.5.1165",{"id":162,"year":163,"html":164,"doi":11},16120763,2015,"Schulz, B., Haser, S. (2015) The ilmenite-pseudorutile-leucoxene alteration sequence in placer sediments in the view of automated SEM mineral liberation analysis. GeoBerlin: 2015: 336.",{"id":166,"year":167,"html":168,"doi":169},15360214,2022,"Imperial, Alexis, Pe-Piper, Georgia, Piper, David J. W., Grey, Ian E. (2022) Identifying Pseudorutile and Kleberite Using Raman Spectroscopy. \u003Ci>Minerals\u003C\u002Fi>, 12 (10) 1210 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3390\u002Fmin12101210'>doi:10.3390\u002Fmin12101210\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fwww.mdpi.com\u002F2075-163X\u002F12\u002F10\u002F1210\u002Fpdf?version=1664106565' class='refpdflink'>\u003C\u002Fa>","10.3390\u002Fmin12101210",[171],{"id":172,"source_url":173,"license_code":174,"credit_html":175,"title":176,"description":177,"author":178,"original_width":179,"original_height":180},20126,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=143580345","CC BY 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=143580345\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Pseudorutile.jpg","Outstanding orange brown crystals of the rare mineral pseudorutile, a mineral much rarer than rutile from Slovaquia (Revúca, Revúca County, Banská Bystrica Region, Slovakia). Ex Vandenbroucke Museum collection from Waregem, Belgium.","David Hospital",631,568,[182],{"id":183,"url":184,"label":185,"formula":186,"spacegroup":187,"year":113},11550,"\u002Fcif\u002F11550.cif","Grey 1975","Fe4.728 Mn.272 Ti9.67 O27","P 63 2 2",[189],"Pseudorutiel",[191,195,199,203],{"lang":192,"names":193},"ca",[194],"pseudorútil",{"lang":196,"names":197},"de",[198],"Pseudorutil",{"lang":200,"names":201},"eu",[202],"Pseudorutilo",{"lang":204,"names":205},"it",[7,202],"Q1616757",{"history":11,"applications":11}]