[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:55445":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":22,"impurities":11,"cim":11,"ima_status":23,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":11,"strunz10ed1":25,"strunz10ed2":26,"strunz10ed3":27,"strunz10ed4":11,"dana8ed1":11,"dana8ed2":11,"dana8ed3":11,"dana8ed4":11,"csystem":28,"cclass":29,"spacegroup":30,"spacegroupset":31,"a":32,"b":11,"c":33,"alpha":11,"beta":11,"gamma":11,"aerror":34,"berror":11,"cerror":34,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":11,"z":35,"csmetamict":13,"commentcrystal":11,"twinning":36,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":11,"tlform":37,"hmin":38,"hmax":38,"hardtype":11,"vhnmin":39,"vhnmax":11,"vhnerror":29,"vhng":11,"vhns":11,"commenthard":40,"dmeas":11,"dmeas2":11,"dcalc":41,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":42,"commentluster":11,"diapheny":11,"streak":11,"colour":43,"commentcolor":11,"colors":44,"streak_colors":11,"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":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":46,"otheroccurrence":11,"type_specimen_store":47,"description_short":48,"aboutname":49,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":50,"reviewed_at":11,"variety_of":11,"varieties":51,"group_members":52,"associates":53,"confused_with":54,"type_localities":67,"occurrence_total":74,"citations":75,"images":98,"structures":99,"synonyms":100,"language_names":103,"wikidata_qid":113,"texts":114},55445,"1:1:55445:5","ebf3cde8-ef16-42d9-b1f4-39d15b7d022a","Wenjiite","Wnj",0,"mineral",null,8,false,"Ti\u003Csub>10\u003C\u002Fsub>Si\u003Csub>x\u003C\u002Fsub>P\u003Csub>y\u003C\u002Fsub>","x > y, 6 ≤ (x + y) ≤ 7","Ti\u003Csub>10\u003C\u002Fsub>Si\u003Csub>x\u003C\u002Fsub>P\u003Csub>y\u003C\u002Fsub>; x>y, 6&#8804;(x+y)&#8804;7",[18,19,20],"Si","Ti","P",[18,19,20],[19],[24],"APPROVED","1","B","0","Hexagonal",20,125,"P63\u002Fmcm ","7.30","5.09",10,1,"Not noted in type material, but it has been noted in synthetic material.","With kangjinlaite in a spheroid 20 μm across enclosed in corundum; as an overgrowth up to 20 μm thick around a jingsuiite grain; a platelet in a lamellar intergrowth with jingsuiite, khamrabaevite-osbornite and deltalumite; and as two grains up to 20 μm in the longest dimension with other minerals.",6.5,"970","Hardness data for synthetic material","4.762","Metallic","Silver gray (synthetic)",[45],"gray","In corundum from a podiform chromitite.","Mineralogical collections of the Geological Museum of China, No. 16 Yangrou Hutong, Xisi, Beijing 100031, People’s Republic of China, catalogue number M16104.","The Ti(P)-analogue of mavlyanovite and xifengite. Chemically similar, to some extent, to zhiqinite and, kangjinlaite, zangboite, UM1989-10-E:FeSiTi, and 'Unnamed (Fe-Si-Ti Alloy)'.\r\n\r\nPhysical properties were determined on synthetic materials.","Named for Bai Wenji (15 October 1935, Jilian China - 11 January 2019), Research Professor of Institute of Geology, Chinese Academy of Geological Sciences. He was the first person to find diamonds, native Fe and other special minerals in chromitite in the Luobusa ophiolite. He discovered and named 7 new mineral species including luobusaite, linzhiite, naquite, zangboite, yarlongite, qusongite, and native titanium.","2025-08-11 12:15:23",[],[],[],[55,61],{"id":56,"name":57,"entrytype":9,"csystem":28,"ima_formula":58,"mindat_formula":58,"hmin":59,"hmax":59,"dmeas":11,"dcalc":60,"primary_image_id":11},38826,"Mavlyanovite","Mn\u003Csub>5\u003C\u002Fsub>Si\u003Csub>3\u003C\u002Fsub>",7,"6.06",{"id":62,"name":63,"entrytype":9,"csystem":28,"ima_formula":64,"mindat_formula":64,"hmin":65,"hmax":65,"dmeas":27,"dcalc":66,"primary_image_id":11},4335,"Xifengite","Fe\u003Csub>5\u003C\u002Fsub>Si\u003Csub>3\u003C\u002Fsub>",5,"6.45",[68],{"id":69,"txt":70,"latitude":71,"longitude":72,"country":73},305074,"Orebody CR-11, Kangjinla Cr deposit, Luobusha ophiolite (\"Luobusa ophiolite\"), Qusum Co. (Qusong Co.), Shannan Prefecture (Lhokha Prefecture; Lhoka Prefecture), Tibet, China",29.1833333,92.3,"China",3,[76,80,84,89,93],{"id":77,"year":78,"html":79,"doi":11},16143414,1955,"Krikorian, O.H. (1955) High temperature studies: I. Reactions of the Refractory Silicides with Carbon and with Nitrogen. II. Thermodynamic Properties of the Carbides. III. Heat of Formation of the 3πu State of C2 from Graphite. Lawrence Berkeley National Radiation Laboratory. Ph.D. Thesis.",{"id":81,"year":82,"html":83,"doi":11},16143415,2004,"Frommeyer, G., Rosenkranz, R. (2004) Structures and properties of the refractory silicides Ti5Si3 and TiSi2 and Ti-Si-(Al) eutectic alloys. In: Senkov, O.N.; Miracle, D.B.; Firstov, S.A. Metallic Materials with High Structural Efficiency, NATO Science Series, Series II: Mathematics, Physics and Chemistry, 146, 287-308.",{"id":85,"year":86,"html":87,"doi":88},16139477,2021,"Miyawaki, Ritsuro, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2021) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) – Newsletter 61. \u003Ci>European Journal of Mineralogy\u003C\u002Fi>,  33 (3) 299-304 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.5194\u002Fejm-33-299-2021'>doi:10.5194\u002Fejm-33-299-2021\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Fejm.copernicus.org\u002Farticles\u002F33\u002F299\u002F2021\u002Fejm-33-299-2021.pdf' class='refpdflink'>\u003C\u002Fa>","10.5194\u002Fejm-33-299-2021",{"id":90,"year":91,"html":92,"doi":11},16968095,2022,"(2022) Wenjiite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fhandbookofmineralogy.org\u002Fpdfs\u002FWenjiite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":94,"year":95,"html":96,"doi":97},15625340,2023,"Xiong, Fahui, Xu, Xiangzhen, Mugnaioli, Enrico, Gemmi, Mauro, Wirth, Richard, Yang, Jingsui, Grew, Edward S. (2023) Wenjiite, Ti\u003Csub>10\u003C\u002Fsub>(Si,P,☐)\u003Csub>7\u003C\u002Fsub>, and kangjinlaite, Ti\u003Csub>11\u003C\u002Fsub>(Si,P)\u003Csub>10\u003C\u002Fsub>, new minerals in the ternary Ti-P-Si system from the Luobusa ophiolite, Tibet, China. \u003Ci>American Mineralogist\u003C\u002Fi>,  108 (1) 197-210 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2022-8226'>doi:10.2138\u002Fam-2022-8226\u003C\u002Fa>","10.2138\u002Fam-2022-8226",[],[],[101,102],"IMA2019-107c","Wenjiiet",[104,108],{"lang":105,"names":106},"ca",[107],"wenjiïta",{"lang":109,"names":110},"de",[111,112],"IMA 2019-107c","Wenjiit","Q107297520",{"history":11,"applications":11}]