[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:4029":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":19,"key_elements":11,"impurities":11,"cim":11,"ima_status":20,"ima_notes":11,"ima_history":11,"approval_year":11,"publication_year":11,"discovery_year":23,"strunz10ed1":24,"strunz10ed2":25,"strunz10ed3":25,"strunz10ed4":26,"dana8ed1":24,"dana8ed2":27,"dana8ed3":28,"dana8ed4":29,"csystem":30,"cclass":31,"spacegroup":32,"spacegroupset":33,"a":34,"b":35,"c":36,"alpha":35,"beta":35,"gamma":35,"aerror":11,"berror":11,"cerror":11,"alphaerror":11,"betaerror":11,"gammaerror":11,"va3":37,"z":38,"csmetamict":14,"commentcrystal":11,"twinning":11,"tranglide":11,"parting":11,"epitaxidescription":11,"morphology":39,"tlform":11,"hmin":40,"hmax":41,"hardtype":11,"vhnmin":42,"vhnmax":35,"vhnerror":11,"vhng":11,"vhns":11,"commenthard":11,"dmeas":43,"dmeas2":44,"dcalc":45,"dmeaserror":11,"dcalcerror":11,"commentdense":11,"lustre":11,"lustretype":46,"commentluster":11,"diapheny":47,"streak":48,"colour":49,"commentcolor":50,"colors":51,"streak_colors":55,"luminescence":11,"uv":11,"cleavage":11,"cleavagetype":57,"fracturetype":58,"tenacity":59,"commentbreak":11,"opticaltype":11,"opticalsign":11,"opticalalpha":35,"opticalalpha2":35,"opticalalphaerror":11,"opticalbeta":35,"opticalbeta2":35,"opticalbetaerror":11,"opticalgamma":35,"opticalgamma2":35,"opticalgammaerror":11,"opticalomega":35,"opticalomega2":35,"opticalomegaerror":11,"opticalepsilon":35,"opticalepsilon2":35,"opticalepsilonerror":11,"opticaln":35,"opticaln2":35,"opticalnerror":11,"optical2vcalc":35,"optical2vcalc2":35,"optical2vcalcerror":11,"optical2vmeasured":35,"optical2vmeasured2":35,"optical2vmeasurederror":11,"rimin":11,"rimax":11,"opticaldispersion":11,"opticalpleochroism":11,"opticalpleochorismdesc":11,"opticalbirefringence":11,"opticalcomments":11,"opticalcolour":11,"opticalinternal":11,"opticaltropic":60,"opticalanisotropism":61,"opticalbireflectance":11,"opticalextinction":11,"opticalr":11,"specdispm":11,"ir":11,"electrical":11,"magnetism":11,"thermalbehaviour":11,"other":11,"industrial":11,"occurrence":62,"otheroccurrence":63,"type_specimen_store":11,"description_short":64,"aboutname":65,"rock_parent":11,"rock_parent2":11,"rock_root":9,"rock_bgs_code":11,"meteoritical_code":11,"updttime":66,"reviewed_at":11,"variety_of":11,"varieties":67,"group_members":68,"associates":87,"confused_with":163,"type_localities":185,"occurrence_total":192,"citations":193,"images":278,"structures":309,"synonyms":326,"language_names":329,"wikidata_qid":408,"texts":409},4029,"1:1:4029:3","7bb28ee9-4abe-4b1d-8394-0612bbb450d4","Troilite","Tro",0,"mineral",null,39447,2052,false,"FeS",[17,18],"Fe","S",[17,18],[21,22],"APPROVED","GRANDFATHERED","1863","2","C","10","8","9","1","Hexagonal",20,126,"P63\u002Fmmc ","5.958","0","11.74",361.7,12,"massive, granular",3.5,4.5,"250","4.67","4.79","4.85","Metallic","Opaque","Brownish black","Gray brown, bronze brown (tarnished), yellow brown, light greyish brown, bronze","tarnishes rapidly on exposure",[52,53,54],"gray","brown","yellow",[53,56],"black","None Observed","Irregular\u002FUneven,Sub-Conchoidal","brittle","Anisotropic","strong","meteorite","Troilite occurs in serpentine, in layered ultramafic intrusives, and in meteorites. Known terrestial occurrences of troilite are not common. Found in a great number of meteorites (also Lunar and Martian) and in planetary nebulae. Found in slags and also in pulverized coal particles after combustion. Based on observations by the Voyager spacecraft in 1979 and Galileo in 1996, troilite seems to be an important phase in the mineral composition of the model rock of Jupiter's Galilean satellites Ganymede and Callisto. Based on the observations of Viking-1 and Viking-2-XRF-soil analyses and Phobos-2 orbital γ-ray data, troilite is likely to be a common mineral in the Martian surface rocks.","Pyrrhotite Group. Chemically the S-analogue of achávalite. Also chemically the Fe analogue of covellite, which has the same space group.\r\n\r\nTroilite, a native iron protosulphide, and related to the species pyrrhotite (monoclinic or hexagonal Fe1-xS; x ...","Named after Domenico Troili (11 April 1722, Macerata, Marche, Italy – 14 February 1793, Macerata, Marche, Italy) who first noted the mineral in a meteorite that fell in 1766 at Albareto, Modena (Italy).\r\n\r\nTroilite is the only Italian mineral whose type locality is actually a meteorite impact site. The Abbé Domenico Troili, a Jesuit, is widely credited by those who study meteorites as having written the first description of the fall of a meteorite (“Ragionamento della caduta di un sasso”, published in Modena in 1766). Troili collected reports from many eyewitnesses, closely examined the stone and detected in it small grains of a brassy mineral he called “marchesita”, which was long assumed to be pyrite, FeS2. Only one century later, the mineral was recognized to be stoichiometric iron sulphide, FeS. In honour of Troili, Gustav Rose named it troilite in 1862.","2026-03-28 15:14:49",[],[69,79],{"id":70,"name":71,"entrytype":9,"csystem":72,"ima_formula":73,"mindat_formula":74,"hmin":40,"hmax":75,"dmeas":76,"dcalc":77,"primary_image_id":78},3328,"Pyrrhotite","Monoclinic","Fe\u003Csub>7\u003C\u002Fsub>S\u003Csub>8\u003C\u002Fsub>","Fe\u003Csub>1-x\u003C\u002Fsub>S",4,"4.58","4.69",30574,{"id":80,"name":81,"entrytype":9,"csystem":82,"ima_formula":83,"mindat_formula":84,"hmin":41,"hmax":41,"dmeas":85,"dcalc":85,"primary_image_id":86},3691,"Smythite","Trigonal","(Fe,Ni)\u003Csub>3+x\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub> (x ≈ 0-0.3)","(Fe,Ni)\u003Csub>3+x\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub> (x=0-0.3)","4.32",22516,[88,95,102,111,118,124,132,139,145,154],{"id":89,"name":90,"entrytype":9,"csystem":82,"ima_formula":91,"mindat_formula":91,"hmin":92,"hmax":92,"dmeas":35,"dcalc":93,"primary_image_id":94},918,"Caswellsilverite","NaCrS\u003Csub>2\u003C\u002Fsub>",2,"3.23",4841,{"id":96,"name":97,"entrytype":9,"csystem":98,"ima_formula":99,"mindat_formula":99,"hmin":75,"hmax":41,"dmeas":35,"dcalc":100,"primary_image_id":101},1097,"Cobaltpentlandite","Isometric","Co\u003Csub>9\u003C\u002Fsub>S\u003Csub>8\u003C\u002Fsub>","5.22",6016,{"id":103,"name":104,"entrytype":9,"csystem":98,"ima_formula":105,"mindat_formula":106,"hmin":41,"hmax":107,"dmeas":108,"dcalc":109,"primary_image_id":110},1230,"Daubréelite","FeCr\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","Fe\u003Csup>2+\u003C\u002Fsup>Cr\u003Csup>3+\u003C\u002Fsup>\u003Csub>2\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>",5,"3.81","3.842",6869,{"id":112,"name":113,"entrytype":9,"csystem":30,"ima_formula":25,"mindat_formula":25,"hmin":114,"hmax":92,"dmeas":115,"dcalc":116,"primary_image_id":117},1740,"Graphite",1,"2.09","2.26",29804,{"id":119,"name":120,"entrytype":9,"csystem":121,"ima_formula":122,"mindat_formula":122,"hmin":41,"hmax":41,"dmeas":35,"dcalc":123,"primary_image_id":11},1837,"Haycockite","Orthorhombic","Cu\u003Csub>4\u003C\u002Fsub>Fe\u003Csub>5\u003C\u002Fsub>S\u003Csub>8\u003C\u002Fsub>","4.33",{"id":125,"name":126,"entrytype":9,"csystem":121,"ima_formula":127,"mindat_formula":127,"hmin":128,"hmax":128,"dmeas":129,"dcalc":130,"primary_image_id":131},2217,"Kirschsteinite","CaFe\u003Csup>2+\u003C\u002Fsup>(SiO\u003Csub>4\u003C\u002Fsub>)",5.5,"3.434","3.596",13376,{"id":133,"name":134,"entrytype":9,"csystem":135,"ima_formula":136,"mindat_formula":136,"hmin":75,"hmax":75,"dmeas":137,"dcalc":138,"primary_image_id":11},2772,"Mooihoekite","Tetragonal","Cu\u003Csub>9\u003C\u002Fsub>Fe\u003Csub>9\u003C\u002Fsub>S\u003Csub>16\u003C\u002Fsub>","4.36","4.37",{"id":140,"name":141,"entrytype":9,"csystem":98,"ima_formula":17,"mindat_formula":17,"hmin":41,"hmax":41,"dmeas":142,"dcalc":143,"primary_image_id":144},2047,"Native Iron","7.3","7.874",17186,{"id":146,"name":147,"entrytype":9,"csystem":135,"ima_formula":148,"mindat_formula":148,"hmin":149,"hmax":150,"dmeas":151,"dcalc":152,"primary_image_id":153},3582,"Schreibersite","(Fe,Ni)\u003Csub>3\u003C\u002Fsub>P",6.5,7,"7.0","7.28",21826,{"id":155,"name":156,"entrytype":9,"csystem":82,"ima_formula":157,"mindat_formula":158,"hmin":114,"hmax":159,"dmeas":160,"dcalc":161,"primary_image_id":162},4136,"Valleriite","2[(Fe,Cu)S] · 1.53[(Mg,Al)(OH)\u003Csub>2\u003C\u002Fsub>]","(Fe\u003Csup>2+\u003C\u002Fsup>,Cu)\u003Csub>4\u003C\u002Fsub>(Mg,Al)\u003Csub>3\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>(OH,O)\u003Csub>6\u003C\u002Fsub>",1.5,"3.14","3.21",27216,[164,169,174,180],{"id":165,"name":166,"entrytype":9,"csystem":30,"ima_formula":167,"mindat_formula":167,"hmin":11,"hmax":11,"dmeas":11,"dcalc":168,"primary_image_id":11},42371,"Buseckite","(Fe,Zn,Mn)S","3.697",{"id":170,"name":171,"entrytype":9,"csystem":98,"ima_formula":15,"mindat_formula":172,"hmin":11,"hmax":11,"dmeas":35,"dcalc":173,"primary_image_id":11},27196,"Keilite","(Fe\u003Csup>2+\u003C\u002Fsup>,Mg)S","3.958",{"id":175,"name":176,"entrytype":9,"csystem":135,"ima_formula":15,"mindat_formula":15,"hmin":177,"hmax":177,"dmeas":35,"dcalc":178,"primary_image_id":179},2512,"Mackinawite",2.5,"4.17",14947,{"id":181,"name":182,"entrytype":9,"csystem":98,"ima_formula":183,"mindat_formula":183,"hmin":11,"hmax":11,"dmeas":35,"dcalc":184,"primary_image_id":11},27575,"Rudashevskyite","(Fe,Zn)S","3.79",[186],{"id":187,"txt":188,"latitude":189,"longitude":190,"country":191},16076,"Albareto meteorite, Albareto, Modena, Modena Province, Emilia-Romagna, Italy",44.6833333,10.95,"Italy",1114,[194,197,201,205,209,213,217,221,226,230,234,238,243,247,251,255,259,264,268,273],{"id":195,"year":11,"html":196,"doi":11},18641252,"Kiskyras, D. A. (1943): Magnetic properties of the minerals of the system FeS-FeS2. Beiträge zur Angewandten Geophysik 10, 308-311.",{"id":198,"year":199,"html":200,"doi":11},16126331,1863,"Haidinger, W. (1863): Meteorit von Albareto im k. k. Hof-Mineralienkabinet vom Jahre 1766, un der troilit: K. Academie der Willenschaften, Vienna (Wien), Mathematisch-naturwissenschaftiche Klasse, Sitzumsberichte, 47, 283-298.",{"id":202,"year":203,"html":204,"doi":11},16126330,1868,"Öfvers. KVA handl. (1868), 25, 197-201.",{"id":206,"year":207,"html":208,"doi":11},16126332,1933,"Hägg, G. & Sucksdorff, I. (1933): Die Kristallstruktur von Troilit und Magnetkies. Zeitschrift für Physikalische Chemie, B22, 444-452.",{"id":210,"year":211,"html":212,"doi":11},521693,1947,"Buerger, M. J. (1947) The cell and symmetry of pyrrhotite. \u003Ci>American Mineralogist\u003C\u002Fi>,  32 (7-8) 411-414 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM32\u002FAM32_411.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":214,"year":215,"html":216,"doi":11},524135,1964,"Carpenter, Robert Heron, Desborough, George A. (1964) Range in solid solution and structure of naturally occurring troilite and pyrrhotite. \u003Ci>American Mineralogist\u003C\u002Fi>,  49 (9-10) 1350-1365 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM49\u002FAM49_1350.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":218,"year":219,"html":220,"doi":11},526062,1973,"Carpenter, Robert H., Bailey, and Arthur C. (1973) Application of Ro and At measurements to the study of pyrrhotite and troilite. \u003Ci>American Mineralogist\u003C\u002Fi>,  58 (5-6) 440-443 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM58\u002FAM58_440.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":222,"year":223,"html":224,"doi":225},198128,1982,"King, H. E., Prewitt, C. T. (1982) High-pressure and high-temperature polymorphism of iron sulfide (FeS) \u003Ci>Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry\u003C\u002Fi>,  38 (7) 1877-1887 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1107\u002Fs0567740882007523'>doi:10.1107\u002Fs0567740882007523\u003C\u002Fa>","10.1107\u002Fs0567740882007523",{"id":227,"year":223,"html":228,"doi":229},151267,"Töpel-Schadt, Jutta, Müller, Wolfgang Friedrich (1982) Transmission electron microscopy on meteoritic troilite. \u003Ci>Physics and Chemistry of Minerals\u003C\u002Fi>,  8 (4). 175-179 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1007\u002Fbf00308240'>doi:10.1007\u002Fbf00308240\u003C\u002Fa>","10.1007\u002Fbf00308240",{"id":231,"year":232,"html":233,"doi":11},16126336,1986,"Zapiski Vserossiyskogo Mineralogicheskogo Obshchestva (1986): 115: 173-177.",{"id":235,"year":236,"html":237,"doi":11},16126339,1999,"Scott, E.R.D. and Pinault, L.J. (1999) Partial Melting and Incipient Segregation of Troilite and Metal in Winonaites, Acapulcoites, IAB and IIE Irons, and Fine-Grained H6 Chondrites. XXX Lunar and Planetary Science Conference, Houston, abstract 1507.",{"id":239,"year":240,"html":241,"doi":242},331924,2002,"Marvin, Ursula B., Cosmo, Mario L. (2002) Domenico Troili (1766): “The true cause of the fall of a stone in Albereto is a subterranean explosion that hurled the stone skyward”. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  37 (12) 1857-1864 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fj.1945-5100.2002.tb01169.x'>doi:10.1111\u002Fj.1945-5100.2002.tb01169.x\u003C\u002Fa>","10.1111\u002Fj.1945-5100.2002.tb01169.x",{"id":244,"year":245,"html":246,"doi":11},16121143,2003,"Selivanov, E.N., Vershinin, A.D., Gulyaeva, R.I. (2003) Thermal expansion of troilite and pyrrhotine [sic] in helium and air. Inorganic Materials: 39: 1097-1102.",{"id":248,"year":245,"html":249,"doi":250},349084,"Thomas, Joan E, Skinner, William M, Smart, Roger S.t.C (2003) A comparison of the dissolution behavior of troilite with other iron(II) sulfides; implications of structure. \u003Ci>Geochimica et Cosmochimica Acta\u003C\u002Fi>,  67 (5) 831-843 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fs0016-7037(02)01146-8'>doi:10.1016\u002Fs0016-7037(02)01146-8\u003C\u002Fa>","10.1016\u002Fs0016-7037(02)01146-8",{"id":252,"year":253,"html":254,"doi":11},16967802,2005,"(2005) Troilite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Ftroilite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":256,"year":253,"html":257,"doi":258},243608,"Tenailleau, C.; Etschmann, B.; Wang, H.; Pring, A.; Grguric, B. A.; Studer, A. (2005) Thermal expansion of troilite and pyrrhotite determined by \u003Ci>in situ\u003C\u002Fi> cooling (873 to 373 K) neutron powder diffraction measurements. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  69 (2). 205-216 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002F0026461056920247'>doi:10.1180\u002F0026461056920247\u003C\u002Fa>","10.1180\u002F0026461056920247",{"id":260,"year":261,"html":262,"doi":263},395539,2006,"Skala, R. (2006) Inversion twinning in troilite. \u003Ci>American Mineralogist\u003C\u002Fi>,  91 (5) 917-921 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2006.1999'>doi:10.2138\u002Fam.2006.1999\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol91\u002FAM91_917.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2006.1999",{"id":265,"year":261,"html":266,"doi":267},395452,"Ono, S., Kikegawa, T. (2006) High-pressure study of FeS, between 20 and 120 GPa, using synchrotron X-ray powder diffraction. \u003Ci>American Mineralogist\u003C\u002Fi>,  91 (11) 1941-1944 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2006.2347'>doi:10.2138\u002Fam.2006.2347\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol91\u002FAM91_1941.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2006.2347",{"id":269,"year":270,"html":271,"doi":272},17382563,2007,"Tan, Zheng, Su, Xuping, Li, Zhi, Liu, Ya, Wang, Jianhua (2007) Phase equilibria in the Zn–Fe–S system at 450°C. \u003Ci>International Journal of Materials Research\u003C\u002Fi>,  98 (1) 16-20 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.3139\u002F146.101435'>doi:10.3139\u002F146.101435\u003C\u002Fa>","10.3139\u002F146.101435",{"id":274,"year":275,"html":276,"doi":277},333954,2013,"Avril, Caroline, Malavergne, Valérie, Caracas, Razvan, Zanda, Brigitte, Reynard, Bruno, Charon, Emeline, Bobocioiu, Ema, Brunet, Fabrice, Borensztajn, Stephan, Pont, Sylvain, et al. (2013) Raman spectroscopic properties and Raman identification of CaS‐MgS‐MnS‐FeS‐Cr\u003Csub>2\u003C\u002Fsub>FeS\u003Csub>4\u003C\u002Fsub> sulfides in meteorites and reduced sulfur‐rich systems. \u003Ci>Meteoritics & Planetary Science\u003C\u002Fi>,  48 (8). 1415-1426 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1111\u002Fmaps.12145'>doi:10.1111\u002Fmaps.12145\u003C\u002Fa>","10.1111\u002Fmaps.12145",[279,289,299],{"id":280,"source_url":281,"license_code":282,"credit_html":283,"title":284,"description":285,"author":286,"original_width":287,"original_height":288},24586,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7803661","CC BY-SA 3.0","André Knöfel, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7803661\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Sikhote alin.jpg","Meteorit \u003Ca href=\"https:\u002F\u002Fde.wikipedia.org\u002Fwiki\u002FSikhote-Alin_(Meteorit)\" class=\"extiw\" title=\"de:Sikhote-Alin (Meteorit)\">Sikhote Alin\u003C\u002Fa>. Scheibe mit \u003Ca href=\"https:\u002F\u002Fde.wikipedia.org\u002Fwiki\u002FTroilit\" class=\"extiw\" title=\"de:Troilit\">Troilit\u003C\u002Fa>-Einschlüssen, einem rekristallisiertem Rand durch hohe Temperaturen beim Flug durch die Atmosphäre und Neumann-Linien","André Knöfel",1321,1096,{"id":290,"source_url":291,"license_code":292,"credit_html":293,"title":294,"description":295,"author":296,"original_width":297,"original_height":298},21827,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=15757428","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=15757428\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Cape York meteorite, pattern.jpg","Octahedrite - a cut, polished, and nitric acid-etched surface of the Cape York Meteorite from Greenland.  The large, black, irregularly rounded structures are masses of troilite - iron monosulfide (FeS).  Each troilite nodule is surrounded by a silvery rim of schreibersite - iron nickel cobalt phosphide ((Fe,Ni,Co)3P).  The criss-crossing blades of metal (Widmanstätten structure) are mostly kamacite, with some taenite.  Collected 1982.  Odessa Meteor Crater Museum public display (Odessa, Texas, USA).","James St. John",810,624,{"id":300,"source_url":301,"license_code":302,"credit_html":303,"title":304,"description":305,"author":306,"original_width":307,"original_height":308},15909,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=182936184","CC BY-SA 4.0","Meteoriten-Deutschlands, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=182936184\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Meteorite Renchen, Sample R3A, Merrillite-Apatite Aggregate and Troilite.jpg","Meteorite Renchen, detailed view of fragment R3A showing a millimeter-sized merrillite–apatite aggregate and troilite.","Meteoriten-Deutschlands",10000,6666,[310,316,320],{"id":311,"url":312,"label":313,"formula":314,"spacegroup":315,"year":261},13874,"\u002Fcif\u002F13874.cif","Skala 2006","Fe S","P -6 2 c",{"id":317,"url":318,"label":319,"formula":314,"spacegroup":315,"year":223},13877,"\u002Fcif\u002F13877.cif","King 1982",{"id":321,"url":322,"label":323,"formula":314,"spacegroup":324,"year":325},13880,"\u002Fcif\u002F13880.cif","Alsen 1925","P 63\u002Fm m c",1925,[327,328],"Meteorkies","Pyrrhotite-2C",[330,334,338,342,346,349,353,358,362,365,369,373,377,382,385,388,391,394,398,401,405],{"lang":331,"names":332},"ar",[333],"ترويليت",{"lang":335,"names":336},"ca",[337],"troilita",{"lang":339,"names":340},"de",[341],"Troilit",{"lang":343,"names":344},"es",[345],"Troilita",{"lang":347,"names":348},"eu",[345],{"lang":350,"names":351},"fa",[352],"ترئولیت",{"lang":354,"names":355},"fr",[356,357],"1317-37-9","Troïlite",{"lang":359,"names":360},"he",[361],"טרויליט",{"lang":363,"names":364},"it",[7],{"lang":366,"names":367},"ja",[368],"トロイリ鉱",{"lang":370,"names":371},"mk",[372],"Троилит",{"lang":374,"names":375},"nb",[376],"troilitt",{"lang":378,"names":379},"nl",[380,381],"Troiliet","troilite",{"lang":383,"names":384},"nn",[376],{"lang":386,"names":387},"pl",[341],{"lang":389,"names":390},"pt",[345,381],{"lang":392,"names":393},"sl",[341],{"lang":395,"names":396},"uk",[397],"Троїліт",{"lang":399,"names":400},"uz",[341],{"lang":402,"names":403},"zh",[404],"隕硫鐵",{"lang":406,"names":407},"zh-hant",[404],"Q425316",{"history":11,"applications":11}]