[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:30325":3},{"id":4,"longid":5,"guid":6,"name":7,"shortcode_ima":8,"entrytype":9,"entrytype_text":10,"varietyof":11,"synid":8,"polytypeof":8,"groupid":8,"weighting":12,"nolocadd":13,"blacklisted":13,"mindat_formula":14,"mindat_formula_note":8,"ima_formula":8,"elements":15,"sigelements":18,"key_elements":8,"impurities":8,"cim":8,"ima_status":8,"ima_notes":8,"ima_history":8,"approval_year":8,"publication_year":8,"discovery_year":8,"strunz10ed1":19,"strunz10ed2":19,"strunz10ed3":19,"strunz10ed4":8,"dana8ed1":19,"dana8ed2":19,"dana8ed3":19,"dana8ed4":19,"csystem":8,"cclass":8,"spacegroup":8,"spacegroupset":19,"a":8,"b":8,"c":8,"alpha":8,"beta":8,"gamma":8,"aerror":8,"berror":8,"cerror":8,"alphaerror":8,"betaerror":8,"gammaerror":8,"va3":8,"z":8,"csmetamict":13,"commentcrystal":8,"twinning":8,"tranglide":8,"parting":8,"epitaxidescription":8,"morphology":8,"tlform":8,"hmin":8,"hmax":8,"hardtype":8,"vhnmin":19,"vhnmax":19,"vhnerror":8,"vhng":8,"vhns":8,"commenthard":8,"dmeas":19,"dmeas2":19,"dcalc":19,"dmeaserror":8,"dcalcerror":8,"commentdense":8,"lustre":8,"lustretype":8,"commentluster":8,"diapheny":8,"streak":8,"colour":8,"commentcolor":8,"colors":8,"streak_colors":8,"luminescence":8,"uv":8,"cleavage":8,"cleavagetype":8,"fracturetype":8,"tenacity":8,"commentbreak":8,"opticaltype":8,"opticalsign":8,"opticalalpha":8,"opticalalpha2":8,"opticalalphaerror":8,"opticalbeta":8,"opticalbeta2":8,"opticalbetaerror":8,"opticalgamma":8,"opticalgamma2":8,"opticalgammaerror":8,"opticalomega":8,"opticalomega2":19,"opticalomegaerror":8,"opticalepsilon":8,"opticalepsilon2":19,"opticalepsilonerror":8,"opticaln":8,"opticaln2":8,"opticalnerror":8,"optical2vcalc":8,"optical2vcalc2":8,"optical2vcalcerror":8,"optical2vmeasured":8,"optical2vmeasured2":8,"optical2vmeasurederror":8,"rimin":8,"rimax":8,"opticaldispersion":8,"opticalpleochroism":8,"opticalpleochorismdesc":8,"opticalbirefringence":8,"opticalcomments":8,"opticalcolour":8,"opticalinternal":8,"opticaltropic":8,"opticalanisotropism":8,"opticalbireflectance":8,"opticalextinction":8,"opticalr":8,"specdispm":8,"ir":8,"electrical":8,"magnetism":8,"thermalbehaviour":8,"other":8,"industrial":8,"occurrence":8,"otheroccurrence":8,"type_specimen_store":8,"description_short":8,"aboutname":20,"rock_parent":8,"rock_parent2":8,"rock_root":21,"rock_bgs_code":8,"meteoritical_code":8,"updttime":22,"reviewed_at":8,"variety_of":23,"varieties":31,"group_members":32,"associates":33,"confused_with":34,"type_localities":35,"occurrence_total":36,"citations":37,"images":71,"structures":230,"synonyms":231,"language_names":234,"wikidata_qid":8,"texts":235},30325,"1:1:30325:9","30619abe-b3a0-482b-b046-ff625126200b","Stink-Fluss",null,2,"variety",1576,706,false,"CaF\u003Csub>2\u003C\u002Fsub>",[16,17],"Ca","F",[16,17],"0","From the German for \"stink\" and \"flow\" in allusion to the odor and the nature as fluorite (Flusspath).",0,"2025-08-11 12:14:55",{"id":11,"name":24,"entrytype":21,"csystem":25,"ima_formula":14,"mindat_formula":14,"hmin":26,"hmax":26,"dmeas":27,"dcalc":28,"strunz10ed1":29,"primary_image_id":30},"Fluorite","Isometric",4,"3.175","3.181","3",29727,[],[],[],[],[],19,[38,42,46,50,54,58,62,67],{"id":39,"year":40,"html":41,"doi":8},16135914,1847,"Hausmann (1847) 1441.",{"id":43,"year":44,"html":45,"doi":8},16135915,1920,"Henrich (1920) Zeitschrift für Angewandte Chemie 33.",{"id":47,"year":48,"html":49,"doi":8},16135916,1930,"Goebel, L. (1930) Radioaktive Zersetzungserscheinungen am Flußspat. Sitzungsberichte der Akademie der Wissenschaften in Wien, mathematisch-naturwissenschaftliche Klasse, Abteilung I, 139, 373-391. [https:\u002F\u002Fwww.zobodat.at\u002Fpdf\u002FSBAWW_139_0373-0391.pdf]",{"id":51,"year":52,"html":53,"doi":8},1118652,1951,"Palache, Charles; Berman, Harry; Frondel, Clifford (1951) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 2 - Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. John Wiley and Sons.",{"id":55,"year":56,"html":57,"doi":8},16135917,1961,"Strunz, H. (1961\u002F62): Die Uranfunde in Bayern von 1804 bis 1962 (einschließlich der radiometrischen Messungen). Acta Albertina Ratisbonensia 24, 5-92. (pp. 35-39)",{"id":59,"year":60,"html":61,"doi":8},16135918,2008,"Dill, H.G., Füssl, M. and Weber, B. (2008) Stinkspat: Ein Oberpfälzer Mineral in der Forschung. Oberpfälzer Heimat, 53, 213-225 (in German).",{"id":63,"year":64,"html":65,"doi":66},238700,2010,"Dill, H.G.; Weber, B. (2010) Accessory minerals of fluorite and their implication regarding the environment of formation (Nabburg–Wölsendorf fluorite district, SE Germany), with special reference to fetid fluorite (“Stinkspat”). \u003Ci>Ore Geology Reviews\u003C\u002Fi>,  37 (2). 65-86 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.oregeorev.2010.01.004'>doi:10.1016\u002Fj.oregeorev.2010.01.004\u003C\u002Fa>","10.1016\u002Fj.oregeorev.2010.01.004",{"id":68,"year":69,"html":70,"doi":8},16014163,2012,"Schmedt auf der Günne, J., Mangstl, M., and Kraus, F. (2012) Occurrence of Difluorine F2 in Nature — In Situ Proof and Quantification by NMR Spectroscopy. Angewandte Chemie, International Edition: 51: 1–4.",[72,82,92,102,110,120,128,136,144,151,158,165,172,179,185,192,199,206,213,220],{"id":73,"source_url":74,"license_code":75,"credit_html":76,"title":77,"description":78,"author":79,"original_width":80,"original_height":81},80957,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=3415513","CC BY-SA 2.5","Hannes Grobe, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=3415513\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Stinkspat hg.jpg","Fluorite (Antozonite). Wölsendorf, Oberpfalz, Southern Germany","Hannes Grobe",2304,1532,{"id":83,"source_url":84,"license_code":85,"credit_html":86,"title":87,"description":88,"author":89,"original_width":90,"original_height":91},80958,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7518218","CC BY-SA 4.0","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=7518218\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Antozonite.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFluorite\" class=\"extiw\" title=\"en:Fluorite\">Antozonite\u003C\u002Fa> (variety of fluorite, dark purple to black (mostly opaque), fluorine-containing gaseous state, by bombarding natural α rays in thorium-uranium deposits. The crushing of the material releases the gas with a smell of ozone) with calcite - Margnac Mine, Compreignac, Haute-Vienne, Limousin, France - (6x5.5cm)","Didier Descouens",3783,2535,{"id":93,"source_url":94,"license_code":95,"credit_html":96,"title":97,"description":98,"author":99,"original_width":100,"original_height":101},80959,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=32102416","CC BY-SA 3.0","Tatsubou, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=32102416\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Antozonite Wilberforce.jpg","Antozonite, from Wilberforce,Ont.Canada","Tatsubou",640,480,{"id":103,"source_url":104,"license_code":85,"credit_html":105,"title":106,"description":107,"author":79,"original_width":108,"original_height":109},80963,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=127141223","Hannes Grobe, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=127141223\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","34Stinkspat wölsendorf hg.jpg","Fluorite (Stinkspat) from Wölsendorf, Bayerischer Wald",5961,4882,{"id":111,"source_url":112,"license_code":113,"credit_html":114,"title":115,"description":116,"author":117,"original_width":118,"original_height":119},80966,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794416","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794416\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite-fluorapatite-amphibole rock (probably early Neoproterozoic, 929 Ma; Richardson-Fission Mine, just southeast of Radium Lake, Haliburton County, southeastern Ontario, Canada).jpg","Fluorite-calcite-fluorapatite-amphibole rock from the Precambrian of Ontario, Canada (8.2 centimeters across at its widest).\n\u003Cp>This attractive rock is from an igneous dike - a \"vein-dike\" or \"vein-dyke\" - that intrudes Precambrian gneisses and amphibolites at the Richardson-Fission Mine near Wilberforce, Ontario, Canada.  The purple mineral is fluorite.  The whitish-gray material is calcite.  The green crystals are fluorapatite.  The black mineral is amphibole.\n\u003C\u002Fp>\u003Cp>Purple fluorite stringers in rocks from this locality resemble gneissic foliation.  The mine targeted radium that had decayed from uranium.  Near uranium-bearing masses, the fluorite has a nearly black color.  When broken, such fluorite emits an unpleasant odor (\"fetid fluorite\", or \"antozonite\", or \"stinkspar\").  A similar phenomenon was noticed long ago in some German mines.  In the early 2010s, the scent was identified and verified as elemental fluorine gas (F2).  This was surprising, as elemental fluorine is highly reactive.\n\u003C\u002Fp>\u003Cp>The Richardson-Fission Mine \"vein-dyke\" has not been dated, but similar igneous bodies occur elsewhere in Ontario.  Radiometric dating from a calcite-bearing \"vein-dyke\" at Bear Lake Diggings revealed an early Neoproterozoic age of 929 Ma.  These Ontario calcitic dikes appear to be part of an alkaline intrusive event in the Grenville Province, possibly associated with some extensional tectonics at the end of Grenville Orogeny.\n\u003C\u002Fp>\nLocality: Richardson-Fission Mine (Richardson Mine; Fission Mine), just southeast of Radium Lake & west of Cope Lake & south of Cardiff Lake, ~3.5 to 4 air-kilometers northeast of the town of Wilberforce, ~25 km west of Bancroft, Cardiff Township, Haliburton County, southeastern Ontario, southeastern Canada","James St. John",3192,2026,{"id":121,"source_url":122,"license_code":113,"credit_html":123,"title":124,"description":125,"author":117,"original_width":126,"original_height":127},80967,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794417","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794417\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 1.jpg","Fluorite-calcite rock from the Precambrian of Ontario, Canada\n\u003Cp>This rock is from an igneous dike - a \"vein-dike\" or \"vein-dyke\" - that intrudes Precambrian basement rocks near Wilberforce, Ontario, Canada.  The purple mineral is fluorite.  The whitish-gray material is calcite.  The yellowish-brown crystals along the middle are fluorapatite.\n\u003C\u002Fp>\u003Cp>The sample probably comes from the Richardson-Fission Mine area near Radium Lake, Ontario.  Purple fluorite stringers in rocks from this locality resemble gneissic foliation.  The mine targeted radium that had decayed from uranium.  Near uranium-bearing masses, the fluorite has a nearly black color.  When broken, such fluorite emits an unpleasant odor (\"fetid fluorite\", or \"antozonite\", or \"stinkspar\").  A similar phenomenon was noticed long ago in some German mines.  In the early 2010s, the scent was identified and verified as elemental fluorine gas (F2).  This was surprising, as elemental fluorine is highly reactive.\n\u003C\u002Fp>\u003Cp>The Richardson-Fission Mine \"vein-dyke\" has not been dated, but similar igneous bodies occur elsewhere in Ontario.  Radiometric dating from a calcite-bearing \"vein-dyke\" at Bear Lake Diggings revealed an early Neoproterozoic age of 929 Ma.  These Ontario calcitic dikes appear to be part of an alkaline intrusive event in the Grenville Province, possibly associated with some extensional tectonics at the end of Grenville Orogeny.\n\u003C\u002Fp>\nLocality: unrecorded \u002F undisclosed locality near the town of Wilberforce, Ontario, Canada (but probably from the Richardson-Fission Mine area (Richardson Mine; Fission Mine), just southeast of Radium Lake & west of Cope Lake & south of Cardiff Lake, ~3.5 to 4 air-kilometers northeast of the town of Wilberforce, ~25 km west of Bancroft, Cardiff Township, Haliburton County, southeastern Ontario, southeastern Canada)",1460,1750,{"id":129,"source_url":130,"license_code":113,"credit_html":131,"title":132,"description":133,"author":117,"original_width":134,"original_height":135},80968,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794418","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794418\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; Richardson-Fission Mine, just southeast of Radium Lake, Haliburton County, southeastern Ontario, Canada).jpg","Fluorite-calcite rock from the Precambrian of Ontario, Canada (8.1 centimeters across at its widest).\n\u003Cp>This attractive rock is from an igneous dike - a \"vein-dike\" or \"vein-dyke\" - that intrudes Precambrian gneisses and amphibolites at the Richardson-Fission Mine near Wilberforce, Ontario, Canada.  The purple mineral is fluorite.  The whitish-gray material is calcite.\n\u003C\u002Fp>\u003Cp>Purple fluorite stringers in rocks from this locality resemble gneissic foliation.  The mine targeted radium that had decayed from uranium.  Near uranium minerals, the fluorite has a nearly black color.  When broken, such fluorite emits an unpleasant odor (\"fetid fluorite\", or \"antozonite\", or \"stinkspar\").  A similar phenomenon was noticed long ago in some German mines.  In the early 2010s, the scent was identified and verified as elemental fluorine gas (F2).  This was surprising, as elemental fluorine is highly reactive and was not expected to occur in nature.\n\u003C\u002Fp>\u003Cp>The Richardson-Fission Mine \"vein-dyke\" has not been dated, but similar igneous bodies occur elsewhere in Ontario.  Radiometric dating from a calcite-bearing \"vein-dyke\" at Bear Lake Diggings revealed an early Neoproterozoic age of 929 Ma.  These Ontario calcitic dikes appear to be part of an alkaline intrusive event in the Grenville Province, possibly associated with some extensional tectonics at the end of Grenville Orogeny.\n\u003C\u002Fp>\nLocality: Richardson-Fission Mine (Richardson Mine; Fission Mine), just southeast of Radium Lake & west of Cope Lake & south of Cardiff Lake, ~3.5 to 4 air-kilometers northeast of the town of Wilberforce, ~25 km west of Bancroft, Cardiff Township, Haliburton County, southeastern Ontario, southeastern Canada",3780,1774,{"id":137,"source_url":138,"license_code":113,"credit_html":139,"title":140,"description":141,"author":117,"original_width":142,"original_height":143},80969,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794419","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794419\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 2.jpg","Fluorite-calcite rock from the Precambrian of Ontario, Canada\n\u003Cp>This rock is from an igneous dike - a \"vein-dike\" or \"vein-dyke\" - that intrudes Precambrian basement rocks near Wilberforce, Ontario, Canada.  The purple mineral is fluorite.  The whitish-gray material is calcite.\n\u003C\u002Fp>\u003Cp>The sample probably comes from the Richardson-Fission Mine area near Radium Lake, Ontario.  Purple fluorite stringers in rocks from this locality resemble gneissic foliation.  The mine targeted radium that had decayed from uranium.  Near uranium-bearing masses, the fluorite has a nearly black color.  When broken, such fluorite emits an unpleasant odor (\"fetid fluorite\", or \"antozonite\", or \"stinkspar\").  A similar phenomenon was noticed long ago in some German mines.  In the early 2010s, the scent was identified and verified as elemental fluorine gas (F2).  This was surprising, as elemental fluorine is highly reactive.\n\u003C\u002Fp>\u003Cp>The Richardson-Fission Mine \"vein-dyke\" has not been dated, but similar igneous bodies occur elsewhere in Ontario.  Radiometric dating from a calcite-bearing \"vein-dyke\" at Bear Lake Diggings revealed an early Neoproterozoic age of 929 Ma.  These Ontario calcitic dikes appear to be part of an alkaline intrusive event in the Grenville Province, possibly associated with some extensional tectonics at the end of Grenville Orogeny.\n\u003C\u002Fp>\nLocality: unrecorded \u002F undisclosed locality near the town of Wilberforce, Ontario, Canada (but probably from the Richardson-Fission Mine area (Richardson Mine; Fission Mine), just southeast of Radium Lake & west of Cope Lake & south of Cardiff Lake, ~3.5 to 4 air-kilometers northeast of the town of Wilberforce, ~25 km west of Bancroft, Cardiff Township, Haliburton County, southeastern Ontario, southeastern Canada)",1361,1997,{"id":145,"source_url":146,"license_code":113,"credit_html":147,"title":148,"description":141,"author":117,"original_width":149,"original_height":150},80970,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794421","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794421\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 4.jpg",1855,1415,{"id":152,"source_url":153,"license_code":113,"credit_html":154,"title":155,"description":141,"author":117,"original_width":156,"original_height":157},80971,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794425","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794425\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 7.jpg",1676,1194,{"id":159,"source_url":160,"license_code":113,"credit_html":161,"title":162,"description":141,"author":117,"original_width":163,"original_height":164},80972,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794426","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794426\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 8.jpg",1183,1334,{"id":166,"source_url":167,"license_code":113,"credit_html":168,"title":169,"description":141,"author":117,"original_width":170,"original_height":171},80973,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794428","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794428\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 10.jpg",2016,1753,{"id":173,"source_url":174,"license_code":113,"credit_html":175,"title":176,"description":141,"author":117,"original_width":177,"original_height":178},80974,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794429","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794429\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 11.jpg",2217,1606,{"id":180,"source_url":181,"license_code":113,"credit_html":182,"title":183,"description":141,"author":117,"original_width":184,"original_height":164},80975,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794432","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794432\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 13.jpg",1438,{"id":186,"source_url":187,"license_code":113,"credit_html":188,"title":189,"description":141,"author":117,"original_width":190,"original_height":191},80976,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794435","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794435\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 14.jpg",2035,1635,{"id":193,"source_url":194,"license_code":113,"credit_html":195,"title":196,"description":141,"author":117,"original_width":197,"original_height":198},80977,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794436","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794436\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 15.jpg",1859,1267,{"id":200,"source_url":201,"license_code":113,"credit_html":202,"title":203,"description":141,"author":117,"original_width":204,"original_height":205},80978,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794440","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794440\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 18.jpg",1594,1447,{"id":207,"source_url":208,"license_code":113,"credit_html":209,"title":210,"description":141,"author":117,"original_width":211,"original_height":212},80979,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794441","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794441\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 17.jpg",1886,1239,{"id":214,"source_url":215,"license_code":113,"credit_html":216,"title":217,"description":141,"author":117,"original_width":218,"original_height":219},80980,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794443","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146794443\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite-calcite rock (probably early Neoproterozoic, 929 Ma; near Wilberforce, Ontario, Canada) 20.jpg",1394,2036,{"id":221,"source_url":222,"license_code":223,"credit_html":224,"title":225,"description":226,"author":227,"original_width":228,"original_height":229},80981,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=184859753","CC0 1.0","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=184859753\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fluorite antozonite, quartz.jpg","fluorite antozonite, quartz : Yaogangxian Mine, Yaogangxian W-Sn ore field, Yizhang Co., Chenzhou, Hunan Province, China","Géry PARENT",1987,1321,[],[232,233],"Antozonite","Stinkspat",[],{"history":8,"applications":8}]