[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"minerals:one:1617":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":22,"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":23,"strunz10ed2":8,"strunz10ed3":8,"strunz10ed4":8,"dana8ed1":23,"dana8ed2":23,"dana8ed3":23,"dana8ed4":23,"csystem":8,"cclass":8,"spacegroup":8,"spacegroupset":23,"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":23,"vhnmax":23,"vhnerror":8,"vhng":8,"vhns":8,"commenthard":8,"dmeas":23,"dmeas2":23,"dcalc":23,"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":23,"opticalalphaerror":8,"opticalbeta":8,"opticalbeta2":23,"opticalbetaerror":8,"opticalgamma":8,"opticalgamma2":23,"opticalgammaerror":8,"opticalomega":8,"opticalomega2":23,"opticalomegaerror":8,"opticalepsilon":8,"opticalepsilon2":23,"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":24,"rock_parent":8,"rock_parent2":8,"rock_root":25,"rock_bgs_code":8,"meteoritical_code":8,"updttime":26,"reviewed_at":8,"variety_of":27,"varieties":37,"group_members":42,"associates":43,"confused_with":44,"type_localities":45,"occurrence_total":46,"citations":47,"images":56,"structures":162,"synonyms":163,"language_names":177,"wikidata_qid":8,"texts":178},1617,"1:1:1617:5","b4947961-4326-4838-9405-33f932f77ef3","Fuchsite",null,2,"variety",2815,3286,false,"K(Al,Cr)\u003Csub>3\u003C\u002Fsub>Si\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>",[16,17,18,19,20,21],"Al","Cr","Si","O","K","H",[16,18,19,20,21],"0","Named in 1842 by Karl F. Emil von Schafhäutl in honour of Johann Nepomuk von Fuchs [May 15, 1774 Mattenzell, near Bremberg, Lower Bavaria, Germany - March 5, 1856 Munich, Germany] professor of chemistry and mineralogy at University of Landshut and curator of the mineral collection. ",0,"2025-08-11 12:14:20",{"id":11,"name":28,"entrytype":25,"csystem":29,"ima_formula":30,"mindat_formula":31,"hmin":32,"hmax":32,"dmeas":33,"dcalc":34,"strunz10ed1":35,"primary_image_id":36},"Muscovite","Monoclinic","KAl\u003Csub>2\u003C\u002Fsub>(Si\u003Csub>3\u003C\u002Fsub>Al)O\u003Csub>10\u003C\u002Fsub>(OH)\u003Csub>2\u003C\u002Fsub>","KAl\u003Csub>2\u003C\u002Fsub>(AlSi\u003Csub>3\u003C\u002Fsub>O\u003Csub>10\u003C\u002Fsub>)(OH)\u003Csub>2\u003C\u002Fsub>",2.5,"2.77","2.83","9",30243,[38],{"id":39,"name":40,"entrytype":9,"csystem":8,"ima_formula":8,"mindat_formula":31,"hmin":8,"hmax":8,"dmeas":23,"dcalc":23,"primary_image_id":41},5417,"Verdite",35550,[],[],[],[],487,[48,52],{"id":49,"year":50,"html":51,"doi":8},16109883,1946,"Whitmore, D.R.E., Berry, L.G., Hawley, J.E. (1946) Chrome micas. Am. Mineral. 31, 1–21.",{"id":53,"year":54,"html":55,"doi":8},16036929,1978,"T. C. Devaraju and K. S. Anantha Murthy (1978) Mineralogy of the fuchsites from Gattihosahalli, Karnataka State —Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences, 87, 255-261.",[57,64,74,83,93,102,110,119,128,136,144,154],{"id":58,"source_url":59,"license_code":60,"credit_html":61,"title":7,"description":8,"author":8,"original_width":62,"original_height":63},88279,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F172116","CC BY-SA 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F172116\" rel=\"noopener\">University of Tartu, Natural History Museum\u003C\u002Fa> via Europeana",1000,616,{"id":65,"source_url":66,"license_code":67,"credit_html":68,"title":69,"description":70,"author":71,"original_width":72,"original_height":73},55848,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1496435","CC BY 2.5","Ra'ike (see also: de:Benutzer:Ra'ike), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=1496435\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fuchsite.jpg","Fuchsite, Variety of Muscovite","Ra'ike (see also: de:Benutzer:Ra'ike)",1807,1410,{"id":75,"source_url":76,"license_code":60,"credit_html":77,"title":78,"description":79,"author":80,"original_width":81,"original_height":82},55849,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9446427","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=9446427\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fuchsite-Groix.jpg","Fuchsite (Var. of \u003Ca href=\"\u002F\u002Fcommons.wikimedia.org\u002Fwiki\u002FMuscovite\" class=\"mw-redirect\" title=\"Muscovite\">Muscovite\u003C\u002Fa>) and Glaucophane \n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality : Groix Island, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGroix\" class=\"extiw\" title=\"en:Groix\">Groix\u003C\u002Fa>, Morbihan, Brittany, France\u003C\u002Fdd>\n\u003Cdd>Size View 2.5cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Didier Descouens",4142,2850,{"id":84,"source_url":85,"license_code":86,"credit_html":87,"title":88,"description":89,"author":90,"original_width":91,"original_height":92},55855,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14867020","CC BY-SA 3.0","Leon Hupperichs, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=14867020\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muscovite-150242.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Muscovite\u003C\u002Fa> (Var.: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Fuchsite\u003C\u002Fa>)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Uspenskaya Mt, Berezovskoe Au Deposit (Berezovsk Mines), Berezovskii (Berezovskii Zavod), Ekaterinburg (Sverdlovsk), Ekaterinburgskaya (Sverdlovskaya) Oblast', Middle Urals, Urals Region, Russia\u003C\u002Fdd>\n\u003Cdd>Field of view 4x3 cm. Specimen and photo Leon Hupperichs.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Leon Hupperichs",841,631,{"id":94,"source_url":95,"license_code":96,"credit_html":97,"title":98,"description":7,"author":99,"original_width":100,"original_height":101},55867,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=90890629","Public domain","it:User:Angelorenzi, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=90890629\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fuchsite 2.jpg","it:User:Angelorenzi",570,519,{"id":103,"source_url":104,"license_code":60,"credit_html":105,"title":106,"description":107,"author":108,"original_width":91,"original_height":109},32422,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=98885440","Sarranpa, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=98885440\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fuchsita.jpg","Fuchsita, variedad de moscovita","Sarranpa",492,{"id":111,"source_url":112,"license_code":60,"credit_html":113,"title":114,"description":115,"author":116,"original_width":117,"original_height":118},55868,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=127740748","Osama Shukir Muhammed Amin FRCP(Glasg), via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=127740748\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Fuchsite from India. Erbil Stones and Gems Museum, Erbil Citadel, Hawler, Iraq.jpg","Fuchsite from India. Erbil Stones and Gems Museum, Erbil Citadel, Hawler, Iraq","Osama Shukir Muhammed Amin FRCP(Glasg)",3381,5240,{"id":120,"source_url":121,"license_code":86,"credit_html":122,"title":123,"description":124,"author":125,"original_width":126,"original_height":127},55850,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10136424","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10136424\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Corundum-Muscovite-63975.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCorundum\" class=\"extiw\" title=\"en:Corundum\">Corundum\u003C\u002Fa> (Var.: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FRuby\" class=\"extiw\" title=\"en:Ruby\">Ruby\u003C\u002Fa>), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Muscovite\u003C\u002Fa> (Var.: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Fuchsite\u003C\u002Fa>)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Eswatini (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-24757.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Lustrous, platy, green fuchsite liberally covers massive ruby matrix on this classic, old-time specimen from South Africa. Fuchsite is the chrome-rich variety of muscovite, which has bright red fluorescence. The piece comes with a Hugh Ford label, a prominent United States dealer from the 1920s to early 1950s. Ex Carl Davis Collection. 6.9 x 4.5 x 2.2 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",381,550,{"id":129,"source_url":130,"license_code":86,"credit_html":131,"title":132,"description":133,"author":125,"original_width":134,"original_height":135},55851,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10161866","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10161866\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muscovite-Quartz-217487.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Muscovite\u003C\u002Fa> (Var.: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Fuchsite\u003C\u002Fa>), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FQuartz\" class=\"extiw\" title=\"en:Quartz\">Quartz\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Chaprot valley, Chalt, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGilgit_District\" class=\"extiw\" title=\"en:Gilgit District\">Gilgit District\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGilgit-Baltistan\" class=\"extiw\" title=\"en:Gilgit-Baltistan\">Northern Areas\u003C\u002Fa>, Pakistan (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-122966.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 2.6 x 2.4 x 0.8 cm.\u003C\u002Fdd>\n\u003Cdd>Fuchsite is actually a rare bright to dark green variety of the common mineral muscovite. In these rare quartz crystals from Pakistan, it takes the form of bright, light green inclusions inside a tabular crystal of quartz. Unusual material from, so far as I know, a single pocket. Over the years I have seen perhaps less than 10 specimens from this pocket found in 1993, which produced strange quartzes of an unearthly green color. They initially were labeled everything from Chrysoprase crystals to Quartz included by dye. It turns out, so far as I know now, that the color is due to dispersed microscopic inclusions of fuchsite, a green mica species. This particular crystal is a superb thumbnail and a floater, complete all around.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",600,509,{"id":137,"source_url":138,"license_code":86,"credit_html":139,"title":140,"description":141,"author":125,"original_width":142,"original_height":143},55852,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10165892","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10165892\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Quartz-Muscovite-243369.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FQuartz\" class=\"extiw\" title=\"en:Quartz\">Quartz\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Muscovite\u003C\u002Fa> (Var.: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuscovite\" class=\"extiw\" title=\"en:Muscovite\">Fuchsite\u003C\u002Fa>)\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Mt.Masomeloka, Mananjary emerald District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FVatovavy-Fitovinany\" class=\"extiw\" title=\"en:Vatovavy-Fitovinany\">Vatovavy-Fitovinany Region\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FFianarantsoa_Province\" class=\"extiw\" title=\"en:Fianarantsoa Province\">Fianarantsoa Province\u003C\u002Fa>, Madagascar (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-133055.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 5.5 x 1.9 x 1.5 cm.\u003C\u002Fdd>\n\u003Cdd>A rare, fine quartz specimen from Madagascar. The water-clear quartz crystal encloses a small quartz crystal that is coated with blue-green fuchsite, making for a striking phantom. Fuchsite is the greenish variety of muscovite, high in chromium and is relatively rare worldwide. There is even fuchsite in the small quartz crystal.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",450,750,{"id":145,"source_url":146,"license_code":147,"credit_html":148,"title":149,"description":150,"author":151,"original_width":152,"original_height":153},55863,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84625730","CC BY 2.0","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84625730\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Auriferous banded quartz-fuchsite hydrothermal vein rock (Abitibi Greenstone Belt, Neoarchean; Placer Dome Mine (Dome Mine), Porcupine Mining District, east of Timmins, Ontario, Canada) 1 (15178961728).jpg","\u003Cp>Auriferous banded quartz-fuchsite hydrothermal vein rock (gold ore) from the Precambrian of Ontario, Canada. (6.3 centimeters across its widest)\n\u003C\u002Fp>\u003Cp>The bedrock in the Timmins, Ontario area is richly gold-mineralized.  Numerous mines exploit gold ores of various lithologies.  This is auriferous banded quartz-fuchsite hydrothermal vein rock - also referred to as strained ribbon quartz.  The \"ribbons\" are greenish-colored and principally composed of fuchsite and chlorite, plus native gold (Au).  Published research has shown that gold was emplaced during minor drops in pressure during many crack-and-seal events (incremental dilation) that formed the ribbon quartz vein.  Crack-and-seal events were initiated by hydraulic fracturing accompanying fluid discharge.\n\u003C\u002Fp>\u003Cp>Geologic context & age: quartz-fuchsite-chlorite-gold hydrothermal vein hosted in carbonatized komatiite, southern flanks of the Porcupine Syncline, Abitibi Greenstone Belt, Neoarchean; gold-quartz-fuchsite mineralization at 2633 to 2670 Ma\n\u003C\u002Fp>\u003Cp>Locality: Dome Mine (Placer Dome Mine), Porcupine Mining District, east of the city of Timmins, Ontario, southeastern Canada (48° 27’ 44.55” North, 81° 14’ 27.89” West)\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Most info. synthesized from:\n\u003C\u002Fp>\u003Cp>Fryer, B.J., R. Kerrich, R.W. Hutchinson, M.G. Peirce & D.S. Rogers.  1979.  Archean precious-metal hydrothermal systems, Dome Mine, Abitibi Greenstone Belt I, patterns of alteration and metal distribution.  Canadian Journal of Earth Sciences 16: 421-439.\n\u003C\u002Fp>\u003Cp>Moritz, R.P. & J.H. Crocket.  1990.  Mechanics of formation of the gold-bearing quartz-fuchsite vein at the Dome Mine, Timmins area, Ontario.  Canadian Journal of Earth Sciences 27: 1609-1620.\n\u003C\u002Fp>\nYork, D., P.W. Layer, N.D. McMaster, C.M. Hall & A. Masliwec.  1991.  The dating of Ontario's gold deposits.  Ontario Geological Survey Open File Report 5738.  161 pp.","James St. John",5834,3948,{"id":155,"source_url":156,"license_code":147,"credit_html":157,"title":158,"description":159,"author":151,"original_width":160,"original_height":161},55864,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84625733","James St. John, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=84625733\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Auriferous banded quartz-fuchsite hydrothermal vein rock (Abitibi Greenstone Belt, Neoarchean; Placer Dome Mine (Dome Mine), Porcupine Mining District, east of Timmins, Ontario, Canada) 2 (15365235032).jpg","\u003Cp>Auriferous banded quartz-fuchsite hydrothermal vein rock (gold ore) from the Precambrian of Ontario, Canada. (4.4 centimeters across at its widest)\n\u003C\u002Fp>\u003Cp>The bedrock in the Timmins, Ontario area is richly gold-mineralized.  Numerous mines exploit gold ores of various lithologies.  This is auriferous banded quartz-fuchsite hydrothermal vein rock - also referred to as strained ribbon quartz.  The \"ribbons\" are greenish-colored and principally composed of fuchsite and chlorite, plus native gold (Au) - this photo shows an irregular surface broken along the \"plane\" of a ribbon.\n\u003C\u002Fp>\u003Cp>Published research has shown that gold was emplaced during minor drops in pressure during many crack-and-seal events (incremental dilation) that formed the ribbon quartz vein.  Crack-and-seal events were initiated by hydraulic fracturing accompanying fluid discharge.\n\u003C\u002Fp>\u003Cp>Geologic context & age: quartz-fuchsite-chlorite-gold hydrothermal vein hosted in carbonatized komatiite, southern flanks of the Porcupine Syncline, Abitibi Greenstone Belt, Neoarchean; gold-quartz-fuchsite mineralization at 2633 to 2670 Ma\n\u003C\u002Fp>\u003Cp>Locality: Dome Mine (Placer Dome Mine), Porcupine Mining District, east of the city of Timmins, Ontario, southeastern Canada (48° 27’ 44.55” North, 81° 14’ 27.89” West)\n\u003C\u002Fp>\n\u003Chr>\n\u003Cp>Most info. synthesized from:\n\u003C\u002Fp>\u003Cp>Fryer, B.J., R. Kerrich, R.W. Hutchinson, M.G. Peirce & D.S. Rogers.  1979.  Archean precious-metal hydrothermal systems, Dome Mine, Abitibi Greenstone Belt I, patterns of alteration and metal distribution.  Canadian Journal of Earth Sciences 16: 421-439.\n\u003C\u002Fp>\u003Cp>Moritz, R.P. & J.H. Crocket.  1990.  Mechanics of formation of the gold-bearing quartz-fuchsite vein at the Dome Mine, Timmins area, Ontario.  Canadian Journal of Earth Sciences 27: 1609-1620.\n\u003C\u002Fp>\nYork, D., P.W. Layer, N.D. McMaster, C.M. Hall & A. Masliwec.  1991.  The dating of Ontario's gold deposits.  Ontario Geological Survey Open File Report 5738.  161 pp.",4203,2243,[],[164,165,166,167,168,169,170,171,172,173,174,175,176],"Chrom-Muskovit","Chrome-mica","Chromium-bearing Muscovite","Chrommuscovit","Chrommuscovite","Cr-muscovite","Crommuscovita","Fuchsit","Fuchsita","Fuxite","Gaebhardit","Gaebhardita","Gaebhardite",[],{"history":8,"applications":8}]