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","Pb\u003Csub>2\u003C\u002Fsub>(Sb,As)\u003Csub>2\u003C\u002Fsub>S\u003Csub>5\u003C\u002Fsub>",[19,20,21,22],"As","Pb","Sb","S",[19,20,21,22],[19,20,21],"5.6.20",[27],"APPROVED",1966,1967,"1966","2","H","C","05d","3","5","9","Monoclinic",4,9,"P21 ","8.429","26.069","8.962","0","117.447",2,5,1,"Data from Topa & Makovicky (2017). Orthorhombic pseudocell with a' = 0.5a = 4.22, b = 26.2, c = 7.90 Å. Space group of the pseudocell is P21cn or Pmcn. The X-ay powder pattern closely resembles that of dufrénoysite. ","Masses up  to 2 cm in diameter. Disseminated anhedral grains.",3.5,"156","172",50,"Metallic","Opaque","Black with weak brown tint","Steel-gray",[61,62,63,64,65],"gray","black","brown","white","pink",[62,63],"Conchoidal","Weak","White to pale pinkish gray","White","Anisotropic","Moderate","(40.2,43.8) 400,\r\n(39.9,43.4) 420,\r\n(39.6,43.0) 440,\r\n(39.2,42.8) 460,\r\n(38.8,42.6) 480,\r\n(38.4,42.3) 500,\r\n(37.9,42.0) 520,\r\n(37.4,41.7) 540,\r\n(37.0,41.4) 560,\r\n(36.5,40.8) 580,\r\n(36.1,40.3) 600,\r\n(35.7,39.8) 620,\r\n(35.3,39.1) 640,\r\n(34.7,38.4) 660,\r\n(34.0,37.6) 680,\r\n(33.3,36.8) 700","KOH (40%) tarnishes veenite iridescent and HNO3 tarnishes it black. KOH generally brings out the polysynthetic twinning also evident under partly crossed nicols.","Marbles produced from Precambrian metasedimentary rocks, formed at the margin of a plutonic intrusion.","Canadian Geological Survey, Ottawa, Canada, 12170.\r\nCanadian Museum of Nature, Ottawa, Canada.\r\nRoyal Ontario Museum, Toronto, Canada.","Dufrénoysite-Veenite Series.\r\n\r\nSartorite homologue, N = 4; the structure is based on zigzag walls of prismatic [3]Pb; these walls separate slabs comprising diagonally-oriented double layers containing Sb and As, and some Pb. Orientation of three-membe...","Named after Rudolf Willem van der Veen (27 January 1883, Buitenzorg (now Bogor), Dutch East Indies (now Indonesia) — 3 April 1925, Wassenaar (near The Hague), South Holland, The Netherlands), metallographer, mining engineer. After his studies in Delft he worked in mines in Argentina, Bolivia, India, Germany, and Spain. From 1916 to 1925 he was professor of economic geology at the Delft University of Technology (Netherlands). In 1925, he posthumously published one of the first books with pictures about ore microscopy.","2025-08-11 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Pb\u003Csub>0.8\u003C\u002Fsub>Tl\u003Csub>0.1\u003C\u002Fsub>Sb\u003Csub>1.3\u003C\u002Fsub>As\u003Csub>0.8\u003C\u002Fsub>S\u003Csub>4\u003C\u002Fsub>","5.323",[],[],[244],{"id":245,"txt":246,"latitude":247,"longitude":248,"country":249},550,"Taylor Pit, Madoc, Centre Hastings Municipality, Hastings County, Ontario, Canada",44.5022222,-77.4663889,"Canada",14,[252,255,258,262,266,270,274],{"id":253,"year":29,"html":254,"doi":11},16856039,"Jambor, John Leslie (1967) New lead sulfantimonides from Madoc, Ontario. Part 1. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  9 (1) 7-24 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM9_7.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":256,"year":29,"html":257,"doi":11},16856040,"Jambor, John Leslie (1967) New lead sulfantimonides from Madoc, Ontario. Part 2 - mineral descriptions. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  9 (2) 191-213 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM9_191.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":259,"year":260,"html":261,"doi":11},16856043,1968,"Jambor, John Leslie (1968) New lead sulfantimonides from Madoc, Ontario. Part 3--Syntheses, paragenesis, origin. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  9 (4). 505-521 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM9_505.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":263,"year":264,"html":265,"doi":11},16863126,1973,"Walia, D. S., Chang, L. L. Y. (1973) Investigations in the systems PbS-Sb2S3-As2S3 and PbS-Bi2S3-As2S3. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  12 (2) 113-119 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Frruff_1.0\u002Fuploads\u002FCM12_113.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":267,"year":268,"html":269,"doi":11},12907587,1982,"Jambor, John L.; Laflamme, J. H. G.; Walker, D. A. (1982) A Re-examination of the Madoc Sulfosalts, in \u003Ci>Ontario\u003C\u002Fi>. \u003Ci>The Mineralogical Record\u003C\u002Fi>,  13 (2). 93-100",{"id":271,"year":272,"html":273,"doi":11},16967965,2005,"(2005) Veenite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fveenite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":275,"year":276,"html":277,"doi":278},244885,2017,"Topa, Dan, Makovicky, Emil (2017) The crystal structure of veenite. \u003Ci>Mineralogical Magazine\u003C\u002Fi>,  81 (2) 355-368 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.2016.080.141'>doi:10.1180\u002Fminmag.2016.080.141\u003C\u002Fa>","10.1180\u002Fminmag.2016.080.141",[280],{"id":281,"source_url":282,"license_code":283,"credit_html":284,"title":285,"description":286,"author":287,"original_width":288,"original_height":289},27368,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=81711872","CC BY-SA 4.0","David Hospital, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=81711872\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Veenite.jpg","Black metallic crystal aggregates of the extremely rare sulphosalt mineral veenite from Mexico (Guitarra Mine, Temascaltepec).","David Hospital",972,667,[],[292,293,294,295,296],"IMA1966-016","Stibiodufrenoysit","Stibiodufrenoysita","Stibiodufrenoysite","Veeniet",[298,302,307,311],{"lang":299,"names":300},"ca",[301],"veenita",{"lang":303,"names":304},"de",[305,306],"IMA 1966-016","Veenit",{"lang":308,"names":309},"eu",[310],"Veenita",{"lang":312,"names":313},"it",[7],"Q2511740",{"history":11,"applications":11}]