{"id":2377,"date":"2025-10-02T23:41:21","date_gmt":"2025-10-02T23:41:21","guid":{"rendered":"https:\/\/dfoto.pl\/?page_id=2377"},"modified":"2025-10-02T23:41:59","modified_gmt":"2025-10-02T23:41:59","slug":"iv-j-arsenity-antymonity-bizmutyty-siarczyny-seleniny-i-telluryny","status":"publish","type":"page","link":"https:\/\/dfoto.pl\/index.php\/about\/mineraly\/iv-tlenki-i-wodorotlenki\/iv-j-arsenity-antymonity-bizmutyty-siarczyny-seleniny-i-telluryny\/","title":{"rendered":"IV\/J \u2013 Arsenity, antymonity, bizmutyty; siarczyny, seleniny i telluryny"},"content":{"rendered":"<p><strong>Grupa IV\/J Strunza (2025) \u2013 Arsenity, antymonity, bizmutyty; siarczyny, seleniny i telluryny<\/strong> obejmuje tlenkowe minera\u0142y, w kt\u00f3rych anionow\u0105 cz\u0119\u015b\u0107 struktury stanowi\u0105 odpowiednio grupy As(III), Sb(III), Bi(III) (arsenity\/antymonity\/bizmutyty) oraz aniony typu XO\u2083 z X = S(IV), Se(IV), Te(IV) (siarczyny\/seleniny\/telluryny). Dzia\u0142 ten porz\u0105dkuje te minera\u0142y wed\u0142ug obecno\u015bci dodatkowych anion\u00f3w (np. Cl\u207b, SO\u2084\u00b2\u207b) oraz wody krystalizacyjnej (H\u2082O). W wersji Strunz-Mindat (2025) IV\/J dzieli si\u0119 na poddzia\u0142y:<\/p>\n<ul>\n<li><strong>4.JA\u20134.JD<\/strong> (arsenity\/antymonity\/bizmutyty \u2013 bez\/z dodatkowymi anionami; bez\/z H\u2082O),<\/li>\n<li><strong>4.JE<\/strong> (siarczyny),<\/li>\n<li><strong>4.JF\u20134.JJ<\/strong> (seleniny \u2013 cztery warianty \u201ebez\/z dodatkowymi anionami; bez\/z H\u2082O\u201d), oraz<\/li>\n<li><strong>4.JK\u20134.JN<\/strong> (telluryny \u2013 analogiczny uk\u0142ad).<\/li>\n<\/ul>\n<p>Uwaga: <strong>jodany<\/strong> s\u0105 rozwini\u0119te jako osobna klasa <strong>IV\/K<\/strong>.<\/p>\n<p><strong>Przyk\u0142ady.<\/strong> W <strong>4.JA<\/strong> znajdziesz m.in. <strong>schafarzykit<\/strong> FeSb\u2082O\u2084, <strong>trippkeit<\/strong> CuAs\u2082O\u2084, <strong>kusachit<\/strong> CuBi\u2082O\u2084, a tak\u017ce z\u0142o\u017cone Fe\u2013As: <strong>ludlockit<\/strong> PbFe\u2084As\u2081\u2080O\u2082\u2082. W <strong>4.JE (siarczyny)<\/strong> typowe s\u0105: <strong>scotlandyt<\/strong> PbSO\u2083, <strong>hannebachit<\/strong> CaSO\u2083\u00b7H\u2082O i <strong>orschallit<\/strong> Ca\u2083(SO\u2083)\u2082(SO\u2084)\u00b712H\u2082O. W\u015br\u00f3d <strong>seleninit\u00f3w<\/strong> (np. <strong>4.JF<\/strong>) klasyczne s\u0105 <strong>molybdomenit<\/strong> PbSeO\u2083 i <strong>paramolybdomenit<\/strong> PbSeO\u2083. W <strong>tellurynach<\/strong> (4.JK\u20134.JN) nale\u017c\u0105 m.in. <strong>plumbotellurynit<\/strong> PbTeO\u2083, <strong>rodalquilarit<\/strong> Fe\u2082(TeO\u2082OH)\u2083(TeO\u2083)Cl, <strong>moctezumit<\/strong> Pb(UO\u2082)(TeO\u2083)\u2082 i <strong>zemannit<\/strong> Mg\u2080\u2024\u2085ZnFe\u00b3\u207a(TeO\u2083)\u2083\u00b74\u20245H\u2082O. Parageneza tych minera\u0142\u00f3w to g\u0142\u00f3wnie <strong>strefy utleniania<\/strong> z\u0142\u00f3\u017c Pb\u2013Ag\u2013Cu, \u015brodowiska hydrotermalne i fumarolowe; w\u0142asno\u015bci fizyczne s\u0105 zr\u00f3\u017cnicowane (cz\u0119sto mi\u0119kkie, o barwach \u017c\u00f3\u0142tych, zielonych, pomara\u0144czowych lub brunatnych), co odzwierciedla zmienny stopie\u0144 polimeryzacji i udzia\u0142 dodatkowych anion\u00f3w\/wody w strukturze.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Grupa IV\/J Strunza (2025) \u2013 Arsenity, antymonity, bizmutyty; siarczyny, seleniny i telluryny obejmuje tlenkowe minera\u0142y, w kt\u00f3rych anionow\u0105 cz\u0119\u015b\u0107 struktury&hellip; <\/p>\n","protected":false},"author":1,"featured_media":0,"parent":2248,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"give_campaign_id":0,"_monsterinsights_skip_tracking":false,"_uf_show_specific_survey":0,"_uf_disable_surveys":false,"footnotes":""},"class_list":["post-2377","page","type-page","status-publish","hentry"],"aioseo_notices":[],"aioseo_head":"\n\t\t<!-- All in One SEO 5.0.0.1 - aioseo.com -->\n\t<meta name=\"description\" content=\"Grupa IV\/J Strunza (2025) \u2013 Arsenity, antymonity, bizmutyty; siarczyny, seleniny i telluryny obejmuje tlenkowe minera\u0142y, w kt\u00f3rych anionow\u0105 cz\u0119\u015b\u0107 struktury stanowi\u0105 odpowiednio grupy As(III), Sb(III), Bi(III) (arsenity\/antymonity\/bizmutyty) oraz aniony typu XO\u2083 z X = S(IV), Se(IV), Te(IV) (siarczyny\/seleniny\/telluryny). Dzia\u0142 ten porz\u0105dkuje te minera\u0142y wed\u0142ug obecno\u015bci dodatkowych anion\u00f3w (np. Cl\u207b, SO\u2084\u00b2\u207b) oraz wody krystalizacyjnej (H\u2082O). 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Dzia\u0142 ten porz\u0105dkuje te minera\u0142y wed\u0142ug obecno\u015bci dodatkowych anion\u00f3w (np. Cl\u207b, SO\u2084\u00b2\u207b) oraz wody krystalizacyjnej (H\u2082O). W","og:url":"https:\/\/dfoto.pl\/index.php\/about\/mineraly\/iv-tlenki-i-wodorotlenki\/iv-j-arsenity-antymonity-bizmutyty-siarczyny-seleniny-i-telluryny\/","article:published_time":"2025-10-02T23:41:21+00:00","article:modified_time":"2025-10-02T23:41:59+00:00","twitter:card":"summary_large_image","twitter:title":"IV\/J \u2013 Arsenity, antymonity, bizmutyty; siarczyny, seleniny i telluryny - dfoto","twitter:description":"Grupa IV\/J Strunza (2025) \u2013 Arsenity, antymonity, bizmutyty; siarczyny, seleniny i telluryny obejmuje tlenkowe minera\u0142y, w kt\u00f3rych anionow\u0105 cz\u0119\u015b\u0107 struktury stanowi\u0105 odpowiednio grupy As(III), Sb(III), Bi(III) (arsenity\/antymonity\/bizmutyty) oraz aniony typu XO\u2083 z X = S(IV), Se(IV), Te(IV) (siarczyny\/seleniny\/telluryny). 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