{"id":811,"date":"2023-03-15T14:57:16","date_gmt":"2023-03-15T13:57:16","guid":{"rendered":"http:\/\/www.krantz.unipr.it\/?post_type=product&#038;p=811"},"modified":"2023-03-15T15:01:43","modified_gmt":"2023-03-15T14:01:43","slug":"413-camptonite-con-sodalite-2","status":"publish","type":"product","link":"http:\/\/www.krantz.unipr.it\/index.php\/prodotto\/413-camptonite-con-sodalite-2\/","title":{"rendered":"413-Camptonite con sodalite"},"content":{"rendered":"<p><strong>DESCRIZIONE:<\/strong><\/p>\n<p>I lamprofiri alcalini sono rocce affini alle basaniti e ai basalti alcalini. Sono spesso associati a rocce carbonatitiche. La loro origine \u00e8 legata, probabilmente, alla differenziazione di magmi basanitici o tefritici, in zone di rifting continentale. A questo gruppo appartengono: <strong>camptoniti<\/strong>, monchiquiti, sannaiti, fourchiti e altre rare rocce. http:\/\/www.alexstrekeisen.it\/vulc\/lamprofiri.php<\/p>\n<p><strong>\u00a0<\/strong><strong>VISTA A 360\u00b0<\/strong><\/p>\n<p><iframe loading=\"lazy\" src=\"https:\/\/www.krantz.unipr.it\/360\/413-Kamptonite con sodalite\/413-Kamptonite con sodalite.html\" width=\"1100\" height=\"700\"><span style=\"display: inline-block; width: 0px; overflow: hidden; line-height: 0;\" data-mce-type=\"bookmark\" class=\"mce_SELRES_start\">\ufeff<\/span><span style=\"display: inline-block; width: 0px; overflow: hidden; line-height: 0;\" data-mce-type=\"bookmark\" class=\"mce_SELRES_start\">\ufeff<\/span><span style=\"display: inline-block; width: 0px; overflow: hidden; line-height: 0;\" data-mce-type=\"bookmark\" class=\"mce_SELRES_start\">\ufeff<\/span><span style=\"display: inline-block; width: 0px; overflow: hidden; line-height: 0;\" data-mce-type=\"bookmark\" class=\"mce_SELRES_start\">\ufeff<\/span><span style=\"display: inline-block; 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width: 0px; overflow: hidden; line-height: 0;\" data-mce-type=\"bookmark\" class=\"mce_SELRES_start\">\ufeff<\/span><span style=\"display: inline-block; width: 0px; overflow: hidden; line-height: 0;\" data-mce-type=\"bookmark\" class=\"mce_SELRES_start\"><span style=\"display: inline-block; width: 0px; overflow: hidden; line-height: 0;\" data-mce-type=\"bookmark\" class=\"mce_SELRES_start\">\ufeff<\/span>\ufeff<\/span><\/iframe><\/p>\n","protected":false},"excerpt":{"rendered":"<p><strong>Collocazione: <\/strong>Vetrina 12, quarto ripiano<\/p>\n<p><strong>Localit\u00e0:\u00a0<\/strong>Roda, Predazzo (Trentino Alto Adige)<\/p>\n<p><b><span data-contrast=\"auto\">Descrizione macroscopica:<\/span><\/b> termine derivante da Campton, New Hampshire, USA. Le camptoniti sono lamprofiri contenenti fenocristalli di anfibolo (kaersutite e\/o orneblenda), Ti-augite, olivina e biotite-flogopite, immersi in una pasta di fondo costituita da plagioclasio, anfibolo e talvolta feldspatoidi. La sodalite, il cui nome deriva dalla sua composizione chimica, venne scoperta nel 1811 nel complesso alcalino di Ilimaussaq in Groenlandia. I minerali del gruppo della sodalite hanno una struttura basata su unit\u00e0 di forma cubo-ottaedrica caratterizzate da ampie cavit\u00e0 in cui vengono accomodati cationi a grande raggio ionico (Cl<sup>&#8211;<\/sup>, S<sub>2<\/sub> o SO<sub>4<\/sub><sup>2-<\/sup>) circondate da Na<sup>+<\/sup> o Ca<sup>2+<\/sup> in coordinazione tetraedrica. http:\/\/www.alexstrekeisen.it<\/p>\n<p><b><span data-contrast=\"auto\">Descrizione\u00a0<\/span><\/b><b><span data-contrast=\"auto\">microfoto<\/span><\/b><b><span data-contrast=\"auto\">:\u00a0<\/span><\/b><\/p>\n<p><strong>prima immagine:\u00a0<\/strong>Cristallo di sodalite (incolore) incluso in eudialite (alto rilievo e di colore bianco sporco-rosa pallido) in una Naujaite. Il\u00edmaussaq, Groenlandia. Immagine a N\/\/, 2x (lato lungo = 7mm)<\/p>\n<p><strong>seconda immagine: <\/strong>Sodalite (estinta) circondata da cancrinite (alti colori di interferenza) inclusa in eudialite (grigio) in una Naujaite. Il\u00edmaussaq, Groenlandia. Immagine a NX, 2x (lato lungo = 7mm)<\/p>\n<p><strong>terza immagine: <\/strong>Cristalli di Sodalite (estinti), biotite e cristalli di Feldspati alcalini in una sienite a sodalite (&#8220;azul bahia&#8221;), Brasile. Immagine a NX, 2x (lato lungo = 7mm)<strong><br \/>\n<\/strong><\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n","protected":false},"featured_media":815,"template":"","meta":{"_lmt_disableupdate":"no","_lmt_disable":"no"},"product_cat":[23],"product_tag":[],"class_list":{"0":"post-811","1":"product","2":"type-product","3":"status-publish","6":"product_cat-magmatiche-ipoabissali","8":"first","9":"outofstock","10":"shipping-taxable","11":"product-type-simple"},"_links":{"self":[{"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/product\/811","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/product"}],"about":[{"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/types\/product"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/media\/815"}],"wp:attachment":[{"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/media?parent=811"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/product_cat?post=811"},{"taxonomy":"product_tag","embeddable":true,"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/product_tag?post=811"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}