{"id":822,"date":"2023-03-16T09:53:22","date_gmt":"2023-03-16T08:53:22","guid":{"rendered":"http:\/\/www.krantz.unipr.it\/?post_type=product&#038;p=822"},"modified":"2023-04-17T11:29:43","modified_gmt":"2023-04-17T09:29:43","slug":"445-basalto-amigdaloide","status":"publish","type":"product","link":"http:\/\/www.krantz.unipr.it\/index.php\/prodotto\/445-basalto-amigdaloide\/","title":{"rendered":"445-Basalto amigdaloide"},"content":{"rendered":"<p><audio class=\"audio-for-speech\"><\/audio><\/p>\n<div class=\"translate-tooltip-mtz translator-hidden\">\n<div class=\"header\">\n<div class=\"header-controls\">Translator<\/div>\n<div class=\"header-controls\"><\/div>\n<\/div>\n<div class=\"translated-text\">\n<div class=\"words\"><\/div>\n<div class=\"sentences\"><\/div>\n<\/div>\n<\/div>\n<p>&nbsp;<\/p>\n<p><strong>DESCRIZIONE:<\/strong><\/p>\n<p>Le amigdale si formano quando vescicole vulcaniche vengono riempite da minerali secondari, derivanti da fluidi circolanti o da processi di alterazione a bassa temperatura. Il termine amigdala deriva dal termine latino &#8220;amygdale&#8221; (mandorla) in quanto queste cavit\u00e0 hanno comunemente una colorazione ed una forma simile alle mandorle. I minerali che comunemente costituiscono le amigdale sono: calcedonio, calcite, ematite o zeoliti. Spesso le amigdale mostrano una morfologia allungata, ci\u00f2 \u00e8 dovuto al fatto che le originarie vescicole vulcaniche sono state deformate dal flusso lavico e per questo motivo, vescicole e amigdale, sono ottimi indicatori per ricostruire il senso di scorrimento di una colata lavica. http:\/\/www.alexstrekeisen.it\/<\/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\/445- Basalto amigdaloide\/445- Basalto amigdaloide.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; 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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\">\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; 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; 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><audio class=\"audio-for-speech\"><\/audio><\/p>\n<div class=\"translate-tooltip-mtz translator-hidden\">\n<div class=\"header\">\n<div class=\"header-controls\">Translator<\/div>\n<div class=\"header-controls\"><\/div>\n<\/div>\n<div class=\"translated-text\">\n<div class=\"words\"><\/div>\n<div class=\"sentences\"><\/div>\n<\/div>\n<\/div>\n<p>&nbsp;<\/p>\n<p><strong>Collocazione: <\/strong>Vetrina 13, quinto ripiano<\/p>\n<p><strong>Localit\u00e0:\u00a0<\/strong>Ahausen, Weilburg (Nassau) &#8211; Germania<\/p>\n<p><b><span data-contrast=\"auto\">Descrizione macroscopica: <\/span><\/b>I basalti sono rocce vulcaniche a grana fine formate essenzialmente da plagioclasio, pirosseno (generalmente augite) e quantit\u00e0 variabili di olivina. Fasi comuni possono essere: orneblenda, biotite, ortopirosseno e feldspatoidi. I basalti sono generalmente porfirici e possono contenere comunemente xenoliti mantellici.<\/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\">: <\/span><\/b><\/p>\n<p><strong>prima immagine:\u00a0<\/strong>Amigdala riempita da calcedonio. Immagine a NX, 2x (lato lungo = 7mm)<\/p>\n<p><strong>seconda immagine:\u00a0<\/strong>Amigdala riempita da calcite. Antartide. Immagine a N\/\/, 2x (lato lungo = 7mm)<\/p>\n<p><strong>terza immagine:\u00a0<\/strong>Amigdala riempita da ossidi di ferro. Antartide. Immagine a N\/\/, 10x (lato lungo = 2mm)<\/p>\n<p>http:\/\/www.alexstrekeisen.it\/<\/p>\n","protected":false},"featured_media":823,"template":"","meta":{"_lmt_disableupdate":"no","_lmt_disable":"no"},"product_cat":[23],"product_tag":[],"class_list":{"0":"post-822","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\/822","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\/823"}],"wp:attachment":[{"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/media?parent=822"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/product_cat?post=822"},{"taxonomy":"product_tag","embeddable":true,"href":"http:\/\/www.krantz.unipr.it\/index.php\/wp-json\/wp\/v2\/product_tag?post=822"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}