{"id":14264,"date":"2021-07-23T17:13:55","date_gmt":"2021-07-23T15:13:55","guid":{"rendered":"http:\/\/volcanx.cluster031.hosting.ovh.net\/?post_type=glossary&#038;p=14264"},"modified":"2021-07-26T17:28:49","modified_gmt":"2021-07-26T15:28:49","slug":"dique-es","status":"publish","type":"glossary","link":"https:\/\/volcanofoundation.org\/es\/glossary\/dique-es\/","title":{"rendered":"DIQUE"},"content":{"rendered":"<p>Los diques son cuerpos tabulares o en forma de l&aacute;mina de <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> que cortan a trav&eacute;s y a trav&eacute;s de las capas de rocas adyacentes. Se forman cuando el <a class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\"  href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'  tabindex='0' role='link'>magma<\/a> se eleva a una fractura existente, o crea una nueva grieta forzando su camino a trav&eacute;s de la roca existente, y luego se solidifica. Cientos de diques pueden invadir el cono y el n&uacute;cleo interior de un volc&aacute;n, a veces preferentemente a lo largo de zonas de debilidad estructural.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Los diques son cuerpos tabulares o en forma de l&aacute;mina de <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">magma<\/a> que cortan a trav&eacute;s y a trav&eacute;s de las capas de rocas adyacentes. Se forman cuando el <a class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MAGMA&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Roca fundida bajo la superficie de la Tierra.&lt;\/div&gt;\" href=\"https:\/\/volcanofoundation.org\/es\/glossary\/magma-es\/\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]' tabindex=\"0\" role=\"link\">magma<\/a> se eleva a una fractura existente, o crea una nueva grieta forzando su camino a trav&eacute;s de la roca existente, y luego se solidifica. Cientos [&hellip;]<\/p>\n","protected":false},"author":8,"featured_media":0,"menu_order":0,"template":"","meta":{"footnotes":""},"class_list":["post-14264","glossary","type-glossary","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/glossary\/14264","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/glossary"}],"about":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/types\/glossary"}],"author":[{"embeddable":true,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/users\/8"}],"version-history":[{"count":0,"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/glossary\/14264\/revisions"}],"wp:attachment":[{"href":"https:\/\/volcanofoundation.org\/es\/wp-json\/wp\/v2\/media?parent=14264"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}