{"id":1160,"date":"2018-09-09T15:05:50","date_gmt":"2018-09-09T15:05:50","guid":{"rendered":"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=1160"},"modified":"2018-10-04T20:09:21","modified_gmt":"2018-10-04T20:09:21","slug":"tinciones-en-carbonatos","status":"publish","type":"page","link":"https:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=1160","title":{"rendered":"Tinciones en carbonatos"},"content":{"rendered":"<ul>\n<li>Mineralog\u00eda. T\u00e9cnicas de estudio: <strong>tinciones<\/strong> y difusor.<\/li>\n<li>Descripci\u00f3n de una <a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=857\">dolom\u00eda<\/a> en funci\u00f3n del tama\u00f1o y morfolog\u00eda cristalina, y textura.<\/li>\n<li>Dolom\u00eda mim\u00e9tica (fantasmas).<\/li>\n<\/ul>\n<h6 style=\"text-align: right;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=842\">INDICE<\/a><\/h6>\n<hr \/>\n<figure id=\"attachment_914\" aria-describedby=\"caption-attachment-914\" style=\"width: 911px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-914 size-full\" src=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/wp-content\/uploads\/2018\/09\/dolo-cal.jpg\" alt=\"\" width=\"911\" height=\"610\" srcset=\"https:\/\/wpd.ugr.es\/~aperezl\/web\/wp-content\/uploads\/2018\/09\/dolo-cal.jpg 911w, https:\/\/wpd.ugr.es\/~aperezl\/web\/wp-content\/uploads\/2018\/09\/dolo-cal-300x201.jpg 300w, https:\/\/wpd.ugr.es\/~aperezl\/web\/wp-content\/uploads\/2018\/09\/dolo-cal-768x514.jpg 768w\" sizes=\"auto, (max-width: 911px) 100vw, 911px\" \/><figcaption id=\"caption-attachment-914\" class=\"wp-caption-text\">Antes de cubrir una l\u00e1mina se puede te\u00f1ir con Alizarin Red S y, de esta manera, los cristales de calcita tomar\u00e1n un color rojo. \u00c9sta es una t\u00e9cnica para diferenciar la calcita de la dolomita. En esta l\u00e1mina s\u00f3lo algunas zonas corresponden a cristales de calcita. La mayor parte de los cristales son de dolomita (cristales no te\u00f1idos de rojo).<\/figcaption><\/figure>\n<h6 style=\"text-align: right;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=842\">INDICE<\/a><\/h6>\n","protected":false},"excerpt":{"rendered":"<p>Mineralog\u00eda. T\u00e9cnicas de estudio: tinciones y difusor. Descripci\u00f3n de una dolom\u00eda en funci\u00f3n del tama\u00f1o y morfolog\u00eda cristalina, y textura. Dolom\u00eda mim\u00e9tica (fantasmas). INDICE INDICE<\/p>\n","protected":false},"author":1,"featured_media":1338,"parent":842,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-templates\/full-width.php","meta":{"footnotes":""},"class_list":["post-1160","page","type-page","status-publish","has-post-thumbnail","h-entry","hentry","h-as-page"],"_links":{"self":[{"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/1160","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1160"}],"version-history":[{"count":10,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/1160\/revisions"}],"predecessor-version":[{"id":1288,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/1160\/revisions\/1288"}],"up":[{"embeddable":true,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/842"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/media\/1338"}],"wp:attachment":[{"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1160"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}