{"id":1728,"date":"2020-10-23T12:15:17","date_gmt":"2020-10-23T15:15:17","guid":{"rendered":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/?page_id=1728"},"modified":"2020-10-23T12:35:57","modified_gmt":"2020-10-23T15:35:57","slug":"dolomito","status":"publish","type":"page","link":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/dolomito\/","title":{"rendered":"Dolomito"},"content":{"rendered":"<p><strong><span style=\"font-size: 14pt\">Defini\u00e7\u00e3o:<\/span> O\u00a0<b>dolomito<\/b> \u00e9 uma rocha sedimentar com mais de 50 % de seu peso constitu\u00eddo por\u00a0 dolomita \u00a0(carbonato duplo de c\u00e1lcio e magn\u00e9sio\u00a0[CaMg(CO<sub>3<\/sub>)<sub>2<\/sub>], cristalizado em romboedros, semelhante \u00e0\u00a0 calcita \u00a0mas menos sol\u00favel em \u00e1cidos), quase sempre associado e \u00e0s vezes interestratificado com o calcario.<sup id=\"cite_ref-1\" class=\"reference\"><\/sup><\/strong><\/p>\n<p style=\"text-align: right\"><span style=\"font-size: 10pt\">Fonte: https:\/\/pt.wikipedia.org\/wiki\/Dolomito<\/span><\/p>\n\n","protected":false},"excerpt":{"rendered":"<p>Defini\u00e7\u00e3o: O\u00a0dolomito \u00e9 uma rocha sedimentar com mais de 50 % de seu peso constitu\u00eddo por\u00a0 dolomita \u00a0(carbonato duplo de c\u00e1lcio e magn\u00e9sio\u00a0[CaMg(CO3)2], cristalizado em romboedros, semelhante \u00e0\u00a0 calcita \u00a0mas menos sol\u00favel em \u00e1cidos), quase sempre associado e \u00e0s vezes interestratificado com o calcario. Fonte: https:\/\/pt.wikipedia.org\/wiki\/Dolomito<\/p>\n","protected":false},"author":1048,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_crdt_document":"","footnotes":""},"class_list":["post-1728","page","type-page","status-publish","hentry","post"],"_links":{"self":[{"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/pages\/1728","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/users\/1048"}],"replies":[{"embeddable":true,"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/comments?post=1728"}],"version-history":[{"count":4,"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/pages\/1728\/revisions"}],"predecessor-version":[{"id":1741,"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/pages\/1728\/revisions\/1741"}],"wp:attachment":[{"href":"https:\/\/wp.ufpel.edu.br\/museudesolosrochaseminerais\/wp-json\/wp\/v2\/media?parent=1728"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}