\n\t\t\t\tRoca subvolc\u00e1nica verde intercalada entre carbonatos marinos del Tri\u00e1sico superior.\n\t\t\t\t<\/figcaption><\/figure>\n\t\t<\/div>\n\n","protected":false},"excerpt":{"rendered":"Adem\u00e1s de todos estos tipos rocas, se pueden reconocer en los afloramientos del Tri\u00e1sico rocas verdes de origen volc\u00e1nico (ofitas). Durante el Tri\u00e1sico hubo etapas en las que el magma lleg\u00f3 a atravesar todas estas rocas sedimentarias ya depositadas. Cuando el magma alcanzaba la superficie se solidificaba y formaba las rocas volc\u00e1nicas.<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":365,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-479","page","type-page","status-publish","h-entry","hentry","h-as-page"],"_links":{"self":[{"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/479","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=479"}],"version-history":[{"count":1,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/479\/revisions"}],"predecessor-version":[{"id":812,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/479\/revisions\/812"}],"up":[{"embeddable":true,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/365"}],"wp:attachment":[{"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=479"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
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