{"id":12,"date":"2013-11-14T14:23:35","date_gmt":"2013-11-14T14:23:35","guid":{"rendered":"http:\/\/wdb.ugr.es\/~aperezl\/?page_id=12"},"modified":"2023-05-03T07:16:27","modified_gmt":"2023-05-03T07:16:27","slug":"investigacion","status":"publish","type":"page","link":"https:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=12","title":{"rendered":"Investigaci\u00f3n"},"content":{"rendered":"<h5>Centros de trabajo:<\/h5>\n<p>\u00b7 <a href=\"http:\/\/www.ugrestratig.es\/index.php\">Departamento de Estratigraf\u00eda y Paleontolog\u00eda<\/a><br \/>\n\u00b7 <a href=\"http:\/\/www.iact.csic.es\/\">Instituto Andaluz de Ciencias de la Tierra (CSIC-Universidad de Granada)<\/a><\/p>\n<p><strong>L\u00edneas y temas de investigaci\u00f3n:<\/strong><\/p>\n<ul>\n<li>Estratigraf\u00eda, Sedimentolog\u00eda, Bioestratigraf\u00eda, Paleogeograf\u00eda y Tect\u00f3nica.<\/li>\n<li>Petrolog\u00eda sedimentaria, facies sedimentarias, medios sedimentarios, discontinuidades estratigr\u00e1ficas.<\/li>\n<li>Plataformas carbon\u00e1ticas, llanuras de mareas, sistemas fluviales costeros.<\/li>\n<li>Carbonatos.<\/li>\n<li>El Tri\u00e1sico.<\/li>\n<\/ul>\n<ol>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=409\" target=\"_blank\" rel=\"noopener\">El Tri\u00e1sico en la Cordillera B\u00e9tica<\/a><\/li>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=395\" target=\"_blank\" rel=\"noopener\">Estratigraf\u00eda del Tri\u00e1sico de facies epicontinental<\/a><\/li>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=399\" target=\"_blank\" rel=\"noopener\">Unidades carbonatadas de facies Muschelkalk<\/a><\/li>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=413\" target=\"_blank\" rel=\"noopener\">El Tri\u00e1sico superior (Formaci\u00f3n Zamoranos) <\/a><\/li>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=404\" target=\"_blank\" rel=\"noopener\">Dep\u00f3sitos de tormenta<\/a><\/li>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=612\" target=\"_blank\" rel=\"noopener\">Evaporitas<\/a><\/li>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=406\" target=\"_blank\" rel=\"noopener\">Diapirismo y resedimentaci\u00f3n<\/a><\/li>\n<li style=\"padding-left: 30px;\"><a href=\"http:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=617\" target=\"_blank\" rel=\"noopener\">Tect\u00f3nica del Tri\u00e1sico<\/a><\/li>\n<li>\u00a0\u00a0\u00a0\u00a0\u00a0 <a href=\"https:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=1434\" target=\"_blank\" rel=\"noopener\">Tect\u00f3nica y sedimentaci\u00f3n (sismitas)<\/a><\/li>\n<\/ol>\n<hr \/>\n<p style=\"text-align: justify;\"><span style=\"color: #800000;\"><strong>Investigador responsable del Grupo de Investigaci\u00f3n de la Junta de Andaluc\u00eda:<\/strong> <\/span><\/p>\n<p style=\"text-align: justify; padding-left: 30px;\"><span style=\"color: #800000;\"><span style=\"color: #333333;\">RNM 208 - Discontinuidades estratigr\u00e1ficas.<\/span><\/span><\/p>\n<p><span style=\"color: #800000;\"><strong>Proyectos actuales de investigaci\u00f3n:<\/strong><\/span><\/p>\n<ul>\n<li>Relaci\u00f3n continente-oc\u00e9ano en la crisis y recuperaci\u00f3n de los ecosistemas en la margen O del Tethys durante la transici\u00f3n P\u00e9rmico-Tri\u00e1sico.<\/li>\n<\/ul>\n<p style=\"padding-left: 60px;\"><em>Investigadores principales:<\/em> Jos\u00e9 T. L\u00f3pez G\u00f3mez y Jos\u00e9 Mar\u00eda Fern\u00e1ndez Barrenechea <em>(Instituto de Geociencias, CSIC-UCM, Madrid)<\/em>.<\/p>\n<ul>\n<li>Cambios bruscos y prolongados en el ecosistema, par\u00e1metros de control e indicadores bi\u00f3ticos\/abi\u00f3ticos: el registro icnol\u00f3gico en el an\u00e1lisis de variaciones paleoambientales.<\/li>\n<\/ul>\n<p style=\"padding-left: 60px;\"><em>Investigador principal: <\/em>Francisco J. Rodr\u00edguez Tovar <em>(Universidad de Granada).<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Centros de trabajo: \u00b7 Departamento de Estratigraf\u00eda y Paleontolog\u00eda \u00b7 Instituto Andaluz de Ciencias de la Tierra (CSIC-Universidad de Granada) L\u00edneas y temas de investigaci\u00f3n: Estratigraf\u00eda, Sedimentolog\u00eda, Bioestratigraf\u00eda, Paleogeograf\u00eda y Tect\u00f3nica. Petrolog\u00eda sedimentaria, facies sedimentarias, medios sedimentarios, discontinuidades estratigr\u00e1ficas. Plataformas carbon\u00e1ticas, llanuras de mareas, sistemas fluviales costeros. Carbonatos. El Tri\u00e1sico. El Tri\u00e1sico en la Cordillera <a href=\"https:\/\/wpd.ugr.es\/~aperezl\/web\/?page_id=12\" class=\"more-link\">...contin\u00faa leyendo<span class=\"screen-reader-text\"> \"Investigaci\u00f3n\"<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-12","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\/12","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=12"}],"version-history":[{"count":23,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/12\/revisions"}],"predecessor-version":[{"id":1730,"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=\/wp\/v2\/pages\/12\/revisions\/1730"}],"wp:attachment":[{"href":"https:\/\/wpd.ugr.es\/~aperezl\/web\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=12"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}