{"id":116,"date":"2017-03-09T23:08:58","date_gmt":"2017-03-09T21:08:58","guid":{"rendered":"https:\/\/webs.uab.cat\/supraterra\/linies-de-recerca\/"},"modified":"2022-10-26T08:22:47","modified_gmt":"2022-10-26T06:22:47","slug":"linies-de-recerca","status":"publish","type":"page","link":"https:\/\/webs.uab.cat\/supraterra\/linies-de-recerca\/","title":{"rendered":"L\u00ednies de recerca"},"content":{"rendered":"\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects\/\" data-type=\"page\" data-id=\"139\">Rifting and inversion tectonics in the Atlas and Northern Andes rifts<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-0\/\" data-type=\"page\" data-id=\"140\">Salt tectonics in the Atlas, Pyrenees and Eastern Cordillera basins<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-1\/\" data-type=\"page\" data-id=\"141\">Crustal structure in the Atlas Mountains and Pyrenees from (hyper)extension to mountain building<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-2\">Tectonics and geomorphology in mountain belts<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-3\">Thermochronology and cosmogenic geochronology applied to mountain building and landform evolution<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-4\">Ordovician rift-related magmatism in the Variscan basement<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-5\">Compositional control on rock microstructural development<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-6\">Age of large shear zones and implications on the Variscan Ibero-Armorican arc<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-7\">SHRIMP precision zircon geochemistry and sediment provenance in orogenic belts<\/a><\/p>\n\n\n\n<p><a href=\"https:\/\/webs.uab.cat\/supraterra\/research-subjects-8\">Sulphide geochemistry and the composition of the lithospheric mantle<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Rifting and inversion tectonics in the Atlas and Northern Andes rifts Salt tectonics in the Atlas, Pyrenees and Eastern Cordillera basins Crustal structure in the Atlas Mountains and Pyrenees from (hyper)extension to mountain building Tectonics and geomorphology in mountain belts Thermochronology and cosmogenic geochronology applied to mountain building and landform evolution Ordovician rift-related magmatism in [&hellip;]<\/p>\n","protected":false},"author":20,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-116","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/pages\/116","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/users\/20"}],"replies":[{"embeddable":true,"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/comments?post=116"}],"version-history":[{"count":1,"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/pages\/116\/revisions"}],"predecessor-version":[{"id":350,"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/pages\/116\/revisions\/350"}],"wp:attachment":[{"href":"https:\/\/webs.uab.cat\/supraterra\/wp-json\/wp\/v2\/media?parent=116"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}