{"id":8089,"date":"2026-05-29T18:15:12","date_gmt":"2026-05-29T23:15:12","guid":{"rendered":"https:\/\/a.hithex.com\/?post_type=courses&#038;p=8089"},"modified":"2026-05-29T23:15:12","modified_gmt":"2026-05-29T23:15:12","slug":"sismica-avanzada","status":"publish","type":"courses","link":"https:\/\/a.hithex.com\/en\/courses\/sismica-avanzada\/","title":{"rendered":"C\u00d3MO SE ORIGINAN LOS TERREMOTOS: GEODIN\u00c1MICA Y TECT\u00d3NICA GLOBAL"},"content":{"rendered":"<div style=\"background: #050505;color: #f1f1f1;padding: 40px;border-radius: 20px;font-family: Arial,sans-serif;line-height: 1.8;border: 1px solid #121212;max-width: 1000px;margin: auto\">\n<h1 style=\"color: #ffffff;font-size: 36px;text-align: center;margin-bottom: 12px;letter-spacing: 1px\">C\u00d3MO SE ORIGINAN LOS TERREMOTOS:<\/p>\n<p>GEODIN\u00c1MICA Y TECT\u00d3NICA GLOBAL<\/h1>\n<p style=\"text-align: center;color: #8f9aa3;font-size: 16px;margin-bottom: 40px\">Formaci\u00f3n especializada del ecosistema THEK sobre din\u00e1mica planetaria,<br \/>tect\u00f3nica global y origen profundo de los sismos.<\/p>\n<div style=\"flex-wrap: wrap;align-items: center;gap: 35px;margin-bottom: 40px\">\n<div style=\"flex: 1;min-width: 280px\">\n<p style=\"font-size: 17px;color: #d6dce2\">Este curso explora los mecanismos internos que controlan la din\u00e1mica<br \/>de la Tierra y la formaci\u00f3n de los terremotos desde una perspectiva<br \/>geof\u00edsica y tect\u00f3nica moderna.<\/p>\n<p style=\"font-size: 17px;color: #d6dce2\">A trav\u00e9s del estudio del manto terrestre, la deriva continental,<br \/>la expansi\u00f3n del fondo marino y el campo magn\u00e9tico planetario,<br \/>comprender\u00e1s c\u00f3mo interact\u00faan las grandes estructuras internas<br \/>del planeta y c\u00f3mo estas influyen en la actividad s\u00edsmica global.<\/p>\n<\/div>\n<p><!-- FIGURA TIERRA --><\/p>\n<div style=\"width: 210px;text-align: center\">\n<p><img decoding=\"async\" style=\"width: 100%;border-radius: 16px;border: 1px solid #1f2a33;background: #0b0f13\" src=\"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/0\/07\/Earth-crust-cutaway-spanish.svg\" alt=\"Capas internas de la Tierra\" \/><\/p>\n<p style=\"font-size: 13px;color: #6f7d88;margin-top: 10px\">Estructura interna terrestre<\/p>\n<\/div>\n<\/div>\n<p><!-- APRENDER\u00c1S --><\/p>\n<div style=\"background: linear-gradient(145deg,#0b1116,#0f151c);padding: 28px;border-radius: 18px;border: 1px solid #18232d;margin-bottom: 30px\">\n<h2 style=\"color: #ffffff;font-size: 24px;margin-bottom: 18px\">\u00bfQu\u00e9 aprender\u00e1s?<\/h2>\n<ul style=\"padding-left: 22px;color: #cfd8df;font-size: 16px\">\n<li>Densidad y comportamiento din\u00e1mico del manto terrestre<\/li>\n<li>Fundamentos de la deriva continental y tect\u00f3nica de placas<\/li>\n<li>Procesos de expansi\u00f3n del fondo oce\u00e1nico<\/li>\n<li>Relaci\u00f3n entre magnetismo terrestre y din\u00e1mica geol\u00f3gica<\/li>\n<li>Origen geodin\u00e1mico de los terremotos<\/li>\n<li>Interacci\u00f3n entre estructuras profundas y actividad s\u00edsmica<\/li>\n<\/ul>\n<\/div>\n<p><!-- PUBLICO --><\/p>\n<div style=\"background: linear-gradient(145deg,#0a0d11,#10151a);padding: 28px;border-radius: 18px;border: 1px solid #1a242d;margin-bottom: 38px\">\n<h2 style=\"color: #ffffff;font-size: 24px;margin-bottom: 18px\">P\u00fablico objetivo<\/h2>\n<p style=\"color: #cfd8df;font-size: 16px\">Dirigido a estudiantes, investigadores, ingenieros, divulgadores cient\u00edficos<br \/>y personas interesadas en comprender el funcionamiento interno de la Tierra,<br \/>los terremotos y la evoluci\u00f3n tect\u00f3nica del planeta.<\/p>\n<\/div>\n<p><!-- BOTONES --><\/p>\n<div style=\"flex-wrap: wrap;justify-content: center;gap: 16px\">\n<p><a style=\"background: linear-gradient(145deg,#1b2733,#243847);color: #ffffff;padding: 14px 26px;text-decoration: none;border-radius: 12px;font-weight: bold;border: 1px solid #314656\" href=\"https:\/\/thekreport.goodstudy1.com\" target=\"_blank\" rel=\"noopener\"><br \/>THEK REPORT<br \/><\/a><\/p>\n<p><a style=\"background: linear-gradient(145deg,#101820,#18232d);color: #ffffff;padding: 14px 26px;text-decoration: none;border-radius: 12px;font-weight: bold;border: 1px solid #233543\" href=\"#\"><br \/>THEK RESEARCH INSTITUTE<br \/><\/a><\/p>\n<p><a style=\"background: linear-gradient(145deg,#0c1218,#161f28);color: #ffffff;padding: 14px 26px;text-decoration: none;border-radius: 12px;font-weight: bold;border: 1px solid #23313d\" href=\"#\"><br \/>CENTRO DE MONITOREO<br \/><\/a><\/p>\n<p><a style=\"background: linear-gradient(145deg,#131920,#1c2731);color: #ffffff;padding: 14px 26px;text-decoration: none;border-radius: 12px;font-weight: bold;border: 1px solid #30404f\" href=\"#\"><br \/>ESCUELA THEK<br \/>geolog\u00eda<\/a><\/p>\n<\/div>\n<\/div>","protected":false},"excerpt":{"rendered":"<p>C\u00d3MO SE ORIGINAN LOS TERREMOTOS: GEODIN\u00c1MICA Y TECT\u00d3NICA GLOBAL Formaci\u00f3n especializada del ecosistema THEK sobre din\u00e1mica planetaria,tect\u00f3nica global y origen<\/p>","protected":false},"author":1,"featured_media":8964,"template":"","course-category":[],"course-tag":[204,208,200,213,207,216,205,214,201,197,203,210,146,202,209,215,206,219,212,217,218,196,198,199,195,211,220,221],"class_list":["post-8089","courses","type-courses","status-publish","has-post-thumbnail","hentry","course-tag-actividad-sismica","course-tag-ciencias-de-la-tierra","course-tag-deriva-continental","course-tag-dinamica-planetaria","course-tag-dinamica-terrestre","course-tag-earth-dynamics","course-tag-estructura-interna-de-la-tierra","course-tag-evolucion-tectonica","course-tag-expansion-del-fondo-marino","course-tag-geodinamica","course-tag-geofisica","course-tag-geologia","course-tag-ingenieria-sismica","course-tag-manto-terrestre","course-tag-monitoreo-sismico","course-tag-ondas-sismicas","course-tag-placas-tectonicas","course-tag-planetary-geology","course-tag-riesgos-naturales","course-tag-seismic-activity","course-tag-seismic-science","course-tag-sismos","course-tag-tectonica-de-placas","course-tag-tectonica-global","course-tag-terremotos","course-tag-terremotos-globales","course-tag-thek","course-tag-thek-research-institute"],"jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/courses\/8089","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/courses"}],"about":[{"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/types\/courses"}],"author":[{"embeddable":true,"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/users\/1"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/media\/8964"}],"wp:attachment":[{"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/media?parent=8089"}],"wp:term":[{"taxonomy":"course-category","embeddable":true,"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/course-category?post=8089"},{"taxonomy":"course-tag","embeddable":true,"href":"https:\/\/a.hithex.com\/en\/wp-json\/wp\/v2\/course-tag?post=8089"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}