{"id":19177,"date":"2018-03-09T09:08:04","date_gmt":"2018-03-09T09:08:04","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/comportamiento-como-arido-para-pavimento-de-ofitas-de-cantabria\/"},"modified":"2018-03-09T09:08:04","modified_gmt":"2018-03-09T09:08:04","slug":"comportamiento-como-arido-para-pavimento-de-ofitas-de-cantabria","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/comportamiento-como-arido-para-pavimento-de-ofitas-de-cantabria\/","title":{"rendered":"Comportamiento como \u00e1rido para pavimento de ofitas de cantabria"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Gema Fern\u00e1ndez Maroto <\/strong><\/h2>\n<p>La presente tesis estudia la correlaci\u00f3n entre la petrograf\u00eda de ofitas de cantabria y su comportamiento como \u00e1rido de pavimento. Para ello se estudian todos los afloramientos y ofitas existentes en cantabria, seleccionando siete de ellos en los que se realizan un estudio cartogr\u00e1fico, estudio petrogr\u00e1fico de las rocas extra\u00eddas y los ensayos de caracterizaci\u00f3n adecuados a su utilizaci\u00f3n pr\u00e1ctica: densidad, porosidad, absorci\u00f3n de agua, coeficiente de desgaste de los \u00e1ngeles, coeficiente de pulimento acelerado, velocidad de propagaci\u00f3n de ondas el\u00e1sticas y resistencia a la compresi\u00f3n uniaxial. las variaciones de comportamiento de los \u00e1ridos se deben tanto a factores de composici\u00f3n mineral\u00f3gica como a factores texturales: el mayor o menor contenido de fases mayoritarias, el tama\u00f1o de grano de los piroxenos, la fisuraci\u00f3n intergranular, el grado de alteraci\u00f3n de los minerales, etc. finalmente se establecen un \u00edndice de explotabilidad enfocado a la jerarquizaci\u00f3n de todos los afloramientos estudiados, para su aprovechamiento como recurso natural.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Comportamiento como \u00e1rido para pavimento de ofitas de cantabria<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Comportamiento como \u00e1rido para pavimento de ofitas de cantabria <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Gema Fern\u00e1ndez Maroto <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 26\/09\/2002<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Gil Fernandez Alvarez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Antonio Arribas moreno <\/li>\n<li>Miguel Torres alonso (vocal)<\/li>\n<li>Jes\u00fas Soriano carrillo (vocal)<\/li>\n<li> D\u00edaz de ter\u00e1n Jos\u00e9 ram\u00f3n (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gema Fern\u00e1ndez Maroto La presente tesis estudia la correlaci\u00f3n entre la petrograf\u00eda de ofitas de cantabria y [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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