{"id":131495,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-del-origen-y-evolucion-de-la-depresion-de-tirajana-gran-canaria\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"analisis-del-origen-y-evolucion-de-la-depresion-de-tirajana-gran-canaria","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/analisis-del-origen-y-evolucion-de-la-depresion-de-tirajana-gran-canaria\/","title":{"rendered":"Analisis del origen y evolucion de la depresion de tirajana, gran canaria."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Alejandro Lomoschitz Mora-figueroa <\/strong><\/h2>\n<p>En el centro-sur de gran canaria (islas canarias) existe una gran depresion en el terreno que corresponde a la cabecera del barranco de tirajana. En su interior se encuentran los denominados \u00abdepositos de deslizamientos gravitacionales\u00bb, que superan los 30 km2 en superficie.  la depresion se ha dividido en siete sectores, donde ha sido posible establecer la distribucion en planta y la geometria de los distintos cuerpos deslizados a una e.  1:10.000. Se han caracterizado 28 grandes deslizamientos que involucran volumenes desde 0.5x106m3 a 1.35 km3 de materiales.  la depresion como tal se inicio dentro del intervalo 0.6 m.A.-51.700 a\u00f1os bp. (Pleisceno medio-superior), y siguio evolucionando hasta la actualidad. Su genesis se atribuye grandes deslizamientos de terreno. Las hipotesis sobre el origen volcanico o tecto-volcanico han sido rechazadas.  por otro lado, se ha comprobado que la edad atribuida al origen y evolucion de su cabecera corresponde con la formacion del delta de juan grande en su cabecera corresponde con la formacion del delta de san juan grande en su desembocadura.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Analisis del origen y evolucion de la depresion de tirajana, gran canaria.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Analisis del origen y evolucion de la depresion de tirajana, gran canaria. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Alejandro Lomoschitz Mora-figueroa <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Polit\u00e9cnica de catalunya<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Jordi Corominas Dulcet<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Antonio Gens Sole <\/li>\n<li>Joan Marti Molist (vocal)<\/li>\n<li>Antonio Cendredo Uceda (vocal)<\/li>\n<li>David Serrat Congost (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alejandro Lomoschitz Mora-figueroa En el centro-sur de gran canaria (islas canarias) existe una gran depresion en el 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