{"id":77998,"date":"2018-03-09T23:23:38","date_gmt":"2018-03-09T23:23:38","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/dinamica-sedimentaria-del-canon-submarino-de-palamos\/"},"modified":"2018-03-09T23:23:38","modified_gmt":"2018-03-09T23:23:38","slug":"dinamica-sedimentaria-del-canon-submarino-de-palamos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/dinamica-sedimentaria-del-canon-submarino-de-palamos\/","title":{"rendered":"Dinamica sedimentaria del ca\u00f1on submarino de palamos."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jacobo Martin De Nascimento <\/strong><\/h2>\n<p>The present thesis focuses on the transfer and accumulation of particulate matter in the  palam\u00f3s canyon, located in the northwestern mediterranean. In the context of the  canyons project, 7 moorings with a total of 7 sediment traps and 18 current meters (some of them equipped with turbidimeters) were deployed in the palam\u00f3s submarine canyon and adjacent slope from march to november 2001, during two consecutive deployments.  total mass fluxes, major constituents (organic carbon, opal, calcium carbonate and lithogenics) contents and fluxes, granulometry and 210pb activity of particulate matter from sediment trap samples were analysed. Horizontal fluxes of suspended particulate matter were calculated from the current meter\/nephelometer pairs. Additionally, three sediment cores were collected in the canyon axis and dated with the radionuclides 210pb and 137cs.  downward particle fluxes measured in the palam\u00f3s canyon were highly variable and significantly higher than those measured in other northwestern mediterranean canyons at similar depths. This high sedimentological activity is related to the morphological characteristics of the canyon and the fact that it incises almost the full width of the continental shelf, with the canyon head located a few kilometres from the coastline.  besides, the steep canyon walls and the gullies incised in the walls enhance the transference of particles from the shelf and upper slope into the canyon. the results evidence that the palam\u00f3s canyon acts as a preferential path for offshore export ofparticulate matter. This difference was further heightened during a major storm in  november 2001.  the spatial-temporal distribution of total mass fluxes and major constituents allowed two domains to be defined in the palam\u00f3s canyon: an inner domain (up to 1200 m depth) constricted by the canyon topography and mainly influenced by the lateral transport of particulate matter from the adjoining shelf, and an<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Dinamica sedimentaria del ca\u00f1on submarino de palamos.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Dinamica sedimentaria del ca\u00f1on submarino de palamos. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jacobo Martin De Nascimento <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Polit\u00e9cnica de catalunya<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 19\/12\/2005<\/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>Alberto Palanques Monteys<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jorge Guill\u00e9n aranda <\/li>\n<li>pere Masqu barri (vocal)<\/li>\n<li> Durrieu de madron xavier (vocal)<\/li>\n<li> Calafat frau Antonio  m. (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jacobo Martin De Nascimento The present thesis focuses on the transfer and accumulation of particulate matter in [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,953,3645,228,15596,37401,3857],"tags":[37403,117042,72335,167781,37405,117043],"class_list":["post-77998","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-ambiental","category-oceanografia","category-politecnica-de-catalunya","category-procesos-del-fondo-marino","category-sedimentologia","tag-alberto-palanques-monteys","tag-calafat-frau-antonio-m","tag-durrieu-de-madron-xavier","tag-jacobo-martin-de-nascimento","tag-jorge-guillen-aranda","tag-pere-masqu-barri"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/77998","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=77998"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/77998\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=77998"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=77998"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=77998"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}