{"id":185,"date":"2015-05-01T21:20:56","date_gmt":"2015-05-01T21:20:56","guid":{"rendered":"http:\/\/sedimentologia.org.ar\/spa\/?page_id=185"},"modified":"2020-11-23T11:27:21","modified_gmt":"2020-11-23T11:27:21","slug":"volumen-15-2008","status":"publish","type":"page","link":"https:\/\/www.sedimentologia.org.ar\/spa\/revista\/volumen-15-2008\/","title":{"rendered":"Volumen 15 | 2008"},"content":{"rendered":"<p><a href=\"http:\/\/sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-1.png\"><img decoding=\"async\" class=\"alignnone size-full wp-image-250\" src=\"http:\/\/sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-1.png\" alt=\"LAJSBA_15-1\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-1-66x66.png 66w, https:\/\/www.sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-1-150x150.png 150w, https:\/\/www.sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-1.png 300w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n<h2 style=\"text-align: left;\"><strong>Volumen 15 &#8211; N\u00famero 1 <\/strong>| Julio 2008<\/h2>\n<p><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-1 hundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-overflow:visible;--awb-margin-top:-15px;--awb-margin-bottom:5px;--awb-background-color:rgba(255,255,255,0);--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-0 fusion_builder_column_1_1 1_1 fusion-one-full fusion-column-first fusion-column-last fusion-column-no-min-height\" style=\"--awb-bg-size:cover;--awb-margin-bottom:0px;\"><div class=\"fusion-column-wrapper fusion-flex-column-wrapper-legacy\"><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;width:100%;\"><div class=\"fusion-separator-border sep-single sep-solid\" style=\"--awb-height:20px;--awb-amount:20px;border-color:#e0dede;border-top-width:1px;\"><\/div><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><em><strong>Editor:<\/strong> Gerardo M. E. Perillo <\/em>| <em>80 p\u00e1ginas<\/em><\/p>\n<div class=\"fusion-clearfix\"><\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-2 hundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-overflow:visible;--awb-margin-top:0px;--awb-margin-bottom:20px;--awb-background-color:rgba(255,255,255,0);--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-1 fusion_builder_column_1_1 1_1 fusion-one-full fusion-column-first fusion-column-last fusion-column-no-min-height\" style=\"--awb-bg-size:cover;--awb-margin-bottom:0px;\"><div class=\"fusion-column-wrapper fusion-flex-column-wrapper-legacy\"><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<div class=\"fusion-clearfix\"><\/div><\/div><\/div><\/div><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-3 hundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-overflow:visible;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-2 fusion_builder_column_1_1 1_1 fusion-one-full fusion-column-first fusion-column-last fusion-column-no-min-height\" style=\"--awb-bg-size:cover;--awb-margin-bottom:0px;\"><div class=\"fusion-column-wrapper fusion-flex-column-wrapper-legacy\"><div class=\"fusion-title title fusion-title-1 fusion-title-text fusion-title-size-three\"><h3 class=\"fusion-title-heading title-heading-left\" style=\"margin:0;\">CONTENIDO<\/h3><span class=\"awb-title-spacer\"><\/span><div class=\"title-sep-container\"><div class=\"title-sep sep-single sep-solid\" style=\"border-color:#e0dede;\"><\/div><\/div><\/div>\n<p><strong>AN\u00c1LISIS ESTRATIGR\u00c1FICO SECUENCIAL DE LAS FORMACIONES HUINCUL Y LISANDRO DEL SUBGRUPO R\u00cdO LIMAY (GRUPO NEUQU\u00c9N &#8211; CRET\u00c1CICO TARD\u00cdO) EN EL DEPARTAMENTO EL CUY, R\u00cdO NEGRO, ARGENTINA<br \/>\n<\/strong><em>M.L. S\u00e1nchez, J. Rossi, S. Morra y P. Armas <\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-1 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000100001&amp;lng=es&amp;nrm=iso&amp;tlng=es\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><strong>PETROGRAF\u00cdA Y GEOQU\u00cdMICA DE LA DOLOM\u00cdA HOSPEDANTE DE UNA MINERALIZACI\u00d3N DE ZN Y PB. PUESTO GREGOR, NEUQU\u00c9N, ARGENTINA<\/strong><br \/>\n<em>M. Cristina G\u00f3mez, Mirta Garrido, Nora Cesaretti y Eduardo Dom\u00ednguez<\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-2 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000100002&amp;lng=es&amp;nrm=iso&amp;tlng=es\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><strong>-SHORT NOTE- GLACIAL DEPOSITS IN THE R\u00cdO DEL PE\u00d1\u00d3N FORMATION (LATE CARBONIFEROUS), R\u00cdO BLANCO BASIN, NORTHWESTERN ARGENTINA<\/strong><br \/>\n<em>E. Gulbranson, C.O. Limarino, S. Marenssi, I. Montanez, N. Tabor, <\/em><em>V. Davydov and C. Colombi<\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-3 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000100003&amp;lng=es&amp;nrm=iso&amp;tlng=en\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><strong>AMBIENTES DE INTERACCI\u00d3N E\u00d3LICA-FLUVIAL EN VALLES INTERMONTANOS: EJEMPLOS ACTUALES Y ANTIGUOS<\/strong><br \/>\n<em>Alfonsina Tripaldi y Carlos O. Limarino<\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-4 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000100004&amp;lng=es&amp;nrm=iso&amp;tlng=es\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><strong>SCREENING OF SEDIMENT POLLUTION IN TRIBUTARIES FROM THE SOUTHWESTERN COAST OF THE R\u00cdO DE LA PLATA ESTUARY<\/strong><br \/>\n<em>Alicia Ronco, Leticia Peluso, Mara Jurado, Gustavo Bulus Rossini and Alfredo Salibian<\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-5 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000100005&amp;lng=es&amp;nrm=iso&amp;tlng=en\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:40px;margin-bottom:40px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><a href=\"http:\/\/sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-2.png\"><img decoding=\"async\" class=\"alignnone size-full wp-image-251\" src=\"http:\/\/sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-2.png\" alt=\"LAJSBA_15-2\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-2-66x66.png 66w, https:\/\/www.sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-2-150x150.png 150w, https:\/\/www.sedimentologia.org.ar\/spa\/wp-content\/uploads\/2015\/05\/LAJSBA_15-2.png 300w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n<h2 style=\"text-align: left;\"><strong>Volumen 15 &#8211; N\u00famero 2 <\/strong>| Diciembre 2008<\/h2>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:-15px;margin-bottom:5px;width:100%;\"><div class=\"fusion-separator-border sep-single sep-solid\" style=\"--awb-height:20px;--awb-amount:20px;border-color:#e0dede;border-top-width:1px;\"><\/div><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><em><strong>Editor:<\/strong> Gerardo M. E. Perillo <\/em>| <em>70 p\u00e1ginas<\/em><\/p>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:0px;margin-bottom:20px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<div class=\"fusion-clearfix\"><\/div><\/div><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-3 fusion_builder_column_1_1 1_1 fusion-one-full fusion-column-first fusion-column-last fusion-column-no-min-height\" style=\"--awb-bg-size:cover;--awb-margin-bottom:0px;\"><div class=\"fusion-column-wrapper fusion-flex-column-wrapper-legacy\"><div class=\"fusion-title title fusion-title-2 fusion-title-text fusion-title-size-three\"><h3 class=\"fusion-title-heading title-heading-left\" style=\"margin:0;\">CONTENIDO<\/h3><span class=\"awb-title-spacer\"><\/span><div class=\"title-sep-container\"><div class=\"title-sep sep-single sep-solid\" style=\"border-color:#e0dede;\"><\/div><\/div><\/div>\n<p><strong>BASALTIC EXPLOSIVE VOLCANISM IN A TUFF-DOMINATED INTRAPLATE SETTING, SARMIENTO FORMATION (MIDDLE EOCENE- LOWER MIOCENE), PATAGONIA ARGENTINA<br \/>\n<\/strong><em>J. M. Paredes, F. Colombo, N. Foix, J. O. Allard, A. Nillini and M. Allo <\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-6 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000200001&amp;lng=es&amp;nrm=iso&amp;tlng=en\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><strong>RASGOS GEOQU\u00cdMICOS DE LAS CALIZAS DE LA FORMACION ARROYO VERDE (EOCENO), EN PUNTA COLORADA. PROVINCIA DE R\u00cdO NEGRO. ARGENTINA. RECONSTRUCCION PALEOAMBIENTAL<\/strong><br \/>\n<em>L. Luna, R. Schillizzi y R. Bonuccelli<\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-7 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000200002&amp;lng=es&amp;nrm=iso&amp;tlng=es\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><strong>LAS SECUENCIAS DEPOSITACIONALES DEL PLIOCENO-CUATERNARIO EN LA PLATAFORMA SUBMARINA ADYACENTE AL LITORAL DEL ESTE BONAERENSE<\/strong><br \/>\n<em>G. Parker, R. A. Violante, C. M. Paterlini, I. P. Costa, S. I. Marcolini y J. L. Cavallotto <\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-8 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000200003&amp;lng=es&amp;nrm=iso&amp;tlng=es\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div>\n<p><strong>GRAIN SIZE ANALYSIS AND CLAY MINERAL ASSOCIATIONS IN BOTTOM SEDIMENTS FROM PARANA RIVER BASIN<\/strong><br \/>\n<em>M. Manassero, C. Camili\u00f3n, D. Poir\u00e9, M. Da Silva and A. Ronco<\/em><\/p>\n<div class=\"fusion-alignleft\"><a class=\"fusion-button button-flat button-small button-custom fusion-button-default button-9 fusion-button-default-span \" style=\"--button_accent_color:#81d742;--button_accent_hover_color:#ffffff;--button_border_hover_color:#ffffff;--button_border_width-top:1px;--button_border_width-right:1px;--button_border_width-bottom:1px;--button_border_width-left:1px;--button-border-radius-top-left:0px;--button-border-radius-top-right:0px;--button-border-radius-bottom-right:0px;--button-border-radius-bottom-left:0px;--button_gradient_top_color:#ffffff;--button_gradient_bottom_color:#ffffff;--button_gradient_top_color_hover:#006253;--button_gradient_bottom_color_hover:#006253;\" target=\"_blank\" rel=\"noopener noreferrer\" href=\"http:\/\/www.scielo.org.ar\/scielo.php?script=sci_arttext&amp;pid=S1851-49792008000200004&amp;lng=es&amp;nrm=iso&amp;tlng=en\"><span class=\"fusion-button-text\">VER EN SCIELO<\/span><\/a><\/div>\n<div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-separator fusion-full-width-sep\" style=\"margin-left: auto;margin-right: auto;margin-top:10px;margin-bottom:25px;width:100%;\"><\/div><div class=\"fusion-sep-clear\"><\/div><div class=\"fusion-clearfix\"><\/div><\/div><\/div><\/div><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Volumen 15 &#8211; N\u00famero 1 | Julio 2008<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":35,"menu_order":25,"comment_status":"open","ping_status":"open","template":"side-navigation.php","meta":{"footnotes":""},"class_list":["post-185","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/pages\/185","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/comments?post=185"}],"version-history":[{"count":12,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/pages\/185\/revisions"}],"predecessor-version":[{"id":1418,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/pages\/185\/revisions\/1418"}],"up":[{"embeddable":true,"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/pages\/35"}],"wp:attachment":[{"href":"https:\/\/www.sedimentologia.org.ar\/spa\/wp-json\/wp\/v2\/media?parent=185"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}