Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas
Analyses carried out on bedded limestone-marl couplets from Castro Island section (latest Coniacian-lower Santonian, Basque-Cantabrian Basin) show clear isotopic (a'780 and al3C) and mineralógica! differences between limestones and marls. Analytical results point out that the sediments suff...
| Authors: | , , |
|---|---|
| Format: | article |
| Publication Date: | 2002 |
| Country: | España |
| Institution: | Universidad de Huelva (UHU) |
| Repository: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Language: | Spanish |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/9353 |
| Online Access: | http://hdl.handle.net/10272/9353 |
| Access Level: | Open access |
| Keyword: | Limestone-marl couplets Stables isotopes Clay mineralogy Climatic variations Coniacian-Santonian Basque-Cantabrian Basin |
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Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicasLimestone-marl couplets from Castro Island (latest Coniacian-lower Santonian, Basque-Cantabriarr Basin): isotopic (ä180 and ä13C) and mineralógical variationsJiménez Berrocoso, A.Zuluaga, María CruzElorza, JavierLimestone-marl coupletsStables isotopesClay mineralogyClimatic variationsConiacian-SantonianBasque-Cantabrian BasinAnalyses carried out on bedded limestone-marl couplets from Castro Island section (latest Coniacian-lower Santonian, Basque-Cantabrian Basin) show clear isotopic (a'780 and al3C) and mineralógica! differences between limestones and marls. Analytical results point out that the sediments suffered a low diagenetic grade, and imply a synsedimentary origin for the limestone-marl couplets. Besides, it is suggested that the deposition of the sediments was influenced by changes in the carbonate production and continental influx strength into the shallow water basin, probably, as a consequence of climatic variations, which could range between wet and dry conditionsSociedad Geológica de España20022002-01-0120022002-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/9353reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/93532026-06-02T14:58:11Z |
| dc.title.none.fl_str_mv |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas Limestone-marl couplets from Castro Island (latest Coniacian-lower Santonian, Basque-Cantabriarr Basin): isotopic (ä180 and ä13C) and mineralógical variations |
| title |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas |
| spellingShingle |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas Jiménez Berrocoso, A. Limestone-marl couplets Stables isotopes Clay mineralogy Climatic variations Coniacian-Santonian Basque-Cantabrian Basin |
| title_short |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas |
| title_full |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas |
| title_fullStr |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas |
| title_full_unstemmed |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas |
| title_sort |
Los pares caliza-marga de la Isla de Castro (Coniaciense final-Santoniense inferior, Cuenca Vasco-Cantábrica): variaciones isotópicas (á!80 y á13C) y mineralógicas |
| dc.creator.none.fl_str_mv |
Jiménez Berrocoso, A. Zuluaga, María Cruz Elorza, Javier |
| author |
Jiménez Berrocoso, A. |
| author_facet |
Jiménez Berrocoso, A. Zuluaga, María Cruz Elorza, Javier |
| author_role |
author |
| author2 |
Zuluaga, María Cruz Elorza, Javier |
| author2_role |
author author |
| dc.contributor.none.fl_str_mv |
|
| dc.subject.none.fl_str_mv |
Limestone-marl couplets Stables isotopes Clay mineralogy Climatic variations Coniacian-Santonian Basque-Cantabrian Basin |
| topic |
Limestone-marl couplets Stables isotopes Clay mineralogy Climatic variations Coniacian-Santonian Basque-Cantabrian Basin |
| description |
Analyses carried out on bedded limestone-marl couplets from Castro Island section (latest Coniacian-lower Santonian, Basque-Cantabrian Basin) show clear isotopic (a'780 and al3C) and mineralógica! differences between limestones and marls. Analytical results point out that the sediments suffered a low diagenetic grade, and imply a synsedimentary origin for the limestone-marl couplets. Besides, it is suggested that the deposition of the sediments was influenced by changes in the carbonate production and continental influx strength into the shallow water basin, probably, as a consequence of climatic variations, which could range between wet and dry conditions |
| publishDate |
2002 |
| dc.date.none.fl_str_mv |
2002 2002-01-01 2002 2002-01-01 |
| dc.type.none.fl_str_mv |
journal article http://purl.org/coar/resource_type/c_6501 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10272/9353 |
| url |
http://hdl.handle.net/10272/9353 |
| dc.language.none.fl_str_mv |
Español spa |
| language_invalid_str_mv |
Español |
| language |
spa |
| dc.rights.none.fl_str_mv |
open access http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
| dc.rights.openaire.fl_str_mv |
info:eu-repo/semantics/openAccess |
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open access http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 3.0 España http://creativecommons.org/licenses/by-nc-nd/3.0/es/ |
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openAccess |
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application/pdf |
| dc.publisher.none.fl_str_mv |
Sociedad Geológica de España |
| publisher.none.fl_str_mv |
Sociedad Geológica de España |
| dc.source.none.fl_str_mv |
reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva instname:Universidad de Huelva (UHU) |
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Universidad de Huelva (UHU) |
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Arias Montano. Repositorio Institucional de la Universidad de Huelva |
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Arias Montano. Repositorio Institucional de la Universidad de Huelva |
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15,81155 |