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The imprint of global climate cycles in the Fuentillejo maar-lake record during the last 50 ka cal BP (central Spain)
Cita
Ortiz Menéndez, José Eugenio 
ORCID: https://orcid.org/0000-0002-5699-2593, Torres Pérez-Hidalgo, Trinidad José ORCID: https://orcid.org/0000-0001-5260-4525, Vegas, Juana, Pardo-Iguzquiza, E, Galán, Luis, García Cortés, Luis Alberto, Ruiz Zapata, Maria Blanca and Gil García, MJ
(2014).
The imprint of global climate cycles in the Fuentillejo maar-lake record during the last 50 ka cal BP (central Spain).
En: "INTIMATE Open Workshop and COST Action ES0907 Final Event", 15/06/2014 - 21/06/2014, Zaragoza. p. 4.
ORCID: https://orcid.org/0000-0002-5699-2593, Torres Pérez-Hidalgo, Trinidad José ORCID: https://orcid.org/0000-0001-5260-4525, Vegas, Juana, Pardo-Iguzquiza, E, Galán, Luis, García Cortés, Luis Alberto, Ruiz Zapata, Maria Blanca and Gil García, MJ
(2014).
The imprint of global climate cycles in the Fuentillejo maar-lake record during the last 50 ka cal BP (central Spain).
En: "INTIMATE Open Workshop and COST Action ES0907 Final Event", 15/06/2014 - 21/06/2014, Zaragoza. p. 4.
Descripción
| Título: | The imprint of global climate cycles in the Fuentillejo maar-lake record during the last 50 ka cal BP (central Spain) |
|---|---|
| Autor/es: |
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| Tipo de Documento: | Ponencia en Congreso o Jornada (Otro) |
| Título del Evento: | INTIMATE Open Workshop and COST Action ES0907 Final Event |
| Fechas del Evento: | 15/06/2014 - 21/06/2014 |
| Lugar del Evento: | Zaragoza |
| Título del Libro: | INTIMATE Open Workshop and COST Action ES0907 Final Event |
| Fecha: | 2014 |
| Materias: | |
| ODS: | |
| Escuela: | E.T.S.I. de Minas y Energía (UPM) |
| Departamento: | Ingeniería Geológica y Minera |
| Licencias Creative Commons: | Reconocimiento - Sin obra derivada - No comercial |
Resumen
We have analysed the geochemical (element analysis), mineralogical and sedimentary facies to characterize the sedimentary record in Fuentillejo maar-lake in the central Spanish volcanic field of Campo de Calatrava and thus be able to reconstruct the cyclicity of the sedimentary and paleoclimatic processes involved. The upper 20 m of core FUENT-1 show variations in clastic input and water chemistry in the lake throughout the last 50 ka cal BP. Being a closed system, the water level in this maar-lake depends primarily on the balance between precipitation and evaporation
Más información
| ID de Registro: | 35113 |
|---|---|
| Identificador DC: | https://oa.upm.es/35113/ |
| Identificador OAI: | oai:oa.upm.es:35113 |
| Depositado por: | Memoria Investigacion |
| Depositado el: | 14 May 2015 06:48 |
| Ultima Modificación: | 14 May 2015 06:48 |
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