Evolución geomorfológica del karst y paleoambientes cuaternarios en el macizo de Patones-Cerro de la Oliva (Madrid)
Loading...
Publication date
Advisors
Department
Research group
Center
Metrics
Export
Abstract
Geomorphological, sedimentological and palaeontological evidences allowed to identify several phases in the evolution of the Patones-Cerro c/e la Oliva karstic massif. The studied speleothems, jointly with data of previous works indicate the presence of at least five episodes of chemical precipitation under favorable climatic conditions during isotopic stages 9-11?, 7, 5, 4-3 and 7, respectively
Keywords
Unesco Subjects
Bibliographic citation
Collections
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España