Por favor, use este identificador para citar o enlazar a este item:
http://hdl.handle.net/10261/31655
COMPARTIR / EXPORTAR:
SHARE CORE BASE | |
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE | |
Título: | Geological factors influencing the concentration of trace elements in the Philippi peatland, eastern Macedonia, Greece |
Autor: | Christanis, K.; Georgakopoulos, Andreas; Fernandez-Turiel, J. L. CSIC ORCID ; Bouzinos, A. | Palabras clave: | Peat Trace elements Philippi fen Holocene Upper Pleistocene Greece |
Fecha de publicación: | jun-1998 | Editor: | Elsevier | Citación: | International Journal of Coal Geology 36(3-4): 295-313 (1998) | Resumen: | Six peat samples obtained from the Holocene and the Weichselian of the Philippi peat deposit, eastern Macedonia, Greece, were analyzed for 48 trace elements by Inductively Coupled Plasma–Mass Spectrometry (ICP–MS). The ash contents of these samples were also determined. Most of the trace elements are associated with the minerals in the peat, while Ge, Mo, Pb, Se, Ta, Tl, U, and W display a greater affinity with the organic matter. Compared with crustal averages (Clarke concentrations), the Philippi peat is enriched in some elements (Ag, As, Au, Cd, Mo, Se, Te, U, and W) because of the respective mineralizations in the area. The Philippi peat is also enriched in Cr, Cu, Mo, Pb, Sc, Sn, T, V, Y, and Zn in comparison with typical fen peats, as well as in As, Cr, Mo, Se, and U in comparison with typical coals. Climatic and hydrogeological conditions strongly influenced the peat-forming environment resulting in a differentiation between Holocene and Weichselian peat. Generally, the Holocene peat contains lower concentrations of trace elements in the northern and southern part of the fen, than the Weichselian one. The opposite trend is observed in the fen area close to the western basin margins. | Descripción: | 17 páginas, 4 figuras, 5 tablas. | Versión del editor: | http://dx.doi.org/10.1016/S0166-5162(98)00004-4 | URI: | http://hdl.handle.net/10261/31655 | DOI: | 10.1016/S0166-5162(98)00004-4 | ISSN: | 0166-5162 |
Aparece en las colecciones: | (Geo3Bcn) Artículos |
Mostrar el registro completo
CORE Recommender
SCOPUSTM
Citations
55
checked on 21-abr-2024
WEB OF SCIENCETM
Citations
51
checked on 23-feb-2024
Page view(s)
376
checked on 24-abr-2024
Google ScholarTM
Check
Altmetric
Altmetric
NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.