Código QR (código de barras bidimensional)

Sub-Boreal aggradation along the Apennine margin of the Central Po Plain: geomorphological and geoarchaeological aspects

The Apennine foothills at the southern limit of the Po Plain consist of a belt of coalescent, gravelly, alluvial fans, trending to the north, towards the depocenter of the plain. Their aggradation is generally considered to have been controled by climate and linked to the glacial periods of the Midd...

ver descrição completa

Na minha lista:
Principais autores: Cremaschi, Mauro, Nicosia, Cristiano
Formato: Artigo
Idioma:Inglês
Publicado em: Groupe français de géomorphologie 2012
Assuntos:
Holocène
cônes alluviaux
géoarchéologie
géomorphologie fluviale
plaine du Pô
micromorphologie des sols
alluvial fans
Holocene
geoarchaeology
alluvial geomorphology
Po Plain
soil micromorphology
Acesso em linha:https://doi.org/10.4000/geomorphologie.9810
https://hdl.handle.net/20.500.13089/gipl
https://journals.openedition.org/geomorphologie/9810
Tags: Adicionar Tag
Sem tags, seja o primeiro a adicionar uma tag!

Registros relacionados