Pleistocene Climate Change in Central Europe

Loess is terrestrial, clastic sediment formed by the accumulation of wind-blown dust. It is usually inter–bedded with paleosol horizons, forming loess-paleosol successions (LPS). Due to their characteristics LPS’s represent valuable records of climate changes during Pleistocene. The thickest LPS sec...

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Detalles Bibliográficos

Autores principales:	Banak, Adriano, Mandic, Oleg, Pavelić, Davor, Kovačić, Marijan, Lirer, Fabrizio
Formato:	Capítulo de libro
Lenguaje:	inglés
Publicado:	IntechOpen 2020
Materias:	Social Sciences and Humanities
Acceso en línea:	https://www.intechopen.com/chapters/73350
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