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Volumn 112, Issue 1-2, 2009, Pages 48-66

Combined use of relative and absolute dating techniques for detecting signals of Alpine landscape evolution during the late Pleistocene and early Holocene

Author keywords

10Be; 14C; Clay minerals; Deglaciation; Soil organic matter; Weathering

Indexed keywords

AGE DETERMINATION; ALPINE ENVIRONMENT; BERYLLIUM ISOTOPE; CARBON ISOTOPE; CLAY MINERAL; DEGLACIATION; DETECTION METHOD; GEOCHRONOLOGY; HOLOCENE; LANDSCAPE EVOLUTION; MASS BALANCE; PLEISTOCENE; PODZOLIZATION; RADIOCARBON DATING; SIGNAL; SOIL ORGANIC MATTER; WEATHERING RATE;

EID: 69749097395     PISSN: 0169555X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.geomorph.2009.05.003     Document Type: Article
Times cited : (41)

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