Saptarshi Dey
Datos Biográficos
| ID | 11136574 |
|---|---|
| NOMBRE | Saptarshi Dey |
| NOMBRES | Saptarshi |
| APELLIDO | Dey |
| FIRMA | DEY S |
| AFILIACIONES | Indian Institute of Technology Gandhinagar |
| ORCID | 0000-0002-4627-4280 |
| VERIFICADO | No |
| TOTAL DE OBRAS | 1 |
| TOTAL DE CITAS | 0 |
| OBRAS COMO AUTOR | 1 |
| OBRAS COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 2023 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2023 |
| ÍNDICE H | 0 |
Dominant role of deglaciation in Late Pleistocene–Early Holocene sediment aggradation in the Upper Chenab valley, NW Himalaya
Sediment transfer from the interiors of the Himalaya is complex because the archives are influenced by both glacial and monsoonal cycles. To deconvolve the coupling of glacial and monsoonal effects on sediment transfer processes, we investigate the Late Pleistocene–Holocene sediment archive in the Upper Chenab valley. Optically stimulated luminescence (OSL) ages from the archive indicate major aggradation during ca. 20–10 ka. Isotopic fingerprint…
Sin obras prominentes en esta página.
Dominant role of deglaciation in Late Pleistocene–Early Holocene sediment aggradation in the Upper Chenab valley, NW Himalaya
Sediment transfer from the interiors of the Himalaya is complex because the archives are influenced by both glacial and monsoonal cycles. To deconvolve the coupling of glacial and monsoonal effects on sediment transfer processes, we investigate the Late Pleistocene–Holocene sediment archive in the Upper Chenab valley. Optically stimulated luminescence (OSL) ages from the archive indicate major aggradation during ca. 20–10 ka. Isotopic fingerprint…
Aggradation (1 obra) · Cryospheric studies and observations (1 obra) · Deglaciation (1 obra) · Fluvial (1 obra) · Geochemistry (1 obra) · Geological formations and processes (1 obra) · Geology (1 obra) · Geology and Paleoclimatology Research (1 obra) · Geomorphology (1 obra) · Glacial period (1 obra)