Holocene evolution and geochronology of a semiarid fluvial system in the western slope of the Central Andes
AMS 14C data in El Tránsito River Valley, Northern Chile
Bibliographic Data
| ID | 14976248 |
|---|---|
| Authors | Albert Cabré Cano, Germán Aguilar Martorell (0000-0002-3926-835X), Rodrigo Riquelme Salazar |
| Year | 2017 |
| Volume | 438 |
| Pages | 20-32 |
| Publication date | 2017-05-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Quaternary International (JOURNAL) |
| Journal identifiers | ISSN: 1040-6182 • E-ISSN: 1873-4553 |
| Publisher | Elsevier BV (PUBLISHER) |
| DOI | 10.1016/j.quaint.2017.04.030 |
| OpenAlex | W2610530955 |
| Language | EN |
| Citations received | 1 |
| References cited | 38 |
Aggradation · Alluvial fan · Alluvium · Fluvial · Geomorphology · Glacial period · Glacier · Holocene · Landslide · Moraine · Physical geography · Structural basin · Surface exposure dating · Tributary · Geological formations and processes · Geology and Paleoclimatology Research · Landslides and related hazards · Geology · Paleontology
Quaternary of Chile
Paleowetlands and regional climate change in the central Atacama Desert, northern chile
Late Pleistocene–early Holocene paraglacial and fluvial sediment history in the Turbio valley, semiarid Chilean Andes
Paraglacial geomorphology
Geological Observations on the Volcanic Islands and Parts of South America visited during the Voyage of HMS “Beagle”
Frequency of debris flows and rockfall along the Mendoza river valley (Central Andes), Argentina
Late Quaternary glacier advances and palaeolake highstands in the Bolivian Altiplano
Recent catastrophic debris flows in Chile
A late-Holocene (<2600 BP) glacial advance in the south-central Andes (29°S), northern Chile
Accurate Dating of Organic Deposits by AMS 14 C Measurement of Macrofossils
Extended 14 C Data Base and Revised Calib 3.0 14 C Age Calibration Program
INTCAL98 Radiocarbon Age Calibration, 24,000-0 cal BP
| Citations per year | 1 |
|---|---|
| Citation span | 2025 - 2025 (1) |
| Highly cited | No |