Shao-Peng Gao
Biographic Data
| ID | 11047138 |
|---|---|
| NAME | Shao-Peng Gao |
| GIVEN NAMES | Shao-Peng |
| FAMILY NAME | Gao |
| SIGNATURE | GAO S |
| AFFILIATIONS | Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, China |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 4 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2016 |
| LATEST PUBLICATION YEAR | 2016 |
| H-INDEX | 1 |
Identification of a late Quaternary alluvial–aeolian sedimentary sequence in the Sichuan Basin, China
The late Quaternary sedimentary sequence in the northwestern part of the Sichuan Basin consists of five lithological units and with increasing depth include the: Chengdu Clay; Brown Clay; Red Clay; Sandy Silt; and basal Muddy Gravel. The genesis, provenance and age of the sediments, as well as the possible presence of hiatuses within this sequence are debated. Measurements of grain-size, magnetic susceptibility, quartz content, quartz δ 18 O valu…
Potential forcing mechanisms of Holocene lake-level changes at Nam Co, Tibetan Plateau
The timing of lake-level fluctuations on the Tibetan Plateau and their relationship with climatic changes is still under debate, and the main reason for this is the lack of suitable archives for reconstructing the paleohydrology and paleoclimatology of the lakes. Here, we present the results of analyses of the shell geochemistry of Radix sp. from an exposed terrace of Nam Co lake on the south-central Tibetan Plateau. Optically stimulated luminesc…
Potential forcing mechanisms of Holocene lake-level changes at Nam Co, Tibetan Plateau
The timing of lake-level fluctuations on the Tibetan Plateau and their relationship with climatic changes is still under debate, and the main reason for this is the lack of suitable archives for reconstructing the paleohydrology and paleoclimatology of the lakes. Here, we present the results of analyses of the shell geochemistry of Radix sp. from an exposed terrace of Nam Co lake on the south-central Tibetan Plateau. Optically stimulated luminesc…
Identification of a late Quaternary alluvial–aeolian sedimentary sequence in the Sichuan Basin, China
The late Quaternary sedimentary sequence in the northwestern part of the Sichuan Basin consists of five lithological units and with increasing depth include the: Chengdu Clay; Brown Clay; Red Clay; Sandy Silt; and basal Muddy Gravel. The genesis, provenance and age of the sediments, as well as the possible presence of hiatuses within this sequence are debated. Measurements of grain-size, magnetic susceptibility, quartz content, quartz δ 18 O valu…
Potential forcing mechanisms of Holocene lake-level changes at Nam Co, Tibetan Plateau
The timing of lake-level fluctuations on the Tibetan Plateau and their relationship with climatic changes is still under debate, and the main reason for this is the lack of suitable archives for reconstructing the paleohydrology and paleoclimatology of the lakes. Here, we present the results of analyses of the shell geochemistry of Radix sp. from an exposed terrace of Nam Co lake on the south-central Tibetan Plateau. Optically stimulated luminesc…
Geological formations and processes (2 works) · Geology and Paleoclimatology Research (2 works) · Aeolian processes (1 work) · Alluvial fan (1 work) · Alluvium (1 work) · Clastic rock (1 work) · Climate change (1 work) · Climatology (1 work) · East Asian Monsoon (1 work) · Forcing (mathematics (1 work)