Shangzhe Zhou
Datos Biográficos
| ID | 3818474 |
|---|---|
| NOMBRE | Shangzhe Zhou |
| NOMBRES | Shangzhe |
| APELLIDO | Zhou |
| FIRMA | ZHOU S |
| AFILIACIONES | South China Normal University |
| ORCID | 0000-0002-6416-4528 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 11 |
| TOTAL DE CITAS | 3 |
| TOTAL COMO AUTOR | 11 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1991 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2016 |
| ÍNDICE H | 1 |
Glacial geomorphology of the Parlung Zangbo Valley, southeastern Tibetan Plateau
We present a glacial geomorphological map (1:825,000) of the Parlung Zangbo Valley in the southeastern Tibetan Plateau based on Google Earth imagery and the 30 m ASTER Global Digital Elevation Model (ASTER GDEM). The mapped region covers 2.9 × 10 4 km 2 , including abundant glacial landforms such as glacial valleys, marginal moraines (including terminal moraines and lateral moraines), and hummocky moraines. Glacial valleys are distributed mainly …
Optical dating of young glacial sediments from the source area of the Urumqi River in Tianshan Mountians, northwestern China
Late Quaternary fluvial terraces near the Daocheng Ice Cap, eastern Tibetan Plateau
The timing of terrace formation relative to the glacial–interglacial cycle and what factors control that timing, such as changes in climate and/or uplift, are controversial. Here we present a study of the terraces along the Yazheku River using electron spin resonance (ESR) dating and analysis of the sedimentary characteristics in order to establish the timing of terrace formation and to assess the forcing mechanisms that have been proposed. The Y…
A visionary geomorphologist and glaciologist
Timing of glacier fluctuations and trigger mechanisms in eastern Qinghai–Tibetan Plateau during the late Quaternary
It is highly debated whether glacial advances on the Qinghai–Tibetan Plateau (QTP) occurred as a response to temperature cooling, or whether they were forced by an increase in moisture brought by the intensive Indian summer monsoon. We here report a case study investigating this issue. Multiple moraine series in the Yingpu Valley, Queer Shan ranges of the Hengduan Mountains, and eastern QTP, provide an excellent archive for examining the timing a…
Quaternary glaciations-extent and chronology in Tibetan plateau
A preliminary study on timing of the oldest Pleistocene glaciation in Qinghai–Tibetan Plateau
ESR dating of glacial tills and glaciations in the Urumqi River headwaters, Tianshan Mountains, China
Quaternary glaciation of the Bailang River Valley, Qilian Shan
The sequence of Quaternary glaciation in the Bayan Har Mountains
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
The sequence of Quaternary glaciation in the Bayan Har Mountains
Quaternary glaciation of the Bailang River Valley, Qilian Shan
A preliminary study on timing of the oldest Pleistocene glaciation in Qinghai–Tibetan Plateau
ESR dating of glacial tills and glaciations in the Urumqi River headwaters, Tianshan Mountains, China
Quaternary glaciations-extent and chronology in Tibetan plateau
Late Quaternary fluvial terraces near the Daocheng Ice Cap, eastern Tibetan Plateau
The timing of terrace formation relative to the glacial–interglacial cycle and what factors control that timing, such as changes in climate and/or uplift, are controversial. Here we present a study of the terraces along the Yazheku River using electron spin resonance (ESR) dating and analysis of the sedimentary characteristics in order to establish the timing of terrace formation and to assess the forcing mechanisms that have been proposed. The Y…
A visionary geomorphologist and glaciologist
Timing of glacier fluctuations and trigger mechanisms in eastern Qinghai–Tibetan Plateau during the late Quaternary
It is highly debated whether glacial advances on the Qinghai–Tibetan Plateau (QTP) occurred as a response to temperature cooling, or whether they were forced by an increase in moisture brought by the intensive Indian summer monsoon. We here report a case study investigating this issue. Multiple moraine series in the Yingpu Valley, Queer Shan ranges of the Hengduan Mountains, and eastern QTP, provide an excellent archive for examining the timing a…
Optical dating of young glacial sediments from the source area of the Urumqi River in Tianshan Mountians, northwestern China
Glacial geomorphology of the Parlung Zangbo Valley, southeastern Tibetan Plateau
We present a glacial geomorphological map (1:825,000) of the Parlung Zangbo Valley in the southeastern Tibetan Plateau based on Google Earth imagery and the 30 m ASTER Global Digital Elevation Model (ASTER GDEM). The mapped region covers 2.9 × 10 4 km 2 , including abundant glacial landforms such as glacial valleys, marginal moraines (including terminal moraines and lateral moraines), and hummocky moraines. Glacial valleys are distributed mainly …
Geology and Paleoclimatology Research (11 obras) · Geology (8 obras) · Geomorphology (8 obras) · Glacial period (8 obras) · Geography (7 obras) · Glacier (6 obras) · Moraine (6 obras) · Paleontology (6 obras) · Physical geography (6 obras) · Quaternary (5 obras)