Zhijiu Cui
Biographic Data
| ID | 6372865 |
|---|---|
| NAME | Zhijiu Cui |
| GIVEN NAMES | Zhijiu |
| FAMILY NAME | Cui |
| SIGNATURE | CUI Z |
| AFFILIATIONS | Peking University |
| VERIFIED | No |
| TOTAL WORKS | 9 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 9 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2002 |
| LATEST PUBLICATION YEAR | 2020 |
| H-INDEX | 0 |
Susceptibility Assessments and Validations of Debris-Flow Events in Meizoseismal Areas
The 2008 Wenchuan earthquake triggered tens of thousands of landslides, resulting in rich loose materials for the 8.13 debris flows. Longchi Town in southwest China’s Sichuan Province was one of the worst hit areas both by the Wenchuan earthquake and 8.13 debris flows. The loose source materials generated by coseismic landslides in the Longxi River watershed of the upper Min River are widely distributed and cover an area of 7.97 km2. The volume h…
Using 10 Be exposure dating to constrain glacial advances during the late glacial and Holocene on Mount Xuebaoding, eastern Tibetan Plateau
Moraines preserved around Mount Xuebaoding (5588 m above sea level) on the eastern margin of the Tibetan Plateau, represent past glacial activity in this area. The chronology of these moraines was established using 10 Be exposure dating. The dating results revealed multiple glacial events prior to the late glacial ( > 14.1±2.2 ka), the late glacial (15.6±1.6 to 11.2±3.0 ka), the early-middle Holocene (9.1±0.9 to 6.7±0.7 ka), and the Neoglacial pe…
Sedimentary evidence of outburst deposits induced by the Diexi paleolandslide-dammed lake of the upper Minjiang River in China
Holocene landslide-dammed lake deposits in the Upper Jinsha River, SE Tibetan Plateau and their ages
Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau
The Diancang Massif is located in a region linking the Tibetan and Yungui Plateaus. Climatically, it is in a transition belt between the south and middle subtropical zones, controlled by Indian monsoon and westerlies. Thus, this study provides more evidences on the evolution of Indian monsoon since the Holocene. We reconstruct the history of climate on the Diancang Massif since 11.5 ka, using integrated correlation of glacial activities, early hu…
Late Pleistocene glaciation of the Diancang and Gongwang Mountains, southeast margin of the Tibetan plateau
A review of glacial sequences of the Kunlun Pass, northern Tibetan Plateau
AMS radiocarbon dating of late Quaternary glacial landforms, source of the Urumqi River, Tien Shan—a pilot study of 14C dating on inorganic carbon
The Quaternary glaciation of Shesan Mountain in Taiwan and glacial classification in monsoon areas
No prominent works on this page.
The Quaternary glaciation of Shesan Mountain in Taiwan and glacial classification in monsoon areas
AMS radiocarbon dating of late Quaternary glacial landforms, source of the Urumqi River, Tien Shan—a pilot study of 14C dating on inorganic carbon
Late Pleistocene glaciation of the Diancang and Gongwang Mountains, southeast margin of the Tibetan plateau
A review of glacial sequences of the Kunlun Pass, northern Tibetan Plateau
Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau
The Diancang Massif is located in a region linking the Tibetan and Yungui Plateaus. Climatically, it is in a transition belt between the south and middle subtropical zones, controlled by Indian monsoon and westerlies. Thus, this study provides more evidences on the evolution of Indian monsoon since the Holocene. We reconstruct the history of climate on the Diancang Massif since 11.5 ka, using integrated correlation of glacial activities, early hu…
Holocene landslide-dammed lake deposits in the Upper Jinsha River, SE Tibetan Plateau and their ages
Using 10 Be exposure dating to constrain glacial advances during the late glacial and Holocene on Mount Xuebaoding, eastern Tibetan Plateau
Moraines preserved around Mount Xuebaoding (5588 m above sea level) on the eastern margin of the Tibetan Plateau, represent past glacial activity in this area. The chronology of these moraines was established using 10 Be exposure dating. The dating results revealed multiple glacial events prior to the late glacial ( > 14.1±2.2 ka), the late glacial (15.6±1.6 to 11.2±3.0 ka), the early-middle Holocene (9.1±0.9 to 6.7±0.7 ka), and the Neoglacial pe…
Sedimentary evidence of outburst deposits induced by the Diexi paleolandslide-dammed lake of the upper Minjiang River in China
Susceptibility Assessments and Validations of Debris-Flow Events in Meizoseismal Areas
The 2008 Wenchuan earthquake triggered tens of thousands of landslides, resulting in rich loose materials for the 8.13 debris flows. Longchi Town in southwest China’s Sichuan Province was one of the worst hit areas both by the Wenchuan earthquake and 8.13 debris flows. The loose source materials generated by coseismic landslides in the Longxi River watershed of the upper Min River are widely distributed and cover an area of 7.97 km2. The volume h…
Geography (7 works) · Geology (7 works) · Geology and Paleoclimatology Research (7 works) · Geomorphology (6 works) · Glacial period (6 works) · Physical geography (6 works) · Paleontology (5 works) · Pleistocene-Era Hominins and Archaeology (5 works) · Geological formations and processes (4 works) · Glacier (4 works)