Haibing Li
Biographic Data
| ID | 6379156 |
|---|---|
| NAME | Haibing Li |
| GIVEN NAMES | Haibing |
| FAMILY NAME | Li |
| SIGNATURE | LI H |
| AFFILIATIONS | Ministry of Natural Resources |
| ORCID | 0000-0001-8110-0545 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2011 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
Mid-Pleistocene drainage rearrangement of the Dadu River in response to plate convergence in southeastern Tibet
The rearrangement of drainage basins provides critical insight into crustal deformation and geodynamic mechanisms. Near the southeastern boundary of the Tibetan Plateau, the Dadu River abruptly shifts from south- to east-flowing, providing important implications for regional tectonogeomorphic development since the mid-Pleistocene. South of the bend, the headwaters of the Anning River occupy an unusually wide valley. Field investigations show that…
A continuous 18-10.2 ka paleo-earthquake events revealed by the Luobozhai lacustrine sediments, eastern Tibetan Plateau
Geochemical features of the pseudotachylytes in the Longmen Shan thrust belt, eastern Tibet
Tectonic uplift and landslides triggered by the Wenchuan earthquake and constraints on orogenic growth
Magnetostratigraphy of sediments from the Yumu Shan, Hexi Corridor and its implications regarding the Late Cenozoic uplift of the NE Tibetan Plateau
No prominent works on this page.
Magnetostratigraphy of sediments from the Yumu Shan, Hexi Corridor and its implications regarding the Late Cenozoic uplift of the NE Tibetan Plateau
Tectonic uplift and landslides triggered by the Wenchuan earthquake and constraints on orogenic growth
Geochemical features of the pseudotachylytes in the Longmen Shan thrust belt, eastern Tibet
Mid-Pleistocene drainage rearrangement of the Dadu River in response to plate convergence in southeastern Tibet
The rearrangement of drainage basins provides critical insight into crustal deformation and geodynamic mechanisms. Near the southeastern boundary of the Tibetan Plateau, the Dadu River abruptly shifts from south- to east-flowing, providing important implications for regional tectonogeomorphic development since the mid-Pleistocene. South of the bend, the headwaters of the Anning River occupy an unusually wide valley. Field investigations show that…
A continuous 18-10.2 ka paleo-earthquake events revealed by the Luobozhai lacustrine sediments, eastern Tibetan Plateau
earthquake and tectonic studies (4 works) · Geology (4 works) · Geomorphology (4 works) · Geological and Geochemical Analysis (3 works) · Geology and Paleoclimatology Research (3 works) · Structural basin (3 works) · Debris (2 works) · Geochemistry (2 works) · Oceanography (2 works) · Plateau (mathematics (2 works)