Mingjian Liang
Biographic Data
| ID | 7511378 |
|---|---|
| NAME | Mingjian Liang |
| GIVEN NAMES | Mingjian |
| FAMILY NAME | Liang |
| SIGNATURE | LIANG M |
| ORCID | 0000-0001-5527-7136 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2014 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
Geomorphological and geological characteristics reflecting the Holocene activity of the Dalangsonggou fault, eastern Tibetan Plateau
Characteristics of stress field and crustal kinematics of the southern region of Sichuan-Yunnan block, southern Tibet Plateau
The Red River fault is a massive tectonic shear zone of the Sichuan-Yunnan block, southern Tibet Plateau. The target area of this study is the Red River fault's middle-northern section and adjacent areas. Considering the spatial difference of tectonic structures and the inhomogeneity of focal mechanism solutions, we divided the target area into three structural units: the northern extension area, the middle strike-slip movement area, and the west…
Late Quaternary fault activity and deformation mechanism in the eastern Tibet Plateau (Dari fault, Bayan Har Block)
The Dari fault is one of several large NW-trending left-lateral strike-slip faults with Holocene activity inside the Bayan Har Block in the east of the Tibetan Plateau. Through interpretation of high-resolution images, field investigations, and trench excavations, we estimated that the average horizontal slip rate has been 2.6 ± 0.6 mm/y since the late Quaternary. We also identified three earthquake events dated to 15,609–12,658 cal BP, 6741–5074…
Determination of mean recurrence interval of large earthquakes on the Garzê-Yushu Fault (Dengke Segment) on the eastern margin of the Qinghai–Tibetan Plateau
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Determination of mean recurrence interval of large earthquakes on the Garzê-Yushu Fault (Dengke Segment) on the eastern margin of the Qinghai–Tibetan Plateau
Characteristics of stress field and crustal kinematics of the southern region of Sichuan-Yunnan block, southern Tibet Plateau
The Red River fault is a massive tectonic shear zone of the Sichuan-Yunnan block, southern Tibet Plateau. The target area of this study is the Red River fault's middle-northern section and adjacent areas. Considering the spatial difference of tectonic structures and the inhomogeneity of focal mechanism solutions, we divided the target area into three structural units: the northern extension area, the middle strike-slip movement area, and the west…
Late Quaternary fault activity and deformation mechanism in the eastern Tibet Plateau (Dari fault, Bayan Har Block)
The Dari fault is one of several large NW-trending left-lateral strike-slip faults with Holocene activity inside the Bayan Har Block in the east of the Tibetan Plateau. Through interpretation of high-resolution images, field investigations, and trench excavations, we estimated that the average horizontal slip rate has been 2.6 ± 0.6 mm/y since the late Quaternary. We also identified three earthquake events dated to 15,609–12,658 cal BP, 6741–5074…
Geomorphological and geological characteristics reflecting the Holocene activity of the Dalangsonggou fault, eastern Tibetan Plateau
earthquake and tectonic studies (4 works) · Fault (geology (4 works) · Geology (4 works) · Plateau (mathematics (4 works) · Seismology (4 works) · Tectonics (4 works) · Active fault (3 works) · Geological and Geochemical Analysis (3 works) · Paleontology (3 works) · Block (permutation group theory (2 works)