Uplift age and rates of the Gurvan Bogd system (Gobi-Altay) by apatite fission track analysis
The dating of the uplift onset of the Mongolian mountain ranges, the northernmost relief
associated with the India-Eurasia convergence, is a fundamental issue to better understand …
associated with the India-Eurasia convergence, is a fundamental issue to better understand …
Mongolian summits: an uplifted, flat, old but still preserved erosion surface
Abstract In Gobi Altay and Altay, Mongolia, several flat surfaces, worn through basement
rocks and uplifted during the ongoing tectonic episode to a similar altitude of 4000 m …
rocks and uplifted during the ongoing tectonic episode to a similar altitude of 4000 m …
Characterizing the present‐day activity of the Tunka and Sayan faults within their relay zone (western Baikal Rift System, Russia)
JF Ritz, A Arzhannikova, R Vassallo, S Arzhannikov… - …, 2018 - Wiley Online Library
Abstract The Sayan and Tunka faults are located at the boundary between the northernmost
mountain belt of Central Asia (the Sayan‐Baikal ranges) and the Siberian platform. These …
mountain belt of Central Asia (the Sayan‐Baikal ranges) and the Siberian platform. These …
Geologic inheritance and earthquake rupture processes: The 1905 M≥ 8 Tsetserleg‐Bulnay strike‐slip earthquake sequence, Mongolia
Abstract In 1905, 14 days apart, two M~ 8 continental strike‐slip earthquakes, the Tsetserleg
and Bulnay earthquakes, occurred on the Bulnay fault system, in Mongolia. Together, they …
and Bulnay earthquakes, occurred on the Bulnay fault system, in Mongolia. Together, they …
Late Pleistocene slip rate of the central Haiyuan fault constrained from optically stimulated luminescence, 14C, and cosmogenic isotope dating and high-resolution …
Y Shao, J Liu-Zeng, J Van der Woerd… - GSA …, 2021 - pubs.geoscienceworld.org
To better constrain the long-term millennial slip rate of the Haiyuan fault in its central part, we
revisited the site of Daqing, where there are multiple paired offset terraces. We used 0.1-m …
revisited the site of Daqing, where there are multiple paired offset terraces. We used 0.1-m …
Earthquake geology of the Bulnay fault (Mongolia)
Abstract The Bulnay earthquake of 23 July 1905 (M w 8.3–8.5), in north‐central Mongolia, is
one of the world's largest recorded intracontinental earthquakes and one of four great …
one of the world's largest recorded intracontinental earthquakes and one of four great …
Horizontal surface-slip distribution through several seismic cycles: The Eastern Bogd fault, Gobi-Altai, Mongolia
Abstract The 1957, MW 8.1, Gobi-Altai earthquake, Southern Mongolia, produced a~ 360-km-
long surface rupture along the Eastern Bogd fault. Cumulative offsets of geomorphic features …
long surface rupture along the Eastern Bogd fault. Cumulative offsets of geomorphic features …
Geomorphic Mesozoic and Cenozoic evolution in the Oka-Jombolok region (East Sayan ranges, Siberia)
M Jolivet, S Arzhannikov, A Arzhannikova… - Journal of Asian Earth …, 2013 - Elsevier
The East Sayan ranges are a key area to understand the interactions between the
transpressive deformation linked to the far-field effects of the India–Asia collision and the …
transpressive deformation linked to the far-field effects of the India–Asia collision and the …
Structural and geochronologic data from the Shin Jinst area, eastern Gobi Altai, Mongolia: Implications for Phanerozoic intracontinental deformation in Asia
MA Lamb, G Badarch, T Navratil, R Poier - Tectonophysics, 2008 - Elsevier
The complex geology of central Asia records significant Phanerozoic growth and
deformation of continental lithosphere, yet many questions about the timing and …
deformation of continental lithosphere, yet many questions about the timing and …
Finding the buried record of past earthquakes with GPR-based palaeoseismology: a case study on the Hope fault, New Zealand
In places where sedimentation and erosion compete at fast rates, part of the record of past
earthquakes on faults may be buried, hence hidden, in the first few metres below the …
earthquakes on faults may be buried, hence hidden, in the first few metres below the …