Marc De Batist
Biographic Data
| ID | 4131949 |
|---|---|
| NAME | Marc De Batist |
| GIVEN NAMES | Marc |
| FAMILY NAME | De Batist |
| SIGNATURE | DE BATIST M |
| AFFILIATIONS | Ghent University |
| ORCID | 0000-0002-1625-2080 |
| VERIFIED | Yes |
| TOTAL WORKS | 7 |
| TOTAL CITATIONS | 2 |
| AUTHOR COUNT | 7 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2008 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 1 |
Geomorphology of the Axial Channel (Southern Bight, North Sea)
This study presents a transnational geomorphological map of the Southern Bight, North Sea, using bathymetric data (EMODnet – c. 115 m horizontal resolution; UKHO – 4 m horizontal resolution). Based on the erosional and/or depositional relationship of the mapped features, a first step is established towards the reconstruction of the evolution of the Axial Channel, i.e. a major geomorphological feature on the southern North Sea seafloor. It reveals…
Sublacustrine canyons of the South and Central Basins of Lake Baikal as a result of interaction of tectonic, lithological and climatic factors
Dropstones in Lacustrine Sediments as a Record of Snow Avalanches—A Validation of the Proxy by Combining Satellite Imagery and Varve Chronology at Kenai Lake (South-Central Alaska)
Snow avalanches cause many fatalities every year and damage local economies worldwide. The present-day climate change affects the snowpack and, thus, the properties and frequency of snow avalanches. Reconstructing snow avalanche records can help us understand past variations in avalanche frequency and their relationship to climate change. Previous avalanche records have primarily been reconstructed using dendrochronology. Here, we investigate the…
The lake floor morphology of the Southern Baikal rift basin as a result of holocene and Late Pleistocene seismogenic and gravitational processes
Historical Nankai-Suruga megathrust earthquakes recorded by tsunami and terrestrial mass movement deposits on the Shirasuka coastal lowlands, Shizuoka Prefecture, Japan
Geological investigations of coastal sediment sequences play a key role in verifying earthquake and tsunami characteristics inferred from historical records. In this paper, we present a multi-proxy investigation of a coastal lowland site facing the Nankai-Suruga megathrust and appraise evidence for tsunamis and earthquake-triggered terrestrial mass movements occurring over the last 800 years. Combining a high-resolution chronology with X-ray comp…
Fault segmentation, paleostress and paleoseismic investigation in the Dodoma Area, Tanzania: Implications for seismic hazard evaluation
The Dodoma area (Tanzania) lies within the Tanzanian craton, in a region where the eastern branch of the East African Rift System seems to die out (or propagate?) into the craton. The area is characterized by low-to moderate-magnitude seismic activity, sometimes concentrated into so-called "earthquake swarms", but also by rare large earthquakes (up to Mw = 6.2). On 4 November 2002, an earthquake ofMw ffi 5.5 struck the
Fault segmentation, paleostress and paleoseismic investigation in the Dodoma Area, Tanzania: Implications for seismic hazard evaluation
Historical Nankai-Suruga megathrust earthquakes recorded by tsunami and terrestrial mass movement deposits on the Shirasuka coastal lowlands, Shizuoka Prefecture, Japan
Geological investigations of coastal sediment sequences play a key role in verifying earthquake and tsunami characteristics inferred from historical records. In this paper, we present a multi-proxy investigation of a coastal lowland site facing the Nankai-Suruga megathrust and appraise evidence for tsunamis and earthquake-triggered terrestrial mass movements occurring over the last 800 years. Combining a high-resolution chronology with X-ray comp…
Fault segmentation, paleostress and paleoseismic investigation in the Dodoma Area, Tanzania: Implications for seismic hazard evaluation
The Dodoma area (Tanzania) lies within the Tanzanian craton, in a region where the eastern branch of the East African Rift System seems to die out (or propagate?) into the craton. The area is characterized by low-to moderate-magnitude seismic activity, sometimes concentrated into so-called "earthquake swarms", but also by rare large earthquakes (up to Mw = 6.2). On 4 November 2002, an earthquake ofMw ffi 5.5 struck the
Fault segmentation, paleostress and paleoseismic investigation in the Dodoma Area, Tanzania: Implications for seismic hazard evaluation
Historical Nankai-Suruga megathrust earthquakes recorded by tsunami and terrestrial mass movement deposits on the Shirasuka coastal lowlands, Shizuoka Prefecture, Japan
Geological investigations of coastal sediment sequences play a key role in verifying earthquake and tsunami characteristics inferred from historical records. In this paper, we present a multi-proxy investigation of a coastal lowland site facing the Nankai-Suruga megathrust and appraise evidence for tsunamis and earthquake-triggered terrestrial mass movements occurring over the last 800 years. Combining a high-resolution chronology with X-ray comp…
Dropstones in Lacustrine Sediments as a Record of Snow Avalanches—A Validation of the Proxy by Combining Satellite Imagery and Varve Chronology at Kenai Lake (South-Central Alaska)
Snow avalanches cause many fatalities every year and damage local economies worldwide. The present-day climate change affects the snowpack and, thus, the properties and frequency of snow avalanches. Reconstructing snow avalanche records can help us understand past variations in avalanche frequency and their relationship to climate change. Previous avalanche records have primarily been reconstructed using dendrochronology. Here, we investigate the…
The lake floor morphology of the Southern Baikal rift basin as a result of holocene and Late Pleistocene seismogenic and gravitational processes
Sublacustrine canyons of the South and Central Basins of Lake Baikal as a result of interaction of tectonic, lithological and climatic factors
Geomorphology of the Axial Channel (Southern Bight, North Sea)
This study presents a transnational geomorphological map of the Southern Bight, North Sea, using bathymetric data (EMODnet – c. 115 m horizontal resolution; UKHO – 4 m horizontal resolution). Based on the erosional and/or depositional relationship of the mapped features, a first step is established towards the reconstruction of the evolution of the Axial Channel, i.e. a major geomorphological feature on the southern North Sea seafloor. It reveals…
Geology (6 works) · Oceanography (4 works) · Paleontology (4 works) · Tectonics (4 works) · Bathymetry (3 works) · earthquake and tectonic studies (3 works) · Geology and Paleoclimatology Research (3 works) · Geomorphology (3 works) · Seismology (3 works) · Canyon (2 works)