8–12 Sept 2025
Hofburg Palace & Online
Europe/Vienna timezone
Platform is live at https://snt2025.ctbto.org

Session

P1.2 The Solid Earth and its Structure

P1.2
12 Sept 2025, 10:00
Zeremoniensaal

Zeremoniensaal

Conveners

P1.2 The Solid Earth and its Structure

  • Onkgopotse Ntibinyane (CTBTO Preparatory Commission)
  • Sherif Ali (CTBTO Preparatory Commission)

Description

E-poster session with display of each e-poster on an assigned touchscreen

Presentation materials

There are no materials yet.
Mohamed Yassien (National Research Institute of Astronomy and Geophysics (NRIAG))
12/09/2025, 10:00
T1.2 The Solid Earth and its Structure
E-poster

The growing interest in pulse-like ground motions, especially occurring near faults, stems from their potential to inflict significant structural damage due to distinct directivity and fling effects. This study seeks to enhance the identification and classification of these impulsive ground motions by integrating traditional data-processing methods with advanced machine learning techniques....

Mr Umar Afegbua Kadiri (Centre for Geodesy and Geodynamics, National Space Research and Development Agency)
12/09/2025, 10:00
T1.2 The Solid Earth and its Structure
E-poster

Probabilistic Seismic Hazard Assessments (PSHA) have not been conducted in large parts of Sub-Saharan Africa (SSA), due to incomplete earthquake catalogues, sparse seismic networks, etc; raising concerns on needed information for planning and disaster risk management. This study aims to bridge this research gap using modern techniques. Updated catalogue from Local Networks, significant data...

Thomas Hardy (Indonesian Agency for Meteorology, Climatology and Geophysics (BMKG))
12/09/2025, 10:00
T1.2 The Solid Earth and its Structure
E-poster

The devastating earthquake followed by the tsunami that occurred in Palu, Indonesia, on 28 September 2018 resulted in the death of more than 4300 people and serious damage to more than 12 000 buildings. Earthquake-induced site displacement is critical information for estimating the magnitude of earthquakes. Compared to a seismometer, which the signal clipping when recording in the near-field...

Maria Rayla dos Santos (Universidade Federal do Rio Grande do Norte)
12/09/2025, 10:00
T1.2 The Solid Earth and its Structure
E-poster

Oceanic transform faults are important tectonic structures connecting mid-ocean ridge sections, controlling their global morphology, movements, deformation, and rupture process. The complete understanding of these fracture zones relies on earthquake focal depth (Z) estimation. Z is a critical parameter for these tectonic studies that is usually difficult to estimate due to unfavorable...

Mr Umar Afegbua Kadiri (Centre for Geodesy and Geodynamics, National Space Research and Development Agency)
12/09/2025, 10:00
T1.2 The Solid Earth and its Structure
E-poster

From 10 to 19 September 2024, residents of Mpape, a densely populated settlement in Abuja, Nigeria, with a high concentration of mining firms, witnessed a series of vibrations that they thought were from usual ground shakings resulting from regular quarry blasts. The duration (nine days) of the vibrations motivated this research to determine the seismotectonic nature and characterize...

Prof. Khalid Zahran (National Research Institute of Astronomy and Geophysics (NRIAG))
12/09/2025, 10:00
T1.2 The Solid Earth and its Structure
E-poster

The Aegean Sea is one of the key regions for the understanding of fundamental tectonic processes, including continental rifting. In addition, the continuous seismicity is attributed to its tectonic settings, which indicates the activities of these tectonics. Thus, tectonics and geodynamics of this region have always been the attention of many interested in earth sciences. Radar altimetry data...