Large earthquakes and cree** faults
RA Harris - Reviews of Geophysics, 2017 - Wiley Online Library
Faults are ubiquitous throughout the Earth's crust. The majority are silent for decades to
centuries, until they suddenly rupture and produce earthquakes. With a focus on shallow …
centuries, until they suddenly rupture and produce earthquakes. With a focus on shallow …
Slip distribution of the February 6, 2023 Mw 7.8 and Mw 7.6, Kahramanmaraş, Turkey earthquake sequence in the East Anatolian fault zone
S Barbot, H Luo, T Wang, Y Hamiel, O Piatibratova… - Seismica, 2023 - par.nsf.gov
On February 6, 2023, two large earthquakes occurred near the Turkish town of
Kahramanmaraş. The moment magnitude (Mw) 7.8 mainshock ruptured a 310 km-long …
Kahramanmaraş. The moment magnitude (Mw) 7.8 mainshock ruptured a 310 km-long …
High‐resolution surface velocities and strain for Anatolia from Sentinel‐1 InSAR and GNSS data
JR Weiss, RJ Walters, Y Morishita… - Geophysical …, 2020 - Wiley Online Library
Measurements of present‐day surface deformation are essential for the assessment of long‐
term seismic hazard. The European Space Agency's Sentinel‐1 satellites enable global …
term seismic hazard. The European Space Agency's Sentinel‐1 satellites enable global …
[کتاب][B] The mechanics of earthquakes and faulting
CH Scholz - 2019 - books.google.com
This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …
Earth observation for the assessment of earthquake hazard, risk and disaster management
JR Elliott - Surveys in geophysics, 2020 - Springer
Earthquakes pose a significant hazard, and due to the growth of vulnerable, exposed
populations, global levels of seismic risk are increasing. In the past three decades, a …
populations, global levels of seismic risk are increasing. In the past three decades, a …
Autonomous extraction of millimeter-scale deformation in InSAR time series using deep learning
B Rouet-Leduc, R Jolivet, M Dalaison… - Nature …, 2021 - nature.com
Systematically characterizing slip behaviours on active faults is key to unraveling the physics
of tectonic faulting and the interplay between slow and fast earthquakes. Interferometric …
of tectonic faulting and the interplay between slow and fast earthquakes. Interferometric …
Heterogeneous interseismic coupling along the **anshuihe‐**aojiang fault system, eastern Tibet
Y Li, JM Nocquet, X Shan, H Jian - Journal of Geophysical …, 2021 - Wiley Online Library
Abstract We use Global Positioning System (GPS) and Interferometric Synthetic Aperture
Radar (InSAR) data to quantify the interseismic coupling along the **anshuihe‐**aojiang …
Radar (InSAR) data to quantify the interseismic coupling along the **anshuihe‐**aojiang …
Fast and slow slip events emerge due to fault geometrical complexity
Active faults release elastic strain energy via a whole continuum of modes of slip, ranging
from devastating earthquakes to slow slip events (SSEs) and persistent creep …
from devastating earthquakes to slow slip events (SSEs) and persistent creep …
Constant strain accumulation rate between major earthquakes on the North Anatolian Fault
E Hussain, TJ Wright, RJ Walters, DPS Bekaert… - Nature …, 2018 - nature.com
Earthquakes are caused by the release of tectonic strain accumulated between events.
Recent advances in satellite geodesy mean we can now measure this interseismic strain …
Recent advances in satellite geodesy mean we can now measure this interseismic strain …
Creep fronts and complexity in laboratory earthquake sequences illuminate delayed earthquake triggering
SBL Cebry, CY Ke, S Shreedharan, C Marone… - Nature …, 2022 - nature.com
Earthquakes occur in clusters or sequences that arise from complex triggering mechanisms,
but direct measurement of the slow subsurface slip responsible for delayed triggering is …
but direct measurement of the slow subsurface slip responsible for delayed triggering is …