[HTML][HTML] Maximum earthquake magnitudes along different sections of the North Anatolian fault zone

M Bohnhoff, P Martínez-Garzón, F Bulut, E Stierle… - Tectonophysics, 2016 - Elsevier
Constraining the maximum likely magnitude of future earthquakes on continental transform
faults has fundamental consequences for the expected seismic hazard. Since the recurrence …

MSATSI: A MATLAB package for stress inversion combining solid classic methodology, a new simplified user‐handling, and a visualization tool

P Martínez‐Garzón, G Kwiatek… - Seismological …, 2014 - pubs.geoscienceworld.org
The estimation of the stress-field orientation from focal mechanisms of earthquakes is a
relevant tool to understand crustal mechanics and the physics of earthquakes. In global …

Microseismic constraints on the mechanical state of the North Anatolian fault zone 13 years after the 1999 M7. 4 Izmit earthquake

E Beaucé, RD van der Hilst… - Journal of Geophysical …, 2022 - Wiley Online Library
Abstract The 17 August 1999 Mw7. 4 Izmit earthquake ruptured the western section of the
North Anatolian Fault Zone and strongly altered the fault zone properties and stress field …

M ≥ 7 earthquake rupture forecast and time‐dependent probability for the sea of Marmara region, Turkey

M Murru, A Akinci, G Falcone, S Pucci… - Journal of …, 2016 - Wiley Online Library
We forecast time‐independent and time‐dependent earthquake ruptures in the Marmara
region of Turkey for the next 30 years using a new fault segmentation model. We also …

A unified earthquake catalogue for the Sea of Marmara Region, Turkey, based on automatized phase picking and travel-time inversion: Seismotectonic implications

C Wollin, M Bohnhoff, P Martínez-Garzón, L Küperkoch… - Tectonophysics, 2018 - Elsevier
The Marmara section of the North Anatolian Fault Zone (NAFZ) is late in its seismic cycle
and can be expected to produce a magnitude M up to 7.4 earthquake during the next …

Spatial-temporal distribution of early aftershocks following the 2016 Ms 6.4 Menyuan, Qinghai, China Earthquake

M Liu, H Li, Z Peng, L Ouyang, Y Ma, J Ma, Z Liang… - Tectonophysics, 2019 - Elsevier
The Lenglongling fault, located in the north Qilian fold zone along the northeastern margin of
the Tibetan Plateau, plays an important role in accommodating the tectonic deformation …

Resolution of non-double-couple components in the seismic moment tensor using regional networks—I: a synthetic case study

E Stierle, V Vavryčuk, J Šílený… - Geophysical Journal …, 2014 - academic.oup.com
We perform a detailed synthetic study on the resolution of non-double-couple (non-DC)
components in the seismic moment tensors from short-period data observed at regional …

Geomechanical model of the Marmara Sea region—II. 3-D contemporary background stress field

T Hergert, O Heidbach - Geophysical Journal International, 2011 - academic.oup.com
We present the contemporary 3-D background stress field of the Marmara Sea region
derived from a geomechanical model. The background stress field (ie the component of the …

Magnitudes of future large earthquakes near Istanbul quantified from 1500 years of historical earthquakes, present-day microseismicity and GPS slip rates

F Bulut, B Aktuğ, C Yaltırak, A Doğru, H Özener - Tectonophysics, 2019 - Elsevier
In the past 1500 years, seven sequences of significant earthquakes have occurred on a 160-
km-long segment of the North Anatolian Fault zone (NAFZ) centered on Istanbul. The most …

Deciphering aseismic deformation along submarine fault branches below the eastern Sea of Marmara (Turkey): Insights from seismicity, strainmeter, and GNSS data

V Durand, A Gualandi, S Ergintav, G Kwiatek… - Earth and Planetary …, 2022 - Elsevier
The recently observed slow transients in the Sea of Marmara are important to quantify the
seismic hazard and risk for the greater Istanbul metropolitan region. In this study, we analyze …