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

Author:

Bohnhoff Marco,Martínez-Garzón Patricia,Bulut Fatih,Stierle Eva,Ben-Zion Yehuda

Funder

Helmholtz Association in the frame of the “Young Investigators Group”

Helmholtz Postdoc Programme

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference132 articles.

1. Evidence for a minimum 52±1 km of total offset along the northern branch of the North Anatolian Fault in northwest Turkey;Akbayram;Tectonophysics,2016

2. Generation and propagation of G waves from the Niigata earthquake of June 16, 1964, 2, Estimation of earthquake moment released, energy, and stress-strain drop from the G wave spectrum;Aki;Bull. Earthq. Res. Inst., Univ. Tokyo,1966

3. Global historical earthquake archive and catalogue (1000—1903);Albini,2013

4. Active Faulting in Northern Turkey. Division Geol. Sci. Contr. no. 1577;Allen,1969

5. Sarköy-Mürefte 1912 earthquake’s tsunami, extension of the associated faulting in the Marmara Sea. Turkey;Altinok;J. Seismol.,2003

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