Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/10708
Authors: | Murru, Maura* Akinci, Aybige* Falcone, Giuseppe* Pucci, Stefano* Console, Rodolfo* Parsons, T.* |
Title: | M ≥ 7 earthquake rupture forecast and time-dependent probability for the sea of Marmara region, Turkey | Journal: | Journal of Geophysical Research: Solid Earth | Series/Report no.: | 4/121(2016) | Issue Date: | Apr-2016 | DOI: | 10.1002/2015JB012595 | URL: | http://onlinelibrary.wiley.com/doi/10.1002/2015JB012595/full | Keywords: | stress interaction Marmara region rupture forecast time-dependent and time-independent probability |
Subject Classification: | 04.06. Seismology 05.08. Risk 04.07. Tectonophysics |
Abstract: | 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 augment time-dependent Brownian passage time (BPT) probability with static Coulomb stress changes (ΔCFF) from interacting faults. We calculate Mw > 6.5 probability from 26 individual fault sources in the Marmara region. We also consider a multisegment rupture model that allows higher-magnitude ruptures over some segments of the northern branch of the North Anatolian Fault Zone beneath the Marmara Sea. A total of 10 different Mw = 7.0 to Mw = 8.0 multisegment ruptures are combined with the other regional faults at rates that balance the overall moment accumulation. We use Gaussian random distributions to treat parameter uncertainties (e.g., aperiodicity, maximum expected magnitude, slip rate, and consequently mean recurrence time) of the statistical distributions associated with each fault source. We then estimate uncertainties of the 30 year probability values for the next characteristic event obtained from three different models (Poisson, BPT, and BPT + ΔCFF) using a Monte Carlo procedure. The Gerede fault segment located at the eastern end of the Marmara region shows the highest 30 year probability, with a Poisson value of 29% and a time-dependent interaction probability of 48%. We find an aggregated 30 year Poisson probability of M > 7.3 earthquakes at Istanbul of 35%, which increases to 47% if time dependence and stress transfer are considered. We calculate a twofold probability gain (ratio time dependent to time independent) on the southern strands of the North Anatolian Fault Zone. |
Appears in Collections: | Article published / in press |
Files in This Item:
File | Description | Size | Format | |
---|---|---|---|---|
Murru_et_al-2016-Journal_of_Geophysical_Research__Solid_Earth.pdf | 2.4 MB | Adobe PDF | View/Open |
WEB OF SCIENCETM
Citations
50
23
checked on Feb 10, 2021
Page view(s)
1,632
checked on Apr 17, 2024
Download(s)
124
checked on Apr 17, 2024