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Heightened Odds of Large Earthquakes Near Istanbul: An Interaction-Based Probability Calculation

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TLDR
The probability of strong shaking in Istanbul from the description of earthquakes on the North Anatolian fault system in the Marmara Sea during the past 500 years is calculated and the resulting catalog is tested against the frequency of damage in Istanbul during the preceding millennium.
Abstract
We calculate the probability of strong shaking in Istanbul, an urban center of 10 million people, from the description of earthquakes on the North Anatolian fault system in the Marmara Sea during the past 500 years and test the resulting catalog against the frequency of damage in Istanbul during the preceding millennium. Departing from current practice, we include the time-dependent effect of stress transferred by the 1999 moment magnitude M = 7.4 Izmit earthquake to faults nearer to Istanbul. We find a 62 ± 15% probability (one standard deviation) of strong shaking during the next 30 years and 32 ± 12% during the next decade.

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Neotectonics of Turkey – a synthesis

TL;DR: In this article, the authors describe Turkey as one of the most actively deforming regions in the world and has a long history of devastating earthquakes, and the belter understanding of its neotectonic features and active tectonics wou...
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A two-stage stochastic programming framework for transportation planning in disaster response

TL;DR: This study proposes a two-stage stochastic programming model to plan the transportation of vital first-aid commodities to disaster-affected areas during emergency response, and a multi-commodity, multi-modal network flow formulation is developed to describe the flow of material over an urban transportation network.
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The north anatolian fault: a new look

TL;DR: The North Anatolian Fault (NAF) as discussed by the authors is a 1200 km-long dextral strike-slip fault zone that formed by progressive strain localization in a generally westerly widening right-lateral keirogen in northern Turkey mostly along an interface juxtaposing subduction-accretion material to its south and older and stiffer continental basements to its north.
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Forecasting the evolution of seismicity in southern California: Animations built on earthquake stress transfer

TL;DR: In this article, a forecast model was developed to reproduce the distribution of main shocks, aftershocks and surrounding seismicity observed during 1986-2003 in a 300 × 310 km area centered on the 1992 M = 7.3 Landers earthquake.
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Earthquake triggering by static, dynamic, and postseismic stress transfer

TL;DR: In this paper, the authors used static Coulomb stress changes associated with earthquake slip to explain aftershock distributions, earthquake sequences, and the quiescence of broad, normally active regions following large earthquakes.
References
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Journal ArticleDOI

New Empirical Relationships among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement

TL;DR: In this article, a series of empirical relationships among moment magnitude (M ), surface rupture length, subsurface rupture length and downdip rupture width, and average surface displacement per event are developed.
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Internal deformation due to shear and tensile faults in a half-space

TL;DR: A complete set of closed analytical expressions for the internal displacements and strains due to shear and tensile faults in a half-space for both point and finite rectangular sources is presented in this paper.
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Static stress changes and the triggering of earthquakes

TL;DR: In this article, a Coulomb failure criterion was proposed for the production of aftershocks, where faults most likely to slip are those optimally orientated for failure as a result of the prevailing regional stress field and the stress change caused by the mainshock.
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The role of stress transfer in earthquake occurrence

TL;DR: In this paper, it was shown that small, sudden stress changes cause large changes in seismicity rate, where rates climb where the stress increases (aftershocks) and fall when the stress drops.
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A constitutive law for rate of earthquake production and its application to earthquake clustering

TL;DR: In this article, the authors proposed a state-variable constitutive formulation for the rate of earthquake production resulting from an applied stressing history, which was implemented using solutions for nucleation of unstable fault slip on faults with experimentally derived rate and state dependent fault properties.
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