A new tsunami hazard assessment for eastern Makran subduction zone by considering splay faults and applying stochastic modeling
Payam Momenia, Katsuichiro Godaa, Mohammad Mokhtariband Mohammad Heidarzadehc
aDepartment of Earth Sciences, University of Western Ontario, London, ON, Canada;bInternational Institute of Earthquake Engineering
and Seismology (IIEES), Tehran, Iran;cDepartment of Architecture and Civil Engineering, University of Bath, Bath, UK
ABSTRACT
Tsunami hazard imposed by possible rupture of splay faults is important as it may significantly
intensify tsunami heights locally. The Makran Subduction Zone (MSZ) in the northwestern
Indian Ocean can generate large thrust earthquakes that could trigger significant tsunamis. In
this paper, the effects of possible rupture of splay faults on the tsunami hazards of eastern MSZ
are studied by developing a framework that uses stochastic earthquake rupture models and
considers uncertainties related to rupture location, rupture geometry, seismic moment split
ratio, earthquake slip asperity location within a fault plane, and earthquake slip heterogeneity.
To quantify these uncertainties, 484 different parameter combinations of tsunami sources are
considered systematically. The geometry of splay faults is developed using the most recent
marine seismic surveys of the tectonic structure of the MSZ. A moment magnitude of 8.6 is
considered as a scenario magnitude. The results of this study are generated in two parts, by
considering average sources and stochastic sources. Results show significant local amplifica-
tion of the maximum tsunami heights due to splay faults. For instance, the maximum wave
height in Pasni, Pakistan can be amplified by a factor of four due to a single splay fault rupture
scenario of average source.
