Results 101 to 110 of about 415 (171)
Probabilistic quantification of tsunami current hazard using statistical emulation. [PDF]
Gopinathan D, Heidarzadeh M, Guillas S.
europepmc +1 more source
The western coast of India is highly vulnerable to tsunami hazards due to its geographical proximity to the Makran Subduction Zone (MSZ), one of the most seismically active margins of the northern Indian Ocean.
Nayan Sharma +4 more
doaj +1 more source
Massive carbon storage in convergent margins initiated by subduction of limestone. [PDF]
Chen C, Förster MW, Foley SF, Liu Y.
europepmc +1 more source
Comparative orotomy of the Archean Superior and Phanerozoic Altaid orogenic systems. [PDF]
Kusky TM, Celâl Şengör AM.
europepmc +1 more source
High interseismic coupling in the Eastern Makran (Pakistan) subduction zone
Estimating the extent of interseismic coupling along subduction zone megathrusts is essential for quantitative assessments of seismic and tsunami hazards.
Lin NY +6 more
core
Geological evidence for AD 1008 tsunami along the Kachchh coast, Western India: Implications for hazard along the Makran Subduction Zone. [PDF]
Prizomwala SP +6 more
europepmc +1 more source
Earthquake source parameters in Zagros region (Iran) from the time-evolutive P-wave displacement. [PDF]
Nazeri S +4 more
europepmc +1 more source
Seismic source characterization (SSC) for probabilistic seismic hazard assessment (PSHA) in regions characterized by subduction megathrusts involves a considerable degree of ambiguity due to the complex nature of subducting plates and large seismogenic ...
Özacar, Atilla Arda +2 more
core
We present a preliminary estimation of tsunami hazard associated with the Makran subduction zone (MSZ) at the northwestern Indian Ocean. Makran is one of the two main tsunamigenic zones in the Indian Ocean, which has produced some tsunamis in the past ...
Zaker, Nasser H. +3 more
core +1 more source
A recovered Moho model by integrated inversion of gravity and seismic depths in Iran. [PDF]
Ebadi S +3 more
europepmc +1 more source

