Identification of hidden faults using determining velocity structure profile by spatial autocorrelation method in the west of Mashhad plain (Northeast of Iran)

Author:

Nemati Seyedeh FatemehORCID,Hafezi Moghadas NaserORCID,Lashkaripour Gholam RezaORCID,Sadeghi HoseinORCID

Publisher

Springer Science and Business Media LLC

Subject

Nature and Landscape Conservation,Earth-Surface Processes,Geology,Geography, Planning and Development,Global and Planetary Change

Reference77 articles.

1. Abrahamson N (1998) Seismological aspects of near-fault ground motions. In 5th Caltrans Seismic Research Workshop.

2. Aghanabati SA (2004) Geology of Iran. Geological Survey and Mineral Exploration of Iran. p 154.

3. Aki K (1957) Space and time spectra of stationary stochastic waves, with special reference to microtremors. Bull Earthq Eng 35: 415–456. http://oceanrep.geomar.de/43280/1/Aki.pdf

4. Anbazhagan P, Kumar A, Sitharam TG (2013) Seismic site classification and correlation between standard penetration test N value and shear wave velocity for LucknowCity in Indo-Gangetic Basin. Pure Appl Geophys 170:299–318. https://doi.org/10.1007/s00024-012-0525-1

5. Apostolidis P, Raptakis D, Roumelioti Z, et al. (2004) Determination of S-wave velocity structure using microtremors and SPAC method applied in Thessaloniki (Greece). Soil Dyn Earthq Eng 24(1): 49–67. https://doi.org/10.1016/j.soildyn.2003.09.001

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