2015
DOI: 10.1007/s12517-015-2061-7
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Near-surface site characterization at Quriyat City, Sultanate of Oman using HVSR and MASW techniques

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Cited by 7 publications
(3 citation statements)
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“…Eleven of 14 sites are situated on weathered/phyllite/granite gneiss/granite schist rock type situated on structurally highly dissected hills. In general, the sites exhibit a flat H/V curve without a clear peak revealing that the station is on bedrock (Surve and Mohan, 2010; Mohamed et al ., 2016; Macau et al ., 2018; Fat‐Helbary et al ., 2019).…”
Section: Resultsmentioning
confidence: 99%
“…Eleven of 14 sites are situated on weathered/phyllite/granite gneiss/granite schist rock type situated on structurally highly dissected hills. In general, the sites exhibit a flat H/V curve without a clear peak revealing that the station is on bedrock (Surve and Mohan, 2010; Mohamed et al ., 2016; Macau et al ., 2018; Fat‐Helbary et al ., 2019).…”
Section: Resultsmentioning
confidence: 99%
“…In earthquake design, the Vs is a vital parameter in both liquefaction potential and soil ampli cation evaluations. However, observation of multi-modal dispersion characteristics and generation of 2-D or 3-D dispersion images becomes possible (Park et al, 2001;Park et al, 2007;Xia et al, 2003;Donohue et al, 2013;Lin et al, 2004;Park and Carnevale, 2010;Mohamed et al, 2013;Mohamed et al, 2016) Field Data Acquisition To obtain more accurate shear-wave velocity for a given site as a function of both depth and surface location a 2-D survey was performed for multiple eld deployments as the source and geophones roll along the survey line (both the source and geophone-array shift 4.0 m). Each shift represents the 1-D model.…”
Section: Data Acquisitionmentioning
confidence: 99%
“…The noise from approximately 0.1 to 1 Hz is generated by sources such as ocean waves, extensive regional storms and tectonic activity, while frequencies above 1 Hz typically originate from closer sources, including local storms, wind and human-made activities [5]. HVSR has been widely applied in sediment thickness estimation-related studies in different environments due to its simplicity in field acquisition and processing [6][7][8][9], including some applications on beaches [3,10,11]. Its complementarity with ERT, which utilizes active electrical input to model the sub-surface resistivities in 2D or 3D, has been highlighted in several works [12][13][14][15][16][17][18].…”
Section: Introductionmentioning
confidence: 99%