Classification of soil stiffness using p-wave.

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dc.contributor.authorSamah, Rose Nadia Abu
dc.date.accessioned2018-07-27T02:30:02Z
dc.date.available2018-07-27T02:30:02Z
dc.date.issued2016-08
dc.description.abstractTomografi seismik biasan (SRT) adalah satu kaedah geofizik yang mengukur perambatan gelombang bunyi di bawah permukaan bumi. Kaedah ini memerlukan tenaga tiruan sebagai sumber. Seismic refraction tomography (SRT) is a geophysical method that measures the propagation of sound wave in Earth’s subsurface. This method required an artificial energy as a seismic source.en_US
dc.identifier.urihttp://hdl.handle.net/123456789/6053
dc.language.isoenen_US
dc.publisherUniversiti Sains Malaysiaen_US
dc.subjectStiffnessen_US
dc.subjectP waveen_US
dc.titleClassification of soil stiffness using p-wave.en_US
dc.typeThesisen_US
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