Broadband laboratory measurements of dispersion in thermally cracked and fluid-saturated quartzite and a synthetic analogue
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Li, Yang
Olin, Melissa
David, Emmanuel
Jackson, Ian
Schijns, Heather
Schmitt, Douglas
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Society of Exploration Geophysicists
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In the field, the seismic waves used for active-source imaging typically contain frequencies from 10 to about 100 Hz, with corresponding wavelengths of tens of meters. This contrasts greatly with the ultrasonic (∼ 1-MHz) wave-speed measurements carried
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Leading Edge, The
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2037-12-31
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