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Abstract

Since the early days of Vibroseis, it has been observed that the vibrator behavior differs for<br>different near-surface conditions. In its simplest form, the earth can be regarded as a spring,<br>resulting in a baseplate motion that decreases with increasing earth stiffness (increasing spring<br>constant). It was also observed that this simple spring model was accurate for low frequencies<br>but inadequate to explain the baseplate motion for higher frequencies, where several<br>resonance phenomena were observed in the vibrator response.

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/content/papers/10.3997/2214-4609.20147512
2008-10-13
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20147512
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