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Abstract

For decades, the seismic information that has been used to estimate lithological and fluid<br>properties of a propagating medium has been data in scalar form. For example, marine<br>seismic data have been generated with scalar sources (air guns suspended in water) and<br>recorded with scalar sensors (hydrophones).

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/content/papers/10.3997/2214-4609.201405690
2003-06-02
2023-12-02

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