1887

Abstract

Seismic velocities are conventionally obtained using ray-based reflection tomography and are often considered only for the purpose of depth imaging. We demonstrate using Valhall wide-azimuth field data that 3D frequency domain full waveform inversion prod

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/content/papers/10.3997/2214-4609.201400395
2009-06-08
2020-04-10
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400395
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