1887

Abstract

Imaging in complex geological areas requires multi-valued traveltime and amplitude information [1], [2]. Traditionally two- point raytracing is used to calculate the shortest traveltime and ray path between two points .

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/content/papers/10.3997/2214-4609.201408238
1998-06-08
2021-08-06
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408238
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