Inversion of velocity parameters in multilayered elliptical anisotropy medium - synthetic data example

In the medium composed of parallel sedimentary layers, model of elliptic anisotropy is often better approximation of real conditions than simple layers with constant velocity. In such model a velocity is described with 3 parameters: a, b (responsible for vertical velocity and its gradient) and χ - e...

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Bibliographic Details
Main Authors: Gierlach Bartosz, Danek Tomasz
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Subjects:
Online Access:https://doi.org/10.1051/e3sconf/20186601017