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Abstract

This paper offers a new method for downward continuation of some stationary geophysical (geothermal or geo-electrical) fields in 3D gradient media.

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/content/papers/10.3997/2214-4609.201410918
1991-05-28
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410918
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