1887

Abstract

The subsurface velocity field in the northern portion of the U.K. Southern Gas Basin is complicated by the presence of (Permian) Zechstein salt swells and diapirs. In addition, the post-zechstein (post-Permian) section displays large lateral velocity variations.

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/content/papers/10.3997/2214-4609.201411905
1990-07-15
2020-10-30
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411905
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