1887

Abstract

There is a large amount of evidence which can be used to demonstrate that the Mesozoic rifting and structural style of the North Atlantic margins is determined by Precambrian extensional structures and not Caledonian (Late Ordovician to Silurian) compressional structures as previously presumed.

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/content/papers/10.3997/2214-4609.201409586
1995-05-29
2020-11-01
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409586
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