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Abstract

The evolutionary history of a basin is in general attempted reconstructed on the basis of the relative distribution of sedimentary strata as a function of the geological history. Associated basin extension models, say of the McKenzie type, presume a homogeneous crust subject to uniform stretching. The validity of such a hypothesis can be examined on the basis of deep (16-40 sTWT) seismic reflection data and is the topic of this presentation.

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/content/papers/10.3997/2214-4609.201410961
1991-05-28
2024-04-26
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