1887

Abstract

Current high resolution sequence stratigraphic models are mainly derived from areas where tectonic subsidence and/or uplift are relatively simple. Subsidence is generally assumed to occur at a uniform rate and to be slow in comparison to eustatic sea-level changes.

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/content/papers/10.3997/2214-4609.201409655
1995-05-29
2020-05-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409655
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