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Abstract

Studies of sequence, sedimentology and structure in four Oligo-Miocene basins in southern Anatolia reveal broadly similar, but diachronous, patterns of evolution that include a significant phase of marginal reef-carbonate development early in the Miocene history of each basin.

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/content/papers/10.3997/2214-4609.201406073
2000-10-01
2021-08-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406073
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