1887

Abstract

The latest Jurassic–Early Barremian carbonate systems of the United Arab Emirates (UAE) and Oman are organized as a succession of prograding wedges over almost 300 km towards the northeast. The integration of outcrop and subsurface data allows the definition of clinoform architecture, the proposal of regional correlations, and the characterization of the main stages of evolution of this part of the Arabian Plate (Figure 1).

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/content/papers/10.3997/2214-4609.20142783
2012-12-09
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20142783
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