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Abstract

The Jurassic Callovian-Oxfordian Tuwaiq Mountain and Hanifa formations contain world-class hydrocarbon source rocks and carbonate reservoir rocks in Saudi Arabia. A regional stratigraphic framework of these formations has been constructed by integrating well logs, the sedimentology of core/drill cuttings, well-log electrofacies, and 3-D seismic interpretations. Seismic sequence stratigraphic analysis and forward stratigraphic modeling played an important role in further constraining this integrated sequence stratigraphic model.

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/content/papers/10.3997/2214-4609.20131812
2013-10-28
2021-12-02
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20131812
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