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Abstract

Investigation of core and outcrop samples of the Cenomanian Natih-B Member (North Oman) indicates that the different lithofacies present experienced rather different diagenesis shortly post-deposition. Petrographic, total organic-carbon (TOC), X-ray diffraction and stable-isotopic analyses have been employed to delineate the controls on early diagenesis and hydrocarbon source potential variability.

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/content/papers/10.3997/2214-4609-pdb.287.1186975
2012-03-04
2023-02-03
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1186975
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