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Abstract

Rock properties of the Natih Formation in Field F were strongly modified as a result of diagenesis. The paragenetic sequence is well defined, and typical for a carbonate field from this geographic location and time period. It exhibits an interplay between early diagenetic processes, faulting and the tectonically controlled circulation of deep burial fluids. Conclusions are supported by detailed petrographic and geochemical data including isotopes, fluid inclusions and elemental compositions.

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/content/papers/10.3997/2214-4609.20145357
2010-01-24
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145357
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