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Abstract

Hydrothermal dolomite (HTD) reservoirs are well-known<br>from exploration and development of hydrocarbon plays in the<br>Middle East. Petroleum geoscientists query for means to<br>model the related reservoir properties. This contribution<br>describes the field geometry, petrography and geochemistry of<br>hydrothermal dolomitisation fronts (Late Jurassic, Lebanon)<br>and aims to investigate the relationship between diagenetic<br>evolution and reservoir quality.

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/content/papers/10.3997/2214-4609-pdb.147.iptc11460
2007-12-04
2024-12-08
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/content/papers/10.3997/2214-4609-pdb.147.iptc11460
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