Glossary
Curve saturation
Curve saturation occurs with dipmeters and resistivity imaging devices when they attempt to gather data beyond the range of the device. This range is a function of mud to formation resistivity and maximum mud resistivity. Resistivity saturation will occur within resistive formations including hydrocarbon charged sections and rock types such a carbonates and evaporites. It is often difficult or impossible to discern features within such sections. A saturated image, however, through a known resistive mass (e.g. carbonate nodule) is a useful check on image polarity.
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About the glossary
This listing is not exhaustive or definitive, do not expect Oxford English Dictionary standards; it is aimed at those who need to understand basic principles and those that read reports on dipmeters and borehole images requiring some technical help to get the most from such documents.
We have attempted to make the descriptions and explanations generic, giving the glossary a wide application and appeal, with minimal, if any, commercial bias. If you spot any mistakes, omissions or any problems with the explanations, please do not hesitate to contact us, and we will try to accommodate your comments.
Acknowledgements
This listing has been derived by Task Geoscientists. All external sources are fully acknowledged.




