Glossary
Mirror image dip
Mirror image dips have a dip equal to the hole inclination and are directed opposite to the hole azimuth for a given depth. Mirror image dips usually arise from automatic processing of dipmeter data when individual curves are affected at the same time by an excursion that swamps the resistivity or acoustic signal from the formation. Stick and pull is the commonest cause of this type of artefact. As each pad is affected at the same time it generates an event on each trace that defines a plane perpendicular to the well bore. All processed dip data should be checked against hole orientation for the presence this feature. The use of angular filters during processing can help minimise this problem, although when holes are drilled almost perpendicular to bedding this problem it can be difficult to untangle mirror image dips from genuine dips. Visual examination and manual picking of dipmeter curves allows a further avenue of analysis when a succession is heavily affected by mirror image dips.
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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.




