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The document compares acoustic and electrical image logs collected from a well in the Coso Geothermal Field in California. It finds that the electrical logs are more sensitive to variations in mineralogy, porosity and fluid content, revealing both natural fractures and rock fabrics. The acoustic logs reveal a similar fracture population but image fewer fractures and do not reveal rock fabric. Both logs can provide information about stress states and fracture properties.

Author

ayoub ghanbari

Language

EN