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Determination of Fractured Zones by Well Logging in Low Transmissivity Geothermal Reservoirs in Kochani Valley, Macedonia, Yugoslavia

Verbovsek, Renato

Key words
Geophysical Surveys; Well Tests; Exploration; Reservoir Parameters; Yugoslavia; Macedonia; Kochani Valley; Spontaneous Potential; Temperature Gradient; Flow Tests; Anomalies; Case Studies; Fractures; Resistivity; Low Temperature; Reservoir; Transistivity
Location
Kocani valley, Macedonia
Conference
Geothermal Resources Council Transactions
Year
1985
Session
Exploration; Geophysical surveys; Fractures; Temperature gra
Language
English

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Abstract

Surface geophysical methods currently used have considerable limitations in localizing deeper fractures or fractured zones bearing thermal waters. When considering geothermal reservoirs with relatively low transmissivities, only a low number of hydraulically active fractures can be encountered. Their number depends statically on the borehole length in the reservoir penetrated. Using standard logging devices it is difficult to detect them during drilling operations. Recent researches in Kochani Valley geothermal area have given us some experience on detecting water bearing fractures. Production logs, such as gradient with differential temperature and flow meter log have revealed as very adequate in detecting them, especially when executed in developed wells. On the basis of this logs, wells were acid treated by injecting acid mixture into fracture depth and in this way specific yield was considerably increased, in some cases for several times.

Copyright 1985, Geothermal Resources Council. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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