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ESTIMATION OF DEEP SUBSURFACE STRUCTURE IN EUROPEAN HOT DRY ROCK TEST SITE, SOULTZ-SOUS-FOR TS, FRANCE, BY USE OF THE AE REFLECTION METHOD

Nobukazu SOMA, Hiroaki NIITSUMA and Roy BARIA

Key words
Soultz-sous-ForÍts
Location
Soultz-sous-Forets, France
Conference
Stanford Geothermal Workshop
Year
2000
Session
Hot dry rock
Language
English

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Abstract

Recently, the further Hot Dry Rock (HDR) development toward great depth has been started at the Soultz-sous-ForÍts, France. Therefore the understandings deeper subsurface structure is taking on more important role. In this paper we present an estimation of deep subsurface structure in the Soultz HDR site by applying a type of reflection technique which we call the AE reflection method in time-frequency domain, where induced acoustic emission (AE) signals are used as wavesource. First, we mention the AE reflection method in time-frequency domain briefly. Next, we show the three-dimensional deep imaging which includes some meaningful reflectors. Then we precisely relate detected reflectors along the trajectory of well GPK-1 and deepened GPK-2, and compare the AE reflection method with other borehole observations. The results indicate a good agreement with distribution of fracture zone in GPK-1 and corresponds with possible fracture zone from a synthetic petrographic log derived from microscopic examination of cuttings during deepening of GPK-2..

Copyright 2000, Stanford Geothermal Program. 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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