首页> 外文会议>Workshop on Geothermal Reservoir Engineering >ESTIMATION OF DEEP SUBSURFACE STRUCTURE IN EUROPEAN HOT DRY ROCK TEST SITE, SOULTZ-SOUS-FOReTS, FRANCE, BY USE OF THE AE REFLECTION METHOD
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ESTIMATION OF DEEP SUBSURFACE STRUCTURE IN EUROPEAN HOT DRY ROCK TEST SITE, SOULTZ-SOUS-FOReTS, FRANCE, BY USE OF THE AE REFLECTION METHOD

机译:估计欧洲热干岩试验网站深度地下结构,使用AE反射方法估算Soultz-Sous-Forets,Soustz-sous-Forets

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Recently, the further Hot Dry Rock (HDR) development toward great depth has been started at the Soultz-sous-Forets, 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 timefrequency 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.
机译:最近,在法国的Soultz-Sous-Forets开始,进一步热干岩石(HDR)开发已经开始。因此,更深层次的地下结构的理解正在进行更重要的作用。在本文中,我们通过应用我们在时间频道中调用AE反射方法的反射技术来估计Soultz HDR站点的深度地下结构,其中诱导声发射(AE)信号用作Wavesource。首先,我们简要介绍时频域中的AE反射方法。接下来,我们展示了包括一些有意义的反射器的三维深度成像。然后,我们沿着GPK-1的轨迹精确地涉及检测到的反射器,并加深GPK-2,并比较AE反射方法与其他钻孔观察。结果表明,与GPK-1中的骨折区分布良好的一致性,并且在加深GPK-2期间,从源自切屑的微观检查的合成岩体原木中可能对应于可能的裂缝区。

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