首页> 外文会议>Geothermal Resources Council annual meeting 2010 >The Tectonic and Magneto-Telluric Survey Effects on the Geothermal Explorations Around the Menderes Massif in the Western Anatolia, Turkey
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The Tectonic and Magneto-Telluric Survey Effects on the Geothermal Explorations Around the Menderes Massif in the Western Anatolia, Turkey

机译:土耳其安那托斯西部Menderes断层附近的构造和磁-碲测量对地热勘探的影响

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Western Anatolia is one of the most active tectonic and seismic areas of the world, and has important geothermal potential. As indicated in several related articles, the area is characterized by high heat flow over a wide area suggesting regional geothermal potential. Although surface manifestations are lacking in many areas, several deeper geothermal reservoirs may be hidden and a few of them have been discovered recently. The lack of wide-spread surface manifestations means that the regional tectonics, resistivity (through magneto-tellurics), geochemistry and seismic reflection surveys are important methods in exploring for geothermal resources in Anatolia. Seismic methods are more expensive and are being used in exploring for potential EGS systems. Reflection seismics have been applied in petroleum exploration in Turkey and that the data are available and are being reviewed to determine the structures that might control geothermal circulation. BM Holding has been exploring geothermal resources around the Menderes Massif since 2005. Exploration in the Menderes Massif has been guided by understanding, the young structural picture and the regional tectonics of western Anatolia and the Aegean region. In extensional tectonic regions as in the western Anatolia of Turkey, geothermal systems located in areas of complex vertical and horizontal tectonics may be mixed and re-equilibrated geochemically due to the different permeability environments. Conventional surface geochemistry methods conducted along surface may not be enough to explore deeper and hotter geothermal reservoirs. Magnetotelluric methods applied to the metamorphic complexes such as Menderes Massif may be strongly influenced by the graphitic contents of the basement metamorphic rocks. Low resistivity anomalies within Menderes grabens also may be misleading because of superimposed basins and extraordinary sediment/ clay thicknesses. Resisting a fall into "anomaly hunting" requires thatseveral common exploration methods may be eliminated or combined in depending on the geological conditions.
机译:安纳托利亚西部是世界上最活跃的构造和地震地区之一,具有重要的地热潜力。如几篇相关文章所述,该区域的特征是在宽广的区域内存在高热流,表明该地区具有地热潜力。尽管许多地区缺乏地表表现,但可能隐藏了一些更深的地热储层,并且最近发现了其中一些。缺乏广泛的地表表现意味着区域构造,电阻率(通过磁电磁学),地球化学和地震反射调查是勘探安纳托利亚地热资源的重要方法。地震方法更昂贵,并被用于探索潜在的EGS系统。反射地震已在土耳其的石油勘探中得到应用,并且已有数据可用并正在接受审查,以确定可能控制地热循环的结构。自2005年以来,BM控股一直在Menderes地块附近勘探地热资源。Menderes地块的勘探工作以了解,年轻的安纳托利亚和爱琴海地区的构造图景以及区域构造为指导。在土耳其安纳托利亚西部的伸展构造区域中,由于渗透率环境的不同,位于垂直构造和水平构造复杂的区域中的地热系统可能会在地球化学上发生混合和重新平衡。沿地表进行的常规地表地球化学方法可能不足以勘探更深,更热的地热储层。应用于变质复合体(如Menderes Massif)的大地电磁方法可能会受到地下变质岩中石墨含量的强烈影响。由于盆地的叠加以及异常的沉积物/黏土厚度,Menderes ens陷内的低电阻率异常也可能会产生误导。抵制“异常狩猎”的要求 根据地质条件,可以取消或组合几种常见的勘探方法。

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