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Magnetotelluric and Seismic Noise Techniques Combination for the Cerdanya Basin Characterization (Eastern Pyrenees)

机译:Cerdanya盆地表征的Magnetelluric和地震噪声技术组合(东比利牛斯)

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A sedimentary Tertiary basin filled with unconsolidated sediments located in eastern Pyrenees has been subjected to a combine passive geophysical survey in order to increase knowledge of bedrock geometry and sediment properties. The methodology consists of combining and integrating both seismic noise techniques (H/V and array) and audio-magnetotelluric (AMT) and magnetotelluric (MT) data. AMT and MT data have been recorded along a NW-SE profile crossing the basin. Four 2D seismic noise arrays and 79 single station measurements were deployed at this profile. H/V technique has been suitable to obtain a soil fundamental frequency. Bedrock depth assessment can be obtained using S-wave velocity profiles derived from seismic noise array analysis. This information will allow establishing a soil fundamental frequency-bedrock depth relationship suitable for this basin. On the other hand, interpretation of the electrical resistivity model obtained from an AMT- MT survey will be constrained by the seismic results. This electrical resistivity model provides a detailed imaging of structural features such as the Cerdanya fault. This methodology, based on sediment characterization from shear-wave velocity and resistivity information, can be an attractive option for basin characterization essential for projects such as reservoir imaging.
机译:填充有位于东方比利牛斯特的未溶解沉积物的沉积三级盆地已经进行了组合被动地球物理调查,以增加基岩几何形状和沉积物的知识。该方法包括组合和集成地震噪声技术(H / V和阵列)和音频 - 磁通尿(AMT)和MagnetOcteluric(MT)数据。 AMT和MT数据沿着盆地的NW-SE型材记录。在此配置文件中部署了四个2D地震噪声阵列和79个单站测量。 H / V技术适合获得土壤基波频率。可以使用来自地震噪声阵列分析的S波速度分布来获得基岩深度评估。该信息将允许建立适合该盆地的土壤基波频率基岩深度关系。另一方面,从AMT-MT调查中获得的电阻率模型的解释将受到地震结果的限制。该电阻率模型提供了诸如Cerdanya故障的结构特征的详细成像。该方法基于剪切波速度和电阻率信息的沉积物表征,可以是盆地表征的有吸引力的盆地,例如储层成像等项目。

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