利用大地电磁资料对玄武岩成像的可行性(英文)
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摘要
磁大地电流法(MT)已成为有助于地下盐和地下玄武岩地震成像的有利方法之一。本文印度卡奇地区(这个地区玄武岩覆盖了中生代沉积岩)。并讨论了利用MT方法作为这样地质背景地区勘探工具的可能性。我们的结果突出了由侵入薄层玄武岩引起的磁大地电流响应的差别。本文讨论的关键问题是在这样的地质背景条件下MT方法能够或不能提供什么。首先我们利用了具有代表性的电阻率一深度模型和研究区的井资料计算了视电阻率和相位响应曲线,然后对这些结果的对比分析,评估了利用MT对Kachchh地区地下火成岩沉积成像的合理性。最后,通过对这个地区野外观测的MT资料一维反演证实了我们的讨论。
The magnetotelluric (MT) method has been among the favorite supporting tools for seismic imaging of sub-salt and sub-basalt targets. In this paper we present an example from Kachchh, India (where basaltic rocks overlie Mesozoic sedimentary rocks), and discuss the feasibility of using MT method as an exploration tool in this geological setting. Our results highlight the difference in magnetotelluric response caused by the thin intra-basalt layering. The key issue addressed in this paper is what MT can and cannot provide in such geological settings. First, we compute apparent resistivity and phase response curves using representative resistivity-depth models and borehole data from the study area. Later, we compare these results to assess the plausibility of using MT to image the sub-volcanic sediments at Kachchh. Finally, we substantiate our discussion through one-dimensional inversion of the field observed MT data from this region that exhibits poor sensitivity of MT for thin basalt layers.
引文
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