| 波西米亚块体西部长周期电磁研究(英文) |
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| 引用本文： | V.Cerv J.Pek 等. 波西米亚块体西部长周期电磁研究(英文)[J]. 地震地质, 2001, 23(2): 166-177. DOI: ISSN:0253-4967.0.2001-02-006 |
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| 作者姓名： | V.Cerv J.Pek 等 |
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| 作者单位： | 1. 捷克共和国科学院地球物理研究所,
2. 捷克共和国科学院地球物理研究所,布拉格 |
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| 摘 要： | 在波西米亚块体西南部做了一条长周期电磁剖面 ,它靠近德国超深钻的位置。用一个二维合成模型对数据做了大体的拟合 ,模型走向东西 ,近地表盖层高度地不均匀畸变。畸变层显示强烈的各向异性 ,优势电导方向为NW -SE至NNW -SSE。讨论了深部区域结构的几个不同的模型 ,其中一个模型可以解释由MT和GDS数据显示的主方向的偏差 ,还讨论了沿特别剖面得到的结果与区域地电结构的关系
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| 关 键 词： | 电磁 波西米亚块体 地电结构 |
LONG PERIOD MAGNETOTELLURIC STUDIES IN THE WESTERN PART OF THE BOHEMIAN MASSIF |
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| V.ACˇGerv,J.Pek,O.Praus. LONG PERIOD MAGNETOTELLURIC STUDIES IN THE WESTERN PART OF THE BOHEMIAN MASSIF[J]. Seismology and Geology, 2001, 23(2): 166-177. DOI: ISSN:0253-4967.0.2001-02-006 |
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| Authors: | V.ACˇGerv J.Pek O.Praus |
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| Abstract: | A long period magnetotelluric profile in SW Bohemia, in the western part of the Bohemian Massif, close to the KTB deep borehole in Oberpfalz, Germany, is studied. The data roughly fit a composite model of a 2D regional structure, striking E-W, overlaid by a layer of highly distorting near-surface inhomogeneities. The distorting layer displays large anisotropy with preferred conductivity in NW-SE to NNW-SSE direction. Several variants of 2D models for the deep regional structure are discussed, including an anisotropic model which can qualitatively explain the discrepancy of the principal directions indicated by the MT and GDS data. The relation of the results obtained along the particular profile to the regional geoelectrical background is studied. |
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| Keywords: | Magnetotelluric Bohemian Massif Geoelectrical structure |
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