کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
10121350 | 1641619 | 2005 | 18 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
3D modelling of electrical anisotropy from electromagnetic array data: hypothesis testing for different upper mantle conduction mechanisms
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فیزیک زمین (ژئو فیزیک)
پیش نمایش صفحه اول مقاله
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چکیده انگلیسی
Upper mantle electrical conductivities provide, besides seismic velocities or thermal diffusivities, another source of information on upper mantle structure and composition. We present the results of a long-period magnetotelluric dataset, consisting of 64 sites covering an area of 300kmÃ400âkm in central Germany, mapping electrical conductivities at the base of the lithosphere. To seperate the effect of crustal and upper mantle structures, we interprete the obtained dataset by 3D conductivity modelling. We observe high conductivities and anisotropies at asthenospheric upper mantle depth, with main bulk conductivities of â¼ 1-2âS/m in west-east and â¼4Ã10â3âS/m in north-south direction, differing by about two orders of magnitude. In comparing with results from laboratory measurements on electrical conductivites for various conduction mechanisms we are able to confine the conduction mechanisms possibly dominating at these depths. With melt volume fractions of 1% only partial melt can be excluded as origin of the high upper mantle conductivities. Instead conductivity enhancement due to hydrogen diffusion along the olivine [1â0â0]-axis is favoured as the dominant conduction mechanism at the base of the lithosphere.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Physics of the Earth and Planetary Interiors - Volume 149, Issues 3â4, 15 April 2005, Pages 225-242
Journal: Physics of the Earth and Planetary Interiors - Volume 149, Issues 3â4, 15 April 2005, Pages 225-242
نویسندگان
A. Gatzemeier, M. Moorkamp,