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Interpretation of gravity and magnetic data with geological constraints for 3D structure of the Thuringian Basin, Germany
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文摘
New methodology for 3D inversion is applied to gravity and magnetics in Thuringia. Short, intermediate and long wavelengths are inverted separately. We diminish degree of non-uniqueness by interpretation using geological constraints. Our model of intermediate sources includes density interface and three intrusions. We study 3D topography of crystalline basement and salt tectonics for local areas.

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