Separation of sources and 3D inversion of gravity and magnetic data for the Thuringian Basin, Germany

Authors

  • Ilya PRUTKIN Institute of Earth Sciences, Jena University
  • Gerhard JENTZSCH Institute of Earth Sciences, Jena University
  • Thomas JAHR Institute of Earth Sciences, Jena University

DOI:

https://doi.org/10.2478/v10126-012-0005-8

Keywords:

potential field methods, 3D inversion, pseudo-gravity, sedimentary basin

Abstract

We propose a novel methodology for separation of potential field sources and its 3D inversion. New approaches are developed to separate sources: i) in depth using a succession of upward and downward continuation; ii) in the lateral direction by means of approximation with the field of 3D line segments; iii) according to density and magnetization contrast based on pseudo-gravity calculation. Our original inversion algorithms allow the recovery of unknown 3D geometry both for a restricted body of arbitrary shape and for a contact surface. For the first time, we apply our algorithms to joint inversion of gravity and magnetic data for a large area (the Thuringian Basin in central Germany). We separate in depth sources of both gravitational and magnetic anomalies for the whole territory of Thuringia and compare corresponding components. A 3D model of the main sources is presented based on approximation with 3D line segments and their further transforming into a restricted body or a contact surface with the same field.

Author Biographies

  • Ilya PRUTKIN, Institute of Earth Sciences, Jena University

    Burgweg 11, 07749 Jena, Germany

  • Gerhard JENTZSCH, Institute of Earth Sciences, Jena University

    Burgweg 11, 07749 Jena, Germany

  • Thomas JAHR, Institute of Earth Sciences, Jena University

    Burgweg 11, 07749 Jena, Germany

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Published

2012-06-30

Issue

Section

original research papers

How to Cite

PRUTKIN, I., JENTZSCH, G., & JAHR, T. (2012). Separation of sources and 3D inversion of gravity and magnetic data for the Thuringian Basin, Germany. Contributions to Geophysics and Geodesy, 42(2), 119-132. https://doi.org/10.2478/v10126-012-0005-8