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Using the Geophysical Inversion of the Gravity Data to Explain the Crustal Structure of South—East China

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Gravity and Geoid

Part of the book series: International Association of Geodesy Symposia ((IAG SYMPOSIA,volume 113))

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Abstract

The geophysical inversion of the gravity data can be used to determine the underground mass density distribution and to explain the Moho undulation as well as the crustal thickness and structure. Although, the inverse gravimetric problem is an ill — posed problem — nounique solution, but from the comprehensive explanation of gravity with deep seismic sounding data and geological data the adequate solution can be obtained.

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References

  • Bott, M. H. P. (1973). Inverse methods in the interpretation of magnetic and gravity anomalies, Methods in computational physics 13, 133–162

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Author information

Authors and Affiliations

  1. Institute of Geophysics, Chinese Academy of Sciences, Beijing, 100101, P. R. China

    Wang Qianshen

Authors
  1. Wang Qianshen
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Editor information

Editors and Affiliations

  1. Department of Mathematical Geodesy and Geoinformatics, Graz University of Technology, Steyrergasse 30, A-8010, Graz, Austria

    Hans Sünkel

  2. Department of Naval Architecture, Marine and Environmental Engineering, University of Trieste, Via Valerio 10, I-34127, Trieste, Italy

    Iginio Marson

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© 1995 Springer-Verlag Berlin Heidelberg

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Qianshen, W. (1995). Using the Geophysical Inversion of the Gravity Data to Explain the Crustal Structure of South—East China. In: Sünkel, H., Marson, I. (eds) Gravity and Geoid. International Association of Geodesy Symposia, vol 113. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-79721-7_30

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  • DOI: https://doi.org/10.1007/978-3-642-79721-7_30

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-540-59204-4

  • Online ISBN: 978-3-642-79721-7

  • eBook Packages: Springer Book Archive

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