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Compressional Tectonics and the Balancing of Crustal Cross Sections

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Joint Interpretation of Geophysical and Geological Data Applied to Lithospheric Studies

Part of the book series: NATO ASI Series ((ASIC,volume 338))

Abstract

Balancing is checking for restorability of structure cross sections to pre-deformational state. Its present forms are based on a supracrustal strain type which consists of little more than translation and layer-parallel simple shear. A simplified form of supracrustal balancing can be applied to the Moho and to the brittle upper crust, but not to the viscous middle crust. There are no rigorous methods of correlation across the viscous gap. The conceptual approach must be based on additional geodynamics, such as visco-elastic load modelling, the search for specific elastic wavelengths, and thermal modelling of decaying lithospheric disturbances.

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Authors and Affiliations

  1. The Anschutz Corporation, 2400 Anaconda Tower, Denver, CO, 80202, USA

    Dietrich Roeder

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  1. Dietrich Roeder
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  1. Geophysical Department, Freie Universität Berlin, Berlin, Germany

    P. Giese

  2. The Anschutz Corporation, Denver, Colorado, USA

    D. Roeder

  3. Istituto di Miniere e Geofisica Applicata, Università Trieste, Trieste, Italy

    R. Nicolich

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Roeder, D. (1991). Compressional Tectonics and the Balancing of Crustal Cross Sections. In: Giese, P., Roeder, D., Nicolich, R. (eds) Joint Interpretation of Geophysical and Geological Data Applied to Lithospheric Studies. NATO ASI Series, vol 338. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-3590-0_8

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  • DOI: https://doi.org/10.1007/978-94-011-3590-0_8

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