Studio delle deformazioni in una coltre argillosa dovute a movimenti lungo faglie nel substrato

Deformations in clay-cover transferred from basement faulting

Authors

  • Carlo Bosi Centro di Studio per la Geologia Tecnica del CNR – Roma, Italy Author
  • Giancarlo Cappellari Centro di Studio per la Geologia Tecnica del CNR – Roma, Italy Author
  • Mario Ottaviani Istituto di Geologia Applicata, Università di Roma, Roma, Italy Author

Keywords:

Shallow tectonics, Faults, Mechanic properties

Abstract

The problem of how a vertical movement along a fault in the base-rock is transferred to the surface through clay layers has been studied. The study has been carried out on the basis of a known geological situation using the finite element method. A non-linearly elastic behavior has been assumed for the clay. Slips of 10 to 100 cm have been considered at the fault. It has been found out that the entire slip is transferred to the surface as a very gently folding and that there is no failure propagating in the clay layers above the base rock.

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Published

2024-07-19

Issue

Section

Research and review papers

How to Cite

Bosi, C., Cappellari, G., & Ottaviani, M. (2024). Studio delle deformazioni in una coltre argillosa dovute a movimenti lungo faglie nel substrato: Deformations in clay-cover transferred from basement faulting. Geografia Fisica E Dinamica Quaternaria, 2(1), 29-34. https://www.gfdq.glaciologia.it/index.php/GFDQ/article/view/1029

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