Asymmetric fold development in the Variscan nappes of Central Sardinia (Italy).

Rodolfo Carosi , David Iacopini, Chiara Montomoli

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

The Meana Sardo Unit (MSU) shows trains of asymmetric SW-verging folds, developed during the thickening stage and nappe development of the Variscan belt in Sardinia. The geometry of the folds and the finite strain analysis results in the hinge of a kilometric fold give information on the folding mechanisms. The strain and the geometry of the fold have been compared to a 2-D geometrical model of development of homogenous non-coaxial deformation. The results show that initial layer parallel shortening and fold amplification followed by simple shearing or by coeval simple and pure shearing, linked to the overthrust of the Low Grade Metamorphic Complex of Barbagia onto MSU, are able to explain the observed fold geometries and finite strain values.
Original languageEnglish
Pages (from-to)939-949
Number of pages11
JournalComptes Rendus. Ge´oscience
Volume336
Issue number10
Early online date19 May 2004
DOIs
Publication statusPublished - Jul 2004

Fingerprint

Sardinia
Hercynian orogeny
nappe
Italy
fold
Shearing
Geometry
Hinges
geometry
shortenings
Amplification
strain analysis
train
folding
amplification

Keywords

  • asymmetric folds
  • folding mechanism
  • finite strain
  • Variscan basement
  • Paleozoic
  • Sardinia

Cite this

Asymmetric fold development in the Variscan nappes of Central Sardinia (Italy). / Carosi , Rodolfo; Iacopini, David; Montomoli, Chiara.

In: Comptes Rendus. Ge´oscience, Vol. 336, No. 10, 07.2004, p. 939-949.

Research output: Contribution to journalArticle

Carosi , Rodolfo ; Iacopini, David ; Montomoli, Chiara. / Asymmetric fold development in the Variscan nappes of Central Sardinia (Italy). In: Comptes Rendus. Ge´oscience. 2004 ; Vol. 336, No. 10. pp. 939-949.
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