Parasitic folds with wrong vergence: How pre-existing geometrical asymmetries can be inherited during multilayer buckle folding. (June 2016)
- Record Type:
- Journal Article
- Title:
- Parasitic folds with wrong vergence: How pre-existing geometrical asymmetries can be inherited during multilayer buckle folding. (June 2016)
- Main Title:
- Parasitic folds with wrong vergence: How pre-existing geometrical asymmetries can be inherited during multilayer buckle folding
- Authors:
- Frehner, Marcel
Schmid, Timothy - Abstract:
- Abstract: Parasitic folds are typical structures in geological multilayer folds; they are characterized by a small wavelength and are situated within folds with larger wavelength. Parasitic folds exhibit a characteristic asymmetry (or vergence) reflecting their structural relationship to the larger-scale fold. Here we investigate if a pre-existing geometrical asymmetry (e.g., from sedimentary structures or folds from a previous tectonic event) can be inherited during buckle folding to form parasitic folds with wrong vergence. We conduct 2D finite-element simulations of multilayer folding using Newtonian materials. The applied model setup comprises a thin layer exhibiting the pre-existing geometrical asymmetry sandwiched between two thicker layers, all intercalated with a lower-viscosity matrix and subjected to layer-parallel shortening. When the two outer thick layers buckle and amplify, two processes work against the asymmetry: layer-perpendicular flattening between the two thick layers and the rotational component of flexural flow folding. Both processes promote de-amplification and unfolding of the pre-existing asymmetry. We discuss how the efficiency of de-amplification is controlled by the larger-scale fold amplification and conclude that pre-existing asymmetries that are open and/or exhibit low amplitude are prone to de-amplification and may disappear during buckling of the multilayer system. Large-amplitude and/or tight to isoclinal folds may be inherited and developAbstract: Parasitic folds are typical structures in geological multilayer folds; they are characterized by a small wavelength and are situated within folds with larger wavelength. Parasitic folds exhibit a characteristic asymmetry (or vergence) reflecting their structural relationship to the larger-scale fold. Here we investigate if a pre-existing geometrical asymmetry (e.g., from sedimentary structures or folds from a previous tectonic event) can be inherited during buckle folding to form parasitic folds with wrong vergence. We conduct 2D finite-element simulations of multilayer folding using Newtonian materials. The applied model setup comprises a thin layer exhibiting the pre-existing geometrical asymmetry sandwiched between two thicker layers, all intercalated with a lower-viscosity matrix and subjected to layer-parallel shortening. When the two outer thick layers buckle and amplify, two processes work against the asymmetry: layer-perpendicular flattening between the two thick layers and the rotational component of flexural flow folding. Both processes promote de-amplification and unfolding of the pre-existing asymmetry. We discuss how the efficiency of de-amplification is controlled by the larger-scale fold amplification and conclude that pre-existing asymmetries that are open and/or exhibit low amplitude are prone to de-amplification and may disappear during buckling of the multilayer system. Large-amplitude and/or tight to isoclinal folds may be inherited and develop type 3 fold interference patterns. Graphical abstract: Highlights: We model multilayer buckle folding with a predefined geometrical asymmetry. If inherited, the asymmetry resembles a parasitic fold with wrong vergence. In the larger-scale fold, layer-perpendicular flattening and flexural flow occurs. Both work against the asymmetry, leading to de-amplification and unfolding. Hence, a pre-existing wrong vergence is difficult to inherit during buckling. … (more)
- Is Part Of:
- Journal of structural geology. Volume 87(2016:Jun.)
- Journal:
- Journal of structural geology
- Issue:
- Volume 87(2016:Jun.)
- Issue Display:
- Volume 87 (2016)
- Year:
- 2016
- Volume:
- 87
- Issue Sort Value:
- 2016-0087-0000-0000
- Page Start:
- 19
- Page End:
- 29
- Publication Date:
- 2016-06
- Subjects:
- Parasitic folds -- Buckle folds -- Fold vergence -- Asymmetric folds -- Structural inheritance -- Finite-element method
Geology, Structural -- Periodicals
Géomorphologie structurale -- Périodiques
Geology, Structural
Periodicals
551.805 - Journal URLs:
- http://www.sciencedirect.com/science/journal/01918141 ↗
http://www.elsevier.com/journals ↗ - DOI:
- 10.1016/j.jsg.2016.04.004 ↗
- Languages:
- English
- ISSNs:
- 0191-8141
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 5066.878000
British Library DSC - BLDSS-3PM
British Library HMNTS - ELD Digital store - Ingest File:
- 9050.xml