Gutenberg Open


Personen: Iacopini, D. (Autor) 
Passchier, Cornelis Willem (Autor) 
Köhn, Daniel (Autor) 
Carosi, R. (Autor) 
Titel: Fabric attractors in general triclinic flow systems and their application to high strain shear zones : a dynamical system approach
Quelle: Journal of structural geology. Bd. 29. H. 2. S. 298 - 317
Erscheinungsjahr:    2007
ISBN / ISSN: 0191-8141
URL der Originalveröffentlichung doi:10.1016/j.jsg.2006.10.002
Zeitschriftenaufsatz Zeitschriftenaufsatz
Sprache: Englisch
Open Access:
Person der Universität:    Passchier, Cornelis Willem  In UnivIS suchen ; Köhn, Daniel  In UnivIS suchen 
Einrichtung: Institut für Geowissenschaften
DDC-Sachgruppe:    Geowissenschaften
DFG-Fachgebiet: Geologie und Paläontologie
ID: 16336  Universitätsbibliothek Mainz
Informationen zu den Nutzungsrechten unserer Inhalte Informationen zu den Nutzungsrechten unserer Inhalte
Abstract: High strain zones may deform by flow with a triclinic symmetry. This paper describes triclinic flow in a reference frame where Instantaneous Stretching Axes (ISA) are fixed. The operation of triclinic flow is described in two ways: first in terms of flow and the nature of flow eigenvectors and in the second part of the paper in terms of finite strain. In monoclinic flow, at least one of the eigenvectors of the flow coincides with one of the ISA and one or two of the eigenvectors act as attractors of foliation or lineation elements. In triclinic flow some flow eigenvectors are undefined since the two largest eigenvalues (controlling the flow) are imaginary. Imaginary eigenvalues are particularly common at high kinematic vorticity and within flow with deviation of the vorticity vector of more than 20° from one of the ISA. Strong deviation from monoclinic flow is therefore possible, but this will not produce permanent foliations or lineations. For triclinic flow that does produce permanent fabrics, the angle between ISA and the fabric is so small that it is unlikely that it can be recognised in nature. A discussion of the potential application of such results within real shear zones is presented.
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