On the development of kink-bands: A case study in the Westasturian-Leonese Zone (Variscan belt, NW Spain)

Jesús Aller,Nilo C Bobillo-Ares,Fernando Bastida

doi:10.1051/bsgf/2020003

Jesús Aller, Nilo C Bobillo-Ares + Show 1 more

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https://doi.org/10.1051/bsgf/2020003

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Abstract

A field analysis of kink bands developed in slates from three areas (Grandas, Boal and Luarca areas) of the Westasturian-Leonese Zone (Iberian Variscan belt) is presented. The analysis of the main parameters that characterize the geometry of the studied kink bands shows that those of the Grandas and Luarca areas exhibit a different evolution than those of the Boal area. In this latter area, the interlimb angle of the kink bands has lower values than those developed in the former areas and it involves rotation of the foliation inside and outside the band. In the areas with higher bulk shortening associated with the development of kink bands, chevron folds formed by juxtaposition of kink bands. Slip between folia and their rotation was probably the dominant mechanism in the formation of the kink bands, as deduced from the different values of the angle between the kink plane and the foliation inside (φK) and outside (φ) the band, and the occurrence of fractures along the kink planes and small steps between folia cross-cutting these fractures planes. The fractures along the kink planes prevented subsequent hinge migration. Geometrical analysis of kink bands formed by slip between folia and their rotation provides an estimation of the changes in area and thickness, and the strain inside the kink band. For angles of folia rotation ψ < 50°, the ratio between the strain ellipse axes is < 3 inside the band; this ratio is almost independent of the orientation of the kink planes with respect to the foliation outside the band (angle φ).

Highlights

Kink bands are strongly asymmetric angular or subangular folds, whose geometry is that of a monoclinal step (Fig. 1)
They have been described in diverse lithologies, kink bands typically develop in laminated materials with a previous well-marked anisotropy
Late Variscan kink bands have been studied in three areas of the Westasturian-Leonese Zone (Grandas, Boal and Luarca areas)

Summary

Introduction

Kink bands are strongly asymmetric angular or subangular folds, whose geometry is that of a monoclinal step (Fig. 1). They have been described in diverse lithologies, kink bands typically develop in laminated materials (mainly shale, slates or schist) with a previous well-marked anisotropy (usually slaty cleavage or schistosity). The term “kink band” has been generalized to refer indistinctly to the band or to the whole fold. Anderson (1964) defined two angles, a and b, for the geometrical analysis of kink bands; these angles were named f and fK, respectively, by Paterson and Weiss (1966), which is the terminology used here (Fig. 1).

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