The relationship between normal drag, relay ramp aspect ratio and fault zone structure

Author:

Childs C.1,Manzocchi T.1,Nicol A.23,Walsh J. J.1,Soden A. M.1,Conneally J. C.1,Delogkos E.1

Affiliation:

1. Fault Analysis Group, School of Earth Sciences, University College Dublin, Belfield, Dublin 4, Ireland

2. GNS Science, Lower Hutt, New Zealand

3. Present address: University of Canterbury, Christchurch, New Zealand

Abstract

AbstractThe boundaries between pairs of adjacent fault segments within normal fault arrays define a spectrum of structures, from relay ramps where the length of overlap between the fault segments is much larger than the separation, through low aspect ratio (overlap/separation) relay ramps and ultimately to underlapping fault segments. Where fault segments underlap, transfer of displacement between them is accommodated by a connecting monocline. When displacement increases and a through-going fault forms, relay ramps are preserved as fault-bounded zones of elevated bed dip and monoclines are preserved as areas of normal drag. Therefore, the orientation and magnitude of bed dips within and adjacent to a fault zone, and the numbers of segments seen on a cross-section through it, depend largely on the aspect ratios of relay ramps in the initial fault array. The aspect ratio of relay ramps varies between different fault systems. An analysis of the geometry of 512 relay ramps from 13 different fault systems suggests that the main controls on aspect ratio are the strength of the sequence at the time of faulting and the underlying structure.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference56 articles.

1. Effect of mechanical interaction on the development of strike-slip faults with echelon patterns

2. Conneally J.C. 2014. The kinematics and geometry of segment boundaries on normal faults. PhD thesis, University College Dublin.

3. Contrasting origins of breached relay zone geometries;Journal of Structural Geology,2014

4. Kinematic analysis of faults in a physical model of growth faulting above a viscous salt analogue

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