Publication details for Dr Nicola De PaolaDe Paola, N., Holdsworth, R.E., Collettini, C., McCaffrey, K.J.W. & Barchi, M.R. (2007). The structural evolution of dilational step-overs in transtensional zones. Geological Society, London. Special Publications 290: 433-445.
- Publication type: Journal Article
- ISSN/ISBN: 978-1-86239-238-0
- DOI: 10.1144/SP190.17
- Further publication details on publisher web site
- Durham Research Online (DRO) - may include full text
Author(s) from Durham
We propose a theoretical model, supported by a field study, to describe the patterns of fault/fracture meshes formed within dilational step-overs developed along faults accommodating regional scale wrench-dominated transtension. The geometry and kinematics of the faulting in the dilational step-overs is related to the angle of divergence (), and differs from the patterns traditionally predicted in dilation zones associated with boundary faults accommodating strike-slip displacements (where = 0°). For low values of oblique divergence (< 30°) and low strain, the fault/fracture mesh comprises interlinked tensile fractures and shear-extensional planes, consistent with wrench-dominated transtension. At higher values of strain, a switch occurs from wrench- to extension-dominated transtension leading to the reactivation and/or disruption of the early formed structures. These structural processes lead to the development of a geometrically complex and kinematically heterogeneous fault pattern, which may affect and/or perturb the development of a through-going fault linking and facilitating the slip transfer between the two overlapping fault segments. As a result, dilational step-over zones will tend to form long-lived sites of localised extension and subsidence in regional transtensional tectonic settings. Cyclic increases/decreases of structural permeability will be related to slip on the major boundary faults that control the distribution of fluid flow paths and, consequently, the long and short term structural evolution of these sites. Our model also predicts complex and more realistic sub-surface fluid migration pathways relevant to our current understanding of hydrothermal ore deposits and hydrocarbon migration and storage.