Thomas B. Phillips
The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling
Phillips, Thomas B.; Naliboff, John B.; McCaffrey, Ken J.W.; Pan, Sophie; van Hunen, Jeroen; Froemchen, Malte
Authors
John B. Naliboff
Professor Kenneth Mccaffrey k.j.w.mccaffrey@durham.ac.uk
Head of Department
Sophie Pan
Professor Jeroen Van Hunen jeroen.van-hunen@durham.ac.uk
Professor
Malte Froemchen malte.froemchen@durham.ac.uk
PGR Student Doctor of Philosophy
Abstract
The lateral distribution of strength within the crust is non-uniform, dictated by crustal lithology and the presence and distribution of heterogeneities within it. During continental extension, areas of crust with distinct lithological and rheological properties manifest strain differently, influencing the structural style, geometry, and evolution of the developing rift system. Here, we use 3D thermo-mechanical models of continental extension to explore how pre-rift upper-crustal strength variations influence rift physiography. We model a km volume containing 125 km wide domains of mechanically “strong” and “weak” upper crust along with two reference domains, based upon geological observations of the Great South Basin, New Zealand, where extension occurs parallel to the boundaries between distinct geological terranes. Crustal strength is represented by varying the initial strength of 5 km3 blocks. Extension is oriented parallel to the domain boundaries such that each domain is subject to the same 5 mm yr−1 extension rate. Our modelling results show that strain initially localises in the weak domain, with faults initially following the distribution of initial plastic strain before reorganising to produce a well-established network, all occurring in the initial 100 kyr. In contrast, little to no localisation occurs in the strong domain, which is characterised by uniform strain. We find that although faults in the weak domain are initially inhibited at the terrane boundaries, they eventually propagate through and “seed” faults in the relatively strong adjacent domains. We show characteristic structural styles associated with strong and weak crust and relate our observations to rift systems developed across laterally heterogeneous crust worldwide, such as the Great South Basin, New Zealand, and the Tanganyika Rift, East Africa.
Citation
Phillips, T. B., Naliboff, J. B., McCaffrey, K. J., Pan, S., van Hunen, J., & Froemchen, M. (2023). The influence of crustal strength on rift geometry and development – insights from 3D numerical modelling. Solid Earth, 14(4), 369-388. https://doi.org/10.5194/se-14-369-2023
Journal Article Type | Article |
---|---|
Acceptance Date | Mar 8, 2023 |
Online Publication Date | Apr 5, 2023 |
Publication Date | 2023 |
Deposit Date | May 16, 2023 |
Publicly Available Date | May 16, 2023 |
Journal | Solid Earth |
Print ISSN | 1869-9510 |
Electronic ISSN | 1869-9529 |
Publisher | European Geosciences Union |
Peer Reviewed | Peer Reviewed |
Volume | 14 |
Issue | 4 |
Pages | 369-388 |
DOI | https://doi.org/10.5194/se-14-369-2023 |
Public URL | https://durham-repository.worktribe.com/output/1174959 |
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Copyright Statement
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
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