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The inner workings of the earthquake cycle: New insight from integrating geophysical observations and microstructures

Dr Laura Gregory (SEE), Prof Sandra Piazolo (SEE), Dr Jessica Hawthorne (Oxford)

Contact email: l.c.gregory@leeds.ac.uk

Slip behaviour at and around faults has been shown to be highly dynamic with variability in behaviour occurring both spatially and temporally.  This exciting project explores the underlying physical processes that lie at the core of this observed dynamic slip behaviour by probing the rock record of fault slip. In this novel project, you will integrate knowledge obtained from seismology, Quaternary fault studies, and quantitative microstructural work to gain an in-depth understanding of the lifecycle of a fault and/or fault zone. Results will be far reaching in fundamental science with direct implications for applied science in terms of earthquake hazard evaluation and prediction.

Earthquakes are one of the main hazards that humanity faces, therefore improving our ability to anticipate how fault zones behave through time is of major importance. However we have still very little understanding of why some faults appear to accommodate different slip modes and others do not, and how and why they cycle between different modes. This project in novel and unique in its cross-disciplinary nature integrating earthquake cycle analysis on real rocks including slip rates using isotopic age dating on fault rocks (Cowie et al., 2017), patterns of geophysical  signals and their link to microstructures from natural and experimental fault rocks. In Leeds we have the rare opportunity of this integration as experts in the respective fields are within the same school. In addition, strong personal links to former Leeds staff members (e.g. Jess Hawthorne, now Oxford University) strengthen this project.

The earthquake cycle typically consists of three periods of fault slip: (1) coseismic, when earthquake rupture occurs at speeds of 1-2 km/sec and results in a huge release of energy during an earthquake, (2) postseismic – during which the fault relaxes and is thought to experience an exponentially decaying rate of stable afterslip, and (3) an interseismic period when the fault is locked and accumulates elastic strain prior to the next earthquake (e.g. Marone, 1998; Barbot et al., 2012). In reality, faults are much more complex and may display an additional range of behaviours associated with steady-state creep, pulsing tremor, and slow slip (e.g. Hawthorne at al., 2016). On timescales covering multiple earthquake cycles, slip behaviour is even more unpredictable. It is now well-recognised that faults can experience periods of enhanced seismic activity with significantly variable recurrence intervals (Figure 1, Weldon et al., 2004; Cowie et al., 2017). It is not known if this range of fault slip behaviour can occur on all faults, or if it is limited to certain types of faults (e.g. plate boundaries vs. continental settings).

Figure 1:(a) Red lines show examples of two different slip histories that have the same long-term slip rate but highly variable recurrence intervals. (b) Demonstrates how cosmogenic nuclides can be used to model variable fault slip, with sampling strategy indicated in the inset of (a), see Cowie et al., (2017)

The mechanical behaviour of a fault zone through time is governed by microphysical and –chemical processes. Proposed important processes included stress induced fracturing and frictional sliding, grain communition, crystal plasticity and pressure solution. So far much of our knowledge of these processes has been gained indirectly by fitting theoretical mechanical behaviour to observed slip behaviour. However, microstructures in fault rocks allow direct derivation of the processes responsible for slip behaviour (e.g. Verbene et al. 2015).  Even though it is clear that the microstructures in fault rocks must hold key answers to the underlying questions of fault slip behaviour, the use of microstructures has been hampered by analytical problems as many structures are extremely fine grained and micron to nanometre scale analysis is necessary.

Recent advances in analytical techniques (e.g. Piazolo et al. 2015, Piazolo et al. 2016) now allows us for the first time to investigate microstructures of fault rocks in unprecedented detail, promising to gain the much needed fundamental knowledge of the mechanochemical processes governing the rheological behaviour of faults through time and space (e.g. Figure 2). To gain such knowledge it is imperative that analysis be conducted in a framework of well constrained case studies, utilizing the natural laboratory of real faults. In order to do so, we must combine the real-world record of the main types of fault behaviour, made on geological scales in time and space, with in-depth microstructural analysis.

Different to laboratory experiments, in the natural scenarios, it is possible to investigate a fault zone over different scale with the background knowledge of its behaviour through time. Such work will augment the experimental work focussing on the physics of one time-step of earthquake slip.

In this project you will collect a set of fault breccia samples “caught in the act” from active fault zones in three potential field areas. One area of focus will be from the Apennines in central Italy, which recently experienced a devastating earthquake sequence that began with an Mw 6.2 resulting in nearly 300 deaths and massive damage and relocation of tens of thousands of people. This regions hosts normal faults that are at varying stages of maturity, and have been show to demonstrate slip rate variability (Figure 3). You will also have the opportunity to investigate normal faults on Crete in Greece and in the basin and range region of the western USA. Target faults in Central Italy and Greece have been extensively studied in terms of their seismic activity and their average Quaternary slip behaviour, and the location of ideal field sites is already known. You will have the unique opportunity to combine knowledge gained through microscopic studies with mesoscale features on these faults, using terrestrial laser scanning datasets detailing the metre-scale fault surface, in collaboration with project partner Prof Ken McCaffrey, from Durham University (e.g. Figure 3c). These faults provide the opportunity to investigate structures from the outcrop to the nanoscale, allowing for a process-oriented analysis of fault rock structure.

Figure 3: Photos of a preserved fault surface from central Italy (a) and the 2016 earthquake rupture (b). (c) shows a terrestrial laser scan (TLS) derived map of fault surface roughness.

Objectives

In this project, the student will work with leading scientists at Leeds (Laura Gregory and Sandra Piazolo) and Oxford (Jess Hawthorne) to integrate latest techniques in characterising fault zone structures in order to understand the dynamics of the physiochemical processes at the core of earthquakes.  The project will address the following questions:

1)      Processes: What physiochemical processes are involved in fast fault slip, creep, and postseismic afterslip?

2)      Recognition: How can geologists recognize prior earthquake cycle behaviour in natural rocks? What is the physical and chemical fingerprint at micro- to meso-scales of different slip behaviour over time?

3)      Effect: What is the mechanical effect of the different processes identified in (1)? What is an appropriate mathematical representation of such dynamic behaviour? Based on the latter, can we predict the timescale and spatial behaviour of fault zones past, present and future?

In order to answers the question posed above, it will be necessary to combine different techniques and approaches.

  1. Investigate the small scale from samples close to or on the fault using the latest field based (e.g. fault zone laser scanning) and analytical (e.g. nanoscale electron microscopy, microtomography) techniques. The field area in central Italy with faults of known Quaternary fault slip rates (e.g. Cowie et al. 2017) will be the initial focus but we anticipate expansion of the field area to Crete (Greece) and/or the western USA.
  2. Develop models of process dynamics derived from field and sample analysis.
  3. Integrate key parameters derived from microstructural analyses into fault slip modelling/physical calculations and compare the results with observed fault behaviours. (e.g. Hawthorne et al. 2016)
  4. Conduct well-constrained experiments of fault slip in the laboratory utilizing the new ice laboratory at University of Leeds followed by subsequent in-depth analysis of experimental samples (e.g. Piazolo et al. 2015).
  5. Develop and test hypotheses linking the observations from the rock record into fault slip behaviours, relying on what we already know from the earthquake and Quaternary records on the faults you have studied.

We expect the balance between these approaches to vary depending on the specific interests of the student. There is the potential to develop novel methods of integrating what you may observe in the rock record with physical models of fault slip; a challenging but important endeavour.

Potential for high impact outcome

Active tectonics and earthquake hazard is a pressing issue facing many countries. We are in a unique position at Leeds to bring together a range of observational, modelling and field approaches to answer important unresolved questions about the earthquake cycles. The research topic has immediate relevance to improving our understanding of the link between faulting and timescale and nature of seismic hazard. There will be ample opportunities to deliver the results of the project at international conferences in addition to UK meetings. Through in-country collaborators, there will be the opportunity to communicate the earthquake hazard to local authorities and civil protection planners.

The project sits in an emerging research field with important fundamental research to be done but also important societal implications. Consequently, we anticipate the project generating several papers being suitable for submission to high impact journals.

Training

You will be part of an active group of researchers and students at SEE that focus on earthquake dynamics including experts in active faulting and microstructural investigation of rocks and minerals Specifically, the student will work under the supervision of Dr. Laura Gregory and Prof Sandra Piazolo within the Tectonics group of the Institute of Geophysics & Tectonics in the School of Earth & Environment at Leeds.  The Institute also hosts the Centre for the Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET http://comet.nerc.ac.uk/) which provides a large group of researchers engaged in active tectonics research with whom the student can interact. This project provides a high level of specialist scientific training in: (i) analysis of seismic data in terms of earthquake cycle, (ii) geological field skills, (iii) Laboratory analysis including state-of-the-art microstructural and –chemical analysis (from outcrop to nanometer scale) (iv) data processing and interpretation of laser scanner data and (v) Deformation modelling related to earthquake cycle. The successful PhD student will have access to a broad spectrum of training workshops put on by the Faculty that include an extensive range from scientific computing through to managing your degree, to preparing for your viva (http://www.emeskillstraining.leeds.ac.uk/).

Student profile

The student should have a strong interest in active tectonics problems, a desire to undertake laboratory and fieldwork overseas, and a strong background in a quantitative science (earth sciences, geophysics, geology, physics, natural sciences). Willingness and excitement for taking up the challenge to work at the boundary of geophysics, mechanics and microstructural analysis utilizing a combination of technique (field analysis, in-depth microstructural analysis, experiments and/or numerical modelling) is a prerequisite.

References

Barbot, S., N Lapusta, and JP Avouac (2012). Under the hood of the earthquake machine: toward predictive modelling of the seismic cycle. Sciece 336, pp 707-710, doi: 10.1126/science.1218796

Cowie, PA, Phillips, RJ, Roberts, GP, McCaffrey, K, Zijerveld, LJJ, Gregory, LC, Faure Walker, J, Wedmore, LNJ, Dunai, TJ, Binnie, SA, Freeman, SPHT, Wilcken, K, Shanks, RP, Huismans, RS, Papanikolaou, I, Michetti, AM, and Wilkinson, M (2017). Orogen-scale uplift I nthe central Italian Apennines drives episodic behaviour of earthquake faults. Scientific Reports 7:44858, doi: 10.1038/srep44858.

Delle Piane, C., Piazolo, S., Timms, N. E., Luzin, V., et al. (in press). Sub-seismic slip in nano calcite fault gouge generates amorphous carbon and crystallographic texture at low temperature. Geology

Dunham, EM, D Belanger, L Cong, and JE Kozdon (2011). Earthquake ruptures with strongly rate-weakening friction and off-fault plasticity, part 2: Nonplanar faults.” Bulletin of the Seismological Society of America 101 (5), pp 2296–2307, doi: 10.1785/0120100076

Hawthorne, JC, Boxtock, MG, Royer, AA, and Thomas, AA (2016). Variations in slow slip moment rate associated with rapid tremor reversals in Cascadia. Geochemistry, Geophysics, Geosystems 17, pp 4899-4919, doi: 10.1002/2016GC006489.

Marone, C (1998). The effect of loading rate on static friction and the rate of fault healing during the earthquake cycle. Nature 391, pp 69-72.

Piazolo S; La Fontaine A; Trimby P; Harley S; Yang L; Armstrong R; Cairney JM (2016) Deformation-induced trace element redistribution in zircon revealed using atom probe tomography, Nature Communications, 7, . doi: 10.1038/ncomms10490

Piazolo S; Montagnat M; Grennerat F; Moulinec H; Wheeler J (2015) Effect of local stress heterogeneities on dislocation fields: Examples from transient creep in polycrystalline ice, Acta Materialia, 90, pp.303-309. doi: 10.1016/j.actamat.2015.02.046

Weldon, R, Scharer, K, Fumal, T, and Biasi, G (2004). Wrightwood and the earthquake cycle: what a long recurrence record tells us about how faults work. GSA Today 14 (9), pp 4-10, doi: 10.1130/1052-5173(2004)0142.0CO;2.

Related undergraduate subjects:

  • Earth science
  • Geological science
  • Geology
  • Geophysical science
  • Geophysics
  • Geoscience
  • Physical science