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  Deformation before and after large earthquakes for seismic hazard assessment (BIEL_U21SCIEC)


   School of Environmental Sciences

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  Dr Lidong Bie, Dr J Johnson  No more applications being accepted  Competition Funded PhD Project (Students Worldwide)

About the Project

Primary Supervisor - Dr Lidong Bie 

Secondary Supervisor - Dr Jessica Johnson

Secondary Supervisor - Dr Zoe Mildon

Secondary Supervisor - Prof Andreas Rietbrock

Scientific background 

In earthquake science, a fundamental yet challenging objective is to find promising precursors that can warn people well in advance of devastating earthquakes. Recent advances in seismic and geodetic observing tools suggest transient deformation caused by processes such as slow slip accompanied by migrating seismicity may be observable weeks to months prior to large earthquakes in subduction zones. In addition, transient deformation is observed at various spatial and temporal scales following earthquakes, indicating complex stress relaxation on the fault and surrounding materials. Establishing the temporal and spatial evolution of deformation is therefore of particular importance for understanding fault behaviour before and after large earthquakes.   

Research methodology 

The project will initially study the East Kunlun fault zone in the north-eastern part of the Tibetan Plateau, focusing on the magnitude 7.4 Maduo earthquake that occurred on 22 May 2021. This earthquake is the strongest in the eastern part of the Plateau since the 2008 Sichuan earthquake and one of the most intensely felt in recent memory. 

This project aims to answer questions such as: 

·      Is the transient deformation rate constant before the earthquake? 

·      How does the deformation rate vary across neighbouring faults before the earthquake? 

·      How does the deformation after the earthquake evolve and what is the likely process controlling the evolvement? 

·      How are the stresses on neighbouring faults affected by the Maduo earthquake and processes after it? 

The student will apply radar interferometry (InSAR) to map surface displacement and generate deformation time-series. The student will develop finite element models to explain the observations, including investigating stress relaxation mechanisms after the earthquake and stress loading on neighbouring faults. 

Training 

Training will be given in InSAR data processing, finite element modelling, Coulomb stress modelling and geophysical hazard processes. The student will visit Germany (subject to restrictions) to work with Prof. Andreas Rietbrock for training on seismic methods.  

For more information on the supervisor for this project, please visit the UEA website www.uea.ac.uk

The start date is 1 October 2022

Entry requirements: Acceptable first degree 2:1 in geology, geophysics, computer sciences or environmental sciences with an interest in geohazards.


Geography (17) Geology (18)

Funding Notes

This PhD project is in a competition for a Faculty of Science funded studentship. Funding is available to UK applicants and comprises ‘home’ tuition fees and an annual stipend of £15,609 for 3 years. Applicants who are not eligible for home tuition fees are welcome to apply but they will be required to fund the difference between home and international tuition fees (which for 2021-22 are detailed on the University’s fees pages at https://www.uea.ac.uk/about/university-information/finance-and-procurement/finance-information-for-students/tuition-fees. Please note tuition fees are subject to an annual increase).

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