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Deciphering magmatic and tectonic processes at the University of East Anglia
Primary supervisor: Dr. Zoja Vukmanovic
Scientific background:
Stratigraphic intrusions represent natural laboratories frozen in time, providing us with an opportunity to study how magma cools and differentiates, and how precious minerals concentrate to form ore deposits. The ore deposits found in these interventions are crucial to achieving a carbon-neutral future.
However, these natural laboratories are often affected by tectonic events, resulting in overprinting of primary magmatic processes. Complex geological history modifies the mineral chemistry and microstructure of rocks. The study area, Bjerkreim-Sokndal (BKS) in southern Norway, provides ample evidence of deformation, representing the best place to study both magmatic and tectonic processes. Apart from ilmenite (Ti) deposits, BKS has recently been identified as the most promising phosphate rock resource in Norway. The main goal of this project is to decipher between magma microstructure and post-emplacement to understand the formation and evolution of intrusion. In addition, how has deformation affected the mineralization of the ore found in the BKS in terms of its microstructure and geochemistry.
Research methodology:
The main objectives of this project are 1) to distinguish between magma microstructure and post-emplacement microstructure, and 2) to determine the effect of deformation on the geochemistry of the major rock-forming minerals. Accomplishing both goals will entail a combination of: 1) fieldwork and petrology; 2) Electron backscatter diffraction analysis (University of Cambridge); 3) Magnetic texture analysis (University of St Andrews) and 4) Mineralogy (Norwegian Geological Survey, Trondheim). The first year field trip (two weeks) will be carried out in Bjerkreim Lobe of the BKS storming area.
an exercise:
The individual will receive customized training in (1) digital and traditional mapping techniques (all supervisors); (2) microscopic analysis by electron backscatter diffraction (EBSD), SEM, transmitted and reflected light microscopy (Vukmanovich); (3) Magnetic rock techniques (McCarthy). Training will be largely individual, working closely with supervisors in their own modern laboratory facilities.
Person specifications:
We are looking for applicants who have a Bachelor’s/Master’s degree in Geology or a related discipline, enthusiasm for field work and a strong drive to succeed. We encourage applications from individuals who would like to shape this project around their research interests.
Entry requirements:
At least a UK BA (Hons) equivalency of 2:1. English language requirements (Faculty of Science equivalent: IELTS 6.5 overall, 6 in each category).
Study method:
Full time
Start date:
October 1, 2026
Financing information
ARIES Scholarships are governed by UKRITerms and Conditions. Successful candidates who meet UKRI’s eligibility criteria will be awarded a fully-funded scholarship, which covers fees, a maintenance stipend (£20,780 per annum for 2025/26) and a Research Training and Support Grant (RTSG). A limited number of scholarships are available to international applicants, with the difference between ‘national’ and ‘international’ fees waived by the registered university. However, please note that ARIES funding does not cover additional costs associated with moving to and living in the UK, such as visa costs or additional health fees.
https://www.jobs.ac.uk/job/DPA002/phd-studentship-magma-emplacement-and-its-evolution-deciphering-between-magmatic-and-tectonic-processes/



