Applications are invited for a post-doctoral research associate (PDRA) position
within the mineral magnetism group of the Department of Earth Sciences,
University of Cambridge. The position is funded by the ERC grant
“Nanopaleomagnetism: a new multiscale approach to paleomagnetic analysis of geological
materials”, a brief description of which is given below. Funding is available
for 3 years in the first instance. Successful applicants will hold a PhD on
taking up the post.
The PDRA project will focus on the application of a dual-beam focussed ion beam
(FIB) workstation to perform 3D slice-and-view tomography of natural samples.
The person appointed will use facilities located in the Department of Materials
Science to study the positions, sizes, shapes, compositions and
crystallographic orientations of magnetic particles embedded in silicate hosts
using a combination of slice-and-view tomography, electron backscattered
diffraction (EBSD) and energy dispersive X-ray analysis (EDX). We seek
candidates with a strong background in electron microscopy and specific
experience with using FIB techniques. Experience with EDX, EBSD and tomography
would be an advantage. It is not necessary to have a background in either Earth
sciences or magnetism, and we invite suitably experienced candidates from any
area of the physical sciences. The successful candidate will have a track
record of publication in peer-reviewed journals, will have good communication
skills and have demonstrated the capacity to perform independent research.
For full details see http://www.jobs.cam.ac.uk/job/1523/
Interested candidates should contact Dr. Richard Harrison (rjh40@esc.cam.ac.uk)
for more information about the project and formal application procedures.
General description of the ERC project:
Adopting cutting-edge techniques from physics and materials science,
Nanopaleomagnetism aims to perform paleomagnetic measurements at submicron
length scales, enabling primary magnetic signals to be extracted from ancient
and severely altered geological materials. 3D measurements of the volume, shape
and spacing of all magnetic particles within a microscale region of interest
will be made using a ‘dual beam’ focussed ion beam workstation. Combined with
high-resolution paleomagnetic measurements and nanometre/nanosecond
electron/X-ray magnetic imaging, nanopaleomagnetism will, for the very first
time, be able to characterise the magnetic properties of geological materials
at fundamental length scales and time scales. The nanoscale measurements will
enable us to capture the essential physics of the remanence acquisition process
and to explore magnetic behaviour ‘in silico’, allowing predictions to be made
that can be tested directly against experimental observations at all length
scales. Sample-return missions to asteroids, comets, moons and planets will
soon provide unprecedented opportunities for extraterrestrial paleomagnetism.
Nanopaleomagnetism will provide the methodology and instrumentation needed to
analyse these precious materials.
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