Low-temperature thermochronology is the study and measurement of the time-temperature history of rocks during exhumation/cooling. Recently, we discovered a new thermochronologic method based on an electron trapping dating method, namely optically stimulated luminescence (OSL)-dating, which should open a new area of research in Earth Sciences. The goal of the project is to further develop this new technique and assess its broad applicability (e.g., to quantify the links that may exist between tectonics and climate).

The project includes fieldwork in Australia and the Swiss Alps, laboratory work and numerical modeling. It involves close collaboration with the University of Oxford and the University of California, Los Angeles (for the experimental work).

The appointment is available for 3 years. The salary of the PhD position is based on the salary scale of the Swiss National Science Foundation.

Applicants should have a university degree, preferably in earth sciences or physics. Please send applications by e-mail to Frédéric Herman (frederic[@]erdw.ethz.ch) by October, 30. Applications must include a CV (with contact information of two referees), university grades of all university classes, and a one-page statement of your background and research interests.

Questions about the project, ETH and/or Zurich can be sent to Frédéric Herman.