Universität Wien

280398 VO MA PE 06 Paleomagnetism (NPI) (2017W)

Details

max. 20 participants
Language: English

Examination dates

Lecturers

Classes (iCal) - next class is marked with N

Lecture will be blocked. The dates for the individual blocks will be discussed and fixed on 3.11., 13:00.

  • Wednesday 04.10. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 11.10. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 18.10. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 25.10. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 08.11. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 15.11. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 22.11. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 29.11. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 06.12. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 13.12. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 10.01. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 17.01. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 24.01. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II
  • Wednesday 31.01. 15:00 - 16:30 Felix-Machatschki-Seminarraum Mineralogie 2B284 2.OG UZA II

Information

Aims, contents and method of the course

Magnetic properties are extremely useful to help understand the genesis and subsequent history of rocks. A number of magnetic properties (Curie temperature, hysteresis parameters, etc.) facilitate the unique identification of each magnetic mineral. These same properties are sensitive to composition, oxidation state, pressure, size and shape of the magnetic mineral assemblage. Knowledge of these parameters is crucial when interpreting complex systems typically encountered in the Earth and planetary sciences. Paleomagnetism , making use of magnetic properties of rocks, is the best method to make quantitative paleogeographic reconstructions of the Earth during the geological past. Moreover, this technique can help unravel the kinematics of deformation within orogenic belts, which is crucial to understand how mountains form and to understand the underlying processes governing plate tectonic processes on Earth. Within this lecture we will get an overview about basics of rock magnetism and its applications in paleomagnetism, magnetostratigraphy, archeomagnetism.

Assessment and permitted materials

oral

Minimum requirements and assessment criteria

Examination topics

Reading list


Association in the course directory

Last modified: Sa 02.04.2022 00:25