DI008
Exploring the Earth's core: a multidisciplinary approach
Exploring the Earth's core: a multidisciplinary approach
Session ID#: 76569
Session Description:
The Earth's core is the most unreachable place in our planet. It is one of Earth’s most active regions, with convection of its molten iron alloy generating the magnetic field observed at the surface of the Earth, and the inner core slowly growing at the expense of the outer core. Understanding the present day properties and long and short term evolution of both the liquid outer core and solid inner core requires discussion and collaboration between computational, theoretical, experimental and observational researchers. For example, constraints on material properties such as the thermal conductivity are still under debate, the structural nature of stratified layers near the outer core’s boundaries remain elusive, and discussions surrounding the inner core crystallization remain ongoing, amongst many other pertinent issues.
We welcome contributions from all disciplines to advance the understanding of the Earth's core including, but not limited to, geochemistry, geodynamics, geomagnetism, mineral physics and seismology.
Co-Organized:
- MR - Mineral and Rock Physics
- S - Seismology
Index Terms:
1507 Core processes [GEOMAGNETISM AND PALEOMAGNETISM]
1510 Dynamo: theories and simulations [GEOMAGNETISM AND PALEOMAGNETISM]
3924 High-pressure behavior [MINERAL PHYSICS]
7207 Core [SEISMOLOGY]
Primary Convener: Marine Lasbleis, Université de Nantes, LPG, CNRS, Nantes, France
Conveners: Jessica C E Irving, Princeton University, Department of Geosciences, Princeton, NJ, United States, Kenji Ohta, Tokyo Institute of Technology, Department of Earth and Planetary Sciences, Tokyo, Japan and Jenny Wong, Institut de Physique du Globe de Paris, Paris, France
Primary Liaison: Marine Lasbleis, Université de Nantes, LPG, CNRS, Nantes, France
See more of: Study of Earth's Deep Interior
