DI31B:
New Insights into the Earth's Core I
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DI31B:
New Insights into the Earth's Core I
New Insights into the Earth's Core I
Session ID#: 32055
Session Description:
The history of Earth’s core remains debated and poorly constrained even as new experiments and observations have contributed to our understanding of the thermal state of outer core and the nucleation of the inner core. Scenarios for the operation and history of the dynamo are challenged by evidence of a stable stratified layer at the outer core’s upper boundary, a high value of thermal conductivity, and the presence of an early magnetic field. In the inner core, seismic observations reveal complex lateral and vertical structure at a broad spectrum of spatial scales, with unknown links to the history of its crystallization, melting, and deformation. We hope this session will bring together a wide range of disciplines, including geodynamic modeling, high-pressure experiments, and seismic observations with the aim of a better understanding Earth’s core.
Primary Convener: Ludovic Huguet, Université Grenoble Alpes, ISTerre, Grenoble, France
Conveners: Vernon F Cormier, University of Connecticut, Groton, CT, United States and Robert Teed, University of Cambridge, Cambridge, United Kingdom
Chairs: Ludovic Huguet, Université Grenoble Alpes, ISTerre, Grenoble, France, Robert Teed, University of Glasgow, Glasgow, G12, United Kingdom and Vernon F Cormier, University of Connecticut, Groton, CT, United States
OSPA Liaison: Vernon F Cormier, University of Connecticut, Groton, CT, United States
Cross-Listed:
- GP - Geomagnetism, Paleomagnetism and Electromagnetism
- 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]
Abstracts Submitted to this Session:
See more of: Study of Earth's Deep Interior
