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  • Structural Seismology: From Crust to Core [Poster]
  • Seismological Explorations of Earth’s Outer Core: Normal Mode and Body Wave Analyses

 

Seismological Explorations of Earth’s Outer Core: Normal Mode and Body Wave Analyses

Date: 4/26/2019

Time: 06:00 PM

Room: Grand Ballroom

Earth’s outer core is a source of both the geodynamo and heat for mantle convection. However, we still do not fully understand its chemical composition, and there debate about whether the uppermost outer core may contain a stratified layer which may be enriched in light elements. We present low frequency normal mode and high frequency body wave investigations of the outer core's properties.

Normal mode oscillations of the whole Earth, excited by large earthquakes, are sensitive to the large-scale variations in velocity and density. We use the centre frequencies of hundreds of oscillations to infer the bulk properties of the outer core. We carry out a Bayesian inversion using a mineralogical Equation-of-State framework to infer the outer core's velocity, density and mineralogical properties, under the assumption that the outer core is well mixed and adiabatic. The model we produce, EPOC, describes the Elastic Parameters of the Outer Core. EPOC predicts seismic velocities at the top of the outer core which are closer to existing body-wave models than to PREM, resolving a long-standing discrepancy. EPOC also fits normal-mode data better than the Preliminary Reference Earth Model. We also consider the effects of relaxing our assumptions that (i) there is no stratified layer at the top of the outer core, and (ii) that PREM is correct outside the outer core.

To better assess the uppermost outer core, which is may be termed the E' layer, we use a novel, iterative measurement technique to measure SmKS differential travel times. SmKS waves are particularly sensitive to the E' layer, and reflect (m-1) times from the underside of the core-mantle boundary. We find that the SmKS differential travel times are better described by models with seismic velocities in the E' layer slower than PREM, such as EPOC or body-wave derived KHOMC (Kaneshima and Helffrich, 2013).

 


Presenting Author: Jessica C. E. Irving


Authors

Jessica C E Irving

Presenting Author Corresponding Author

jirving@princeton.edu

Princeton University, Princeton, New Jersey, United States

Presenting Author
Corresponding Author

Sanne Cottaar

sc845@cam.ac.uk

University of Cambridge, Cambridge, , United Kingdom

Vedran Lekic

ved@umd.edu

University of Maryland, College Park, Maryland, United States

Wenbo Wu

wenbow@princeton.edu

Princeton Unversity, Princeton, New Jersey, United Kingdom

Seismological Explorations of Earth’s Outer Core: Normal Mode and Body Wave Analyses

Category

Structural Seismology: From Crust to Core

Description