[Skip to Content]
Banner
Menu
  • Home
  • Submit Abstract
  • Home
  • 2021 Annual Meeting Session Gallery
  • Advances in Seismic Interferometry: Theory, Computation and Applications [Poster]
  • Imaging Yellowstone’s Melt Distribution With Full Waveform Inversion of Ambient Noise

← Back to Sessions

Imaging Yellowstone’s Melt Distribution With Full Waveform Inversion of Ambient Noise

Session: Advances in Seismic Interferometry: Theory, Computation and Applications [Poster]

Type: Poster

Date: 4/22/2021

Presentation Time: 11:30 AM Pacific

Description: 

The Yellowstone hotspot hosts a complex crustal magmatic system that drives hydrothermal activity, seismicity, and periodic ground deformation. Seismic tomography has constrained the presence of a partially molten magma reservoir at middle-to-upper crustal depths centered below the Yellowstone caldera, but key aspects of the system such as the total volume and distribution of melt remain open questions. Interpretations of previous tomographic images of Yellowstone are complicated by an incomplete understanding of how large crustal magmatic systems affect seismic waveforms. In particular, tomographic studies based on asymptotic methods may underestimate the seismic wave speed anomaly of the magma reservoir because first arriving energy may be diffracted around strong low wave speed anomalies. Compared to asymptotic methods, full waveform inversion approaches enable improved resolution since they incorporate more accurate sensitivity kernels based on realistic wave propagation physics. Here, we present the initial iterations of a new ambient noise dataset based full waveform inversion of Yellowstone’s crust and uppermost mantle. Our starting model, which is based on inverting Rayleigh wave dispersion measurements of vertical component noise correlation functions, shares many key features with previous tomography results, including a roughly 10% slow shear wave speed anomaly centered below the Yellowstone caldera. The continued iterations of the full waveform inversion promise to sharpen features in the model and more accurately recover the strength of the anomaly associated with Yellowstone’s crustal magmatic system, which is critical for understanding the volume and distribution of melt.

Presenting Author: Ross R. Maguire

Student Presenter: No


Authors

Ross Maguire

Presenting Author

Corresponding Author

maguir12@msu.edu

Michigan State University

Min Chen

chenmi22@msu.edu

Michigan State University

Brandon Schmandt

bschmandt@unm.edu

University of New Mexico

Chengxin Jiang

chengxin.jiang1@anu.edu.au

Australian National University

Justin Wilgus

jwilgus@unm.edu

University of New Mexico

Jiaqi Li

lijiaqi9@msu.edu

Michigan State University

 

Imaging Yellowstone’s Melt Distribution With Full Waveform Inversion of Ambient Noise

Category

Advances in Seismic Interferometry: Theory, Computation and Applications