Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data

Research output: Contribution to journalJournal articleResearchpeer-review

Standard

Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data. / Joshi, Rakshit; Knapmeyer-Endrun, Brigitte; Mosegaard, Klaus; Igel, Heiner; Christensen, Ulrich R.

In: Earth and Space Science, Vol. 8, No. 10, e2021EA001733, 16.10.2021.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Joshi, R, Knapmeyer-Endrun, B, Mosegaard, K, Igel, H & Christensen, UR 2021, 'Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data', Earth and Space Science, vol. 8, no. 10, e2021EA001733. https://doi.org/10.1029/2021EA001733

APA

Joshi, R., Knapmeyer-Endrun, B., Mosegaard, K., Igel, H., & Christensen, U. R. (2021). Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data. Earth and Space Science, 8(10), [e2021EA001733]. https://doi.org/10.1029/2021EA001733

Vancouver

Joshi R, Knapmeyer-Endrun B, Mosegaard K, Igel H, Christensen UR. Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data. Earth and Space Science. 2021 Oct 16;8(10). e2021EA001733. https://doi.org/10.1029/2021EA001733

Author

Joshi, Rakshit ; Knapmeyer-Endrun, Brigitte ; Mosegaard, Klaus ; Igel, Heiner ; Christensen, Ulrich R. / Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data. In: Earth and Space Science. 2021 ; Vol. 8, No. 10.

Bibtex

@article{b7fbf13c907a4bca890bf63bf5d0633b,
title = "Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data",
abstract = "The estimation of crustal structure and thickness is essential in understanding the formation and evolution of terrestrial planets. Initial planetary missions with seismic instrumentation on board face the additional challenge of dealing with seismic activity levels that are only poorly constrained a priori. For example, the lack of plate tectonics on Mars leads to low seismicity, which could, in turn, hinder the application of many terrestrial data analysis techniques. Here we propose using a joint inversion of receiver functions and apparent incidence angles, which contain information on absolute S-wave velocities of the subsurface. Since receiver function inversions suffer from a velocity depth trade-off, we in addition exploit a simple relation that defines apparent S-wave velocity as a function of observed apparent P-wave incidence angles to constrain the parameter space. We then use the Neighborhood Algorithm for the inversion of a suitable joint objective function. The resulting ensemble of models is then used to derive uncertainty estimates for each model parameter. In preparation for the analysis of data from the InSight mission, we show the application of our proposed method on Mars synthetics and sparse terrestrial data sets from different geological settings using both single and multiple events. We use information-theoretic statistical tests as model selection criteria and discuss their relevance and implications in a seismological framework.",
keywords = "seismology, receiver functions, planets, crustal thickness, joint inversion, incidence angles, CRUSTAL STRUCTURE, UPPER-MANTLE, MOHO DEPTH, NEIGHBORHOOD ALGORITHM, GEOPHYSICAL INVERSION, STRUCTURE BENEATH, SEISMOGRAMS, WAVES, POLARIZATION, VELOCITIES",
author = "Rakshit Joshi and Brigitte Knapmeyer-Endrun and Klaus Mosegaard and Heiner Igel and Christensen, {Ulrich R.}",
year = "2021",
month = oct,
day = "16",
doi = "10.1029/2021EA001733",
language = "English",
volume = "8",
journal = "Earth and Space Science",
issn = "2333-5084",
publisher = "American Geophysical Union",
number = "10",

}

RIS

TY - JOUR

T1 - Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data

AU - Joshi, Rakshit

AU - Knapmeyer-Endrun, Brigitte

AU - Mosegaard, Klaus

AU - Igel, Heiner

AU - Christensen, Ulrich R.

PY - 2021/10/16

Y1 - 2021/10/16

N2 - The estimation of crustal structure and thickness is essential in understanding the formation and evolution of terrestrial planets. Initial planetary missions with seismic instrumentation on board face the additional challenge of dealing with seismic activity levels that are only poorly constrained a priori. For example, the lack of plate tectonics on Mars leads to low seismicity, which could, in turn, hinder the application of many terrestrial data analysis techniques. Here we propose using a joint inversion of receiver functions and apparent incidence angles, which contain information on absolute S-wave velocities of the subsurface. Since receiver function inversions suffer from a velocity depth trade-off, we in addition exploit a simple relation that defines apparent S-wave velocity as a function of observed apparent P-wave incidence angles to constrain the parameter space. We then use the Neighborhood Algorithm for the inversion of a suitable joint objective function. The resulting ensemble of models is then used to derive uncertainty estimates for each model parameter. In preparation for the analysis of data from the InSight mission, we show the application of our proposed method on Mars synthetics and sparse terrestrial data sets from different geological settings using both single and multiple events. We use information-theoretic statistical tests as model selection criteria and discuss their relevance and implications in a seismological framework.

AB - The estimation of crustal structure and thickness is essential in understanding the formation and evolution of terrestrial planets. Initial planetary missions with seismic instrumentation on board face the additional challenge of dealing with seismic activity levels that are only poorly constrained a priori. For example, the lack of plate tectonics on Mars leads to low seismicity, which could, in turn, hinder the application of many terrestrial data analysis techniques. Here we propose using a joint inversion of receiver functions and apparent incidence angles, which contain information on absolute S-wave velocities of the subsurface. Since receiver function inversions suffer from a velocity depth trade-off, we in addition exploit a simple relation that defines apparent S-wave velocity as a function of observed apparent P-wave incidence angles to constrain the parameter space. We then use the Neighborhood Algorithm for the inversion of a suitable joint objective function. The resulting ensemble of models is then used to derive uncertainty estimates for each model parameter. In preparation for the analysis of data from the InSight mission, we show the application of our proposed method on Mars synthetics and sparse terrestrial data sets from different geological settings using both single and multiple events. We use information-theoretic statistical tests as model selection criteria and discuss their relevance and implications in a seismological framework.

KW - seismology

KW - receiver functions

KW - planets

KW - crustal thickness

KW - joint inversion

KW - incidence angles

KW - CRUSTAL STRUCTURE

KW - UPPER-MANTLE

KW - MOHO DEPTH

KW - NEIGHBORHOOD ALGORITHM

KW - GEOPHYSICAL INVERSION

KW - STRUCTURE BENEATH

KW - SEISMOGRAMS

KW - WAVES

KW - POLARIZATION

KW - VELOCITIES

U2 - 10.1029/2021EA001733

DO - 10.1029/2021EA001733

M3 - Journal article

VL - 8

JO - Earth and Space Science

JF - Earth and Space Science

SN - 2333-5084

IS - 10

M1 - e2021EA001733

ER -

ID: 284172686