Crustal thickness of Antarctica estimated using data from gravimetric satellites
Computing a better crustal thickness model is still a necessary improvement in Antarctica. In this remote continent where almost all the bedrock is covered by the ice sheet, seismic investigations do not reach a sufficient spatial resolution for geological and geophysical purposes. Here, we present...
Published in: | Solid Earth |
---|---|
Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
2018
|
Subjects: | |
Online Access: | https://doi.org/10.5194/se-9-457-2018 https://se.copernicus.org/articles/9/457/2018/ |
id |
ftcopernicus:oai:publications.copernicus.org:se61845 |
---|---|
record_format |
openpolar |
spelling |
ftcopernicus:oai:publications.copernicus.org:se61845 2023-05-15T13:55:28+02:00 Crustal thickness of Antarctica estimated using data from gravimetric satellites Llubes, Muriel Seoane, Lucia Bruinsma, Sean Rémy, Frédérique 2018-09-27 application/pdf https://doi.org/10.5194/se-9-457-2018 https://se.copernicus.org/articles/9/457/2018/ eng eng doi:10.5194/se-9-457-2018 https://se.copernicus.org/articles/9/457/2018/ eISSN: 1869-9529 Text 2018 ftcopernicus https://doi.org/10.5194/se-9-457-2018 2020-07-20T16:23:20Z Computing a better crustal thickness model is still a necessary improvement in Antarctica. In this remote continent where almost all the bedrock is covered by the ice sheet, seismic investigations do not reach a sufficient spatial resolution for geological and geophysical purposes. Here, we present a global map of Antarctic crustal thickness computed from space gravity observations. The DIR5 gravity field model, built from GOCE and GRACE gravimetric data, is inverted with the Parker–Oldenburg iterative algorithm. The BEDMAP products are used to estimate the gravity effect of the ice and the rocky surface. Our result is compared to crustal thickness calculated from seismological studies and the CRUST1.0 and AN1 models. Although the CRUST1.0 model shows a very good agreement with ours, its spatial resolution is larger than the one we obtain with gravimetric data. Finally, we compute a model in which the crust–mantle density contrast is adjusted to fit the Moho depth from the CRUST1.0 model. In East Antarctica, the resulting density contrast clearly shows higher values than in West Antarctica. Text Antarc* Antarctic Antarctica East Antarctica Ice Sheet West Antarctica Copernicus Publications: E-Journals Antarctic East Antarctica Oldenburg West Antarctica Solid Earth 9 2 457 467 |
institution |
Open Polar |
collection |
Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
Computing a better crustal thickness model is still a necessary improvement in Antarctica. In this remote continent where almost all the bedrock is covered by the ice sheet, seismic investigations do not reach a sufficient spatial resolution for geological and geophysical purposes. Here, we present a global map of Antarctic crustal thickness computed from space gravity observations. The DIR5 gravity field model, built from GOCE and GRACE gravimetric data, is inverted with the Parker–Oldenburg iterative algorithm. The BEDMAP products are used to estimate the gravity effect of the ice and the rocky surface. Our result is compared to crustal thickness calculated from seismological studies and the CRUST1.0 and AN1 models. Although the CRUST1.0 model shows a very good agreement with ours, its spatial resolution is larger than the one we obtain with gravimetric data. Finally, we compute a model in which the crust–mantle density contrast is adjusted to fit the Moho depth from the CRUST1.0 model. In East Antarctica, the resulting density contrast clearly shows higher values than in West Antarctica. |
format |
Text |
author |
Llubes, Muriel Seoane, Lucia Bruinsma, Sean Rémy, Frédérique |
spellingShingle |
Llubes, Muriel Seoane, Lucia Bruinsma, Sean Rémy, Frédérique Crustal thickness of Antarctica estimated using data from gravimetric satellites |
author_facet |
Llubes, Muriel Seoane, Lucia Bruinsma, Sean Rémy, Frédérique |
author_sort |
Llubes, Muriel |
title |
Crustal thickness of Antarctica estimated using data from gravimetric satellites |
title_short |
Crustal thickness of Antarctica estimated using data from gravimetric satellites |
title_full |
Crustal thickness of Antarctica estimated using data from gravimetric satellites |
title_fullStr |
Crustal thickness of Antarctica estimated using data from gravimetric satellites |
title_full_unstemmed |
Crustal thickness of Antarctica estimated using data from gravimetric satellites |
title_sort |
crustal thickness of antarctica estimated using data from gravimetric satellites |
publishDate |
2018 |
url |
https://doi.org/10.5194/se-9-457-2018 https://se.copernicus.org/articles/9/457/2018/ |
geographic |
Antarctic East Antarctica Oldenburg West Antarctica |
geographic_facet |
Antarctic East Antarctica Oldenburg West Antarctica |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet West Antarctica |
op_source |
eISSN: 1869-9529 |
op_relation |
doi:10.5194/se-9-457-2018 https://se.copernicus.org/articles/9/457/2018/ |
op_doi |
https://doi.org/10.5194/se-9-457-2018 |
container_title |
Solid Earth |
container_volume |
9 |
container_issue |
2 |
container_start_page |
457 |
op_container_end_page |
467 |
_version_ |
1766262133443526656 |