Details
| Originalsprache | Englisch |
|---|---|
| Titel des Sammelwerks | Third EAGE Conference on Seismic Inversion |
| Seiten | 1-5 |
| ISBN (elektronisch) | 9789462825048 |
| Publikationsstatus | Veröffentlicht - Okt. 2024 |
| Veranstaltung | 3rd EAGE Conference on Seismic Inversion, SI 2024 - Naples, Italien Dauer: 14 Okt. 2024 → 16 Okt. 2024 |
Abstract
This study presents a seismic full-waveform inversion approach using orthogonally shear waves to image glacial sediments in a transmission geometry. Starting from a homogeneous model and using frequencies between 80 and 250 Hz in a multi-stage approach, we obtain high-resolution subsurface models. Despite the identical workflow, the resulting models exhibit different structural features, yet they align with the lithology provided by core information at their respective resolution power.
ASJC Scopus Sachgebiete
- Erdkunde und Planetologie (insg.)
- Geophysik
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Third EAGE Conference on Seismic Inversion. 2024. S. 1-5.
Publikation: Beitrag in Buch/Bericht/Sammelwerk/Konferenzband › Aufsatz in Konferenzband › Forschung › Peer-Review
}
TY - GEN
T1 - High-resolution shear wave crosshole full-waveform inversion
AU - Beraus, S.
AU - Köhn, D.
AU - Bohlen, T.
AU - Buness, H.
AU - Burschil, T.
AU - Gabriel, G.
N1 - Publisher Copyright: © 3rd EAGE Conference on Seismic Inversion 2024.
PY - 2024/10
Y1 - 2024/10
N2 - This study presents a seismic full-waveform inversion approach using orthogonally shear waves to image glacial sediments in a transmission geometry. Starting from a homogeneous model and using frequencies between 80 and 250 Hz in a multi-stage approach, we obtain high-resolution subsurface models. Despite the identical workflow, the resulting models exhibit different structural features, yet they align with the lithology provided by core information at their respective resolution power.
AB - This study presents a seismic full-waveform inversion approach using orthogonally shear waves to image glacial sediments in a transmission geometry. Starting from a homogeneous model and using frequencies between 80 and 250 Hz in a multi-stage approach, we obtain high-resolution subsurface models. Despite the identical workflow, the resulting models exhibit different structural features, yet they align with the lithology provided by core information at their respective resolution power.
UR - http://www.scopus.com/inward/record.url?scp=85216884480&partnerID=8YFLogxK
U2 - 10.3997/2214-4609.202438039
DO - 10.3997/2214-4609.202438039
M3 - Conference contribution
AN - SCOPUS:85216884480
SP - 1
EP - 5
BT - Third EAGE Conference on Seismic Inversion
T2 - 3rd EAGE Conference on Seismic Inversion, SI 2024
Y2 - 14 October 2024 through 16 October 2024
ER -