Details
| Originalsprache | Englisch |
|---|---|
| Titel des Sammelwerks | 23rd European Meeting of Environmental and Engineering Geophysics |
| Seiten | 1-5 |
| Seitenumfang | 5 |
| ISBN (elektronisch) | 9789462822238 |
| Publikationsstatus | Veröffentlicht - 3 Sept. 2017 |
| Extern publiziert | Ja |
| Veranstaltung | 23rd European Meeting of Environmental and Engineering Geophysics - Malmo, Schweden Dauer: 3 Sept. 2017 → 7 Sept. 2017 |
Abstract
A high-resolution P-wave vibroseis reflection survey and PSDM processing are used to image the structure of the Tannwald Basin, a 250 m-deep, distal branch basin of the Rhine Glacier. The basin substratum, the basin base, as well as the basin infill could be identified. The subglacial deposits (e.g. till) can be clearly distinguished from basin fines (e.g. marl, silt and sand). We identified five seismic facies as well as a number of subfacies. Internal features of the basin comprises an allochthonous Molasse block and a system of eskers in section. The interpretation will be used to locate a drill site for the ICDP-project DOVE and provides information for S-wave and multi-component processing.
ASJC Scopus Sachgebiete
- Erdkunde und Planetologie (insg.)
- Geotechnik und Ingenieurgeologie
- Erdkunde und Planetologie (insg.)
- Geochemie und Petrologie
- Energie (insg.)
- Energieanlagenbau und Kraftwerkstechnik
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23rd European Meeting of Environmental and Engineering Geophysics. 2017. S. 1-5.
Publikation: Beitrag in Buch/Bericht/Sammelwerk/Konferenzband › Aufsatz in Konferenzband › Forschung › Peer-Review
}
TY - GEN
T1 - Seismic Facies Characterization of the Overdeepened Glacial Tannwald Basin
AU - Burschil, T.
AU - Buness, H.
AU - Tanner, D.
AU - Gabriel, G.
AU - Krawczyk, C.
N1 - Funding Information: The project was funded by German Research Foundation DFG, grants KR2073/3-1, GA749/5-1.
PY - 2017/9/3
Y1 - 2017/9/3
N2 - A high-resolution P-wave vibroseis reflection survey and PSDM processing are used to image the structure of the Tannwald Basin, a 250 m-deep, distal branch basin of the Rhine Glacier. The basin substratum, the basin base, as well as the basin infill could be identified. The subglacial deposits (e.g. till) can be clearly distinguished from basin fines (e.g. marl, silt and sand). We identified five seismic facies as well as a number of subfacies. Internal features of the basin comprises an allochthonous Molasse block and a system of eskers in section. The interpretation will be used to locate a drill site for the ICDP-project DOVE and provides information for S-wave and multi-component processing.
AB - A high-resolution P-wave vibroseis reflection survey and PSDM processing are used to image the structure of the Tannwald Basin, a 250 m-deep, distal branch basin of the Rhine Glacier. The basin substratum, the basin base, as well as the basin infill could be identified. The subglacial deposits (e.g. till) can be clearly distinguished from basin fines (e.g. marl, silt and sand). We identified five seismic facies as well as a number of subfacies. Internal features of the basin comprises an allochthonous Molasse block and a system of eskers in section. The interpretation will be used to locate a drill site for the ICDP-project DOVE and provides information for S-wave and multi-component processing.
UR - http://www.scopus.com/inward/record.url?scp=85088410688&partnerID=8YFLogxK
U2 - 10.3997/2214-4609.201702101
DO - 10.3997/2214-4609.201702101
M3 - Conference contribution
AN - SCOPUS:85088410688
SP - 1
EP - 5
BT - 23rd European Meeting of Environmental and Engineering Geophysics
T2 - 23rd European Meeting of Environmental and Engineering Geophysics
Y2 - 3 September 2017 through 7 September 2017
ER -