Details
| Original language | English |
|---|---|
| Title of host publication | 23rd European Meeting of Environmental and Engineering Geophysics |
| Pages | 1-5 |
| Number of pages | 5 |
| ISBN (electronic) | 9789462822238 |
| Publication status | Published - 3 Sept 2017 |
| Externally published | Yes |
| Event | 23rd European Meeting of Environmental and Engineering Geophysics - Malmo, Sweden Duration: 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 subject areas
- Earth and Planetary Sciences(all)
- Geotechnical Engineering and Engineering Geology
- Earth and Planetary Sciences(all)
- Geochemistry and Petrology
- Energy(all)
- Energy Engineering and Power Technology
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23rd European Meeting of Environmental and Engineering Geophysics. 2017. p. 1-5.
Research output: Chapter in book/report/conference proceeding › Conference contribution › Research › 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 -