Sarah Beraus
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View article: Data-driven lithofacies prediction of unconsolidated sediments from wireline logs
Data-driven lithofacies prediction of unconsolidated sediments from wireline logs Open
Detailed knowledge of the lithostratigraphy of unconsolidated sediments is essential for many scientific and industrial applications. Although drill cores provide lithological and petrophysical information (e.g., lithofacies, permeability,…
View article: Seismic- and core-based glacial sequence stratigraphy in an overdeepened trough in the northern Alpine foreland of Switzerland
Seismic- and core-based glacial sequence stratigraphy in an overdeepened trough in the northern Alpine foreland of Switzerland Open
In the context of a project of the International Continental Scientific Drilling Program (ICDP) (DOVE; Drilling Overdeepened Alpine Valleys), a series of boreholes were drilled into buried overdeepened glacial troughs in the central and ea…
View article: Seismic crosshole full‐waveform inversion of high‐frequency SV‐waves for glacial sediment characterization
Seismic crosshole full‐waveform inversion of high‐frequency SV‐waves for glacial sediment characterization Open
We present a two‐dimensional, high‐resolution full‐waveform inversion approach of crosshole seismic data to image fine glacial sediments in an overdeepened Alpine valley, the Tannwald Basin (ICDP site 5068_1) north of Lake Constance. A ver…
View article: High-resolution SH-wave crosshole seismic full-waveform inversion in the glacially overdeepened Tannwald Basin
High-resolution SH-wave crosshole seismic full-waveform inversion in the glacially overdeepened Tannwald Basin Open
During the Quaternary, the Rhine Glacier formed several overdeepened valleys, including the Tannwald Basin (ICDP site 5068_1, Germany) about 45 km North of Lake Constance. These structures form sedimentary climate archives and thus help to…
View article: A comprehensive crosshole seismic experiment in glacial sediments at the ICDP DOVE site in the Tannwald Basin
A comprehensive crosshole seismic experiment in glacial sediments at the ICDP DOVE site in the Tannwald Basin Open
Glaciers have shaped the Alpine landscape by carving deep valleys and depositing sediments to form overdeepened basins. Understanding these processes provides information on the evolution of the climate and landscape. One such overdeepened…
View article: High-resolution crosshole seismic imaging of glacial sediments by full-waveform inversion
High-resolution crosshole seismic imaging of glacial sediments by full-waveform inversion Open
During the Quaternary, glaciers shaped the Alpine region by excavating deep valleys and refilling them with the sediments that they transported. One such overdeepened valley is the Tannwald Basin (ICDP site 5068_1), which was created by th…
View article: Seismic and core-based glacial sequence stratigraphy of an overdeepened valley fill in northern Switzerland 
Seismic and core-based glacial sequence stratigraphy of an overdeepened valley fill in northern Switzerland  Open
In the context of the DOVE (Drilling Overdeepened Alpine Valleys) project, supported by the International Continental Scientific Drilling Program (ICDP), a series of boreholes were drilled into buried overdeepened glacial troughs situated …