Earth System Science Data (May 2023)
Moho depths beneath the European Alps: a homogeneously processed map and receiver functions database
- K. Michailos,
- K. Michailos,
- G. Hetényi,
- G. Hetényi,
- M. Scarponi,
- M. Scarponi,
- M. Scarponi,
- J. Stipčević,
- I. Bianchi,
- I. Bianchi,
- L. Bonatto,
- W. Czuba,
- M. Di Bona,
- A. Govoni,
- K. Hannemann,
- T. Janik,
- D. Kalmár,
- D. Kalmár,
- R. Kind,
- R. Kind,
- F. Link,
- F. P. Lucente,
- S. Monna,
- C. Montuori,
- S. Mroczek,
- S. Mroczek,
- A. Paul,
- C. Piromallo,
- J. Plomerová,
- J. Rewers,
- S. Salimbeni,
- F. Tilmann,
- F. Tilmann,
- P. Środa,
- J. Vergne
Affiliations
- K. Michailos
- Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland
- K. Michailos
- now at: Department of Earth Sciences, University of Geneva, Geneva, Switzerland
- G. Hetényi
- Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland
- G. Hetényi
- Kövesligethy Radó Seismological Observatory, Institute of Earth Physics and Space Science, Budapest, Hungary
- M. Scarponi
- Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland
- M. Scarponi
- Institute of Geophysics, Czech Academy of Sciences, Prague, Czech Republic
- M. Scarponi
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- J. Stipčević
- Department of Geophysics, Faculty of Science, University of Zagreb, Zagreb, Croatia
- I. Bianchi
- Department of Meteorology and Geophysics, University of Vienna, Vienna, Austria
- I. Bianchi
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- L. Bonatto
- Department of Physics, University of La Serena, La Serena, Región de Coquimbo, Chile
- W. Czuba
- Department of Seismic Lithospheric Research, Institute of Geophysics Polish Academy of Sciences, Warszawa, Poland
- M. Di Bona
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- A. Govoni
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- K. Hannemann
- Westfälische Wilhelms Universität Münster, Institut für Geophysik, Münster, Germany
- T. Janik
- Department of Seismic Lithospheric Research, Institute of Geophysics Polish Academy of Sciences, Warszawa, Poland
- D. Kalmár
- Kövesligethy Radó Seismological Observatory, Institute of Earth Physics and Space Science, Budapest, Hungary
- D. Kalmár
- MTA FI Lendület Pannon LitH2Oscope Research Group, Institute of Earth Physics and Space Science, Budapest, Hungary
- R. Kind
- Institute for Geological Sciences, Freie Universität Berlin, Malteserstr. 74–100, 12249 Berlin, Germany
- R. Kind
- GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
- F. Link
- Institute of Geosciences, Goethe University Frankfurt, Frankfurt, Germany
- F. P. Lucente
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- S. Monna
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- C. Montuori
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- S. Mroczek
- Institute for Geological Sciences, Freie Universität Berlin, Malteserstr. 74–100, 12249 Berlin, Germany
- S. Mroczek
- GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
- A. Paul
- CNRS, IRD, Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, Univ. Gustave Eiffel, ISTerre, 38000 Grenoble, France
- C. Piromallo
- Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
- J. Plomerová
- Institute of Geophysics, Czech Academy of Sciences, Prague, Czech Republic
- J. Rewers
- Department of Seismic Lithospheric Research, Institute of Geophysics Polish Academy of Sciences, Warszawa, Poland
- S. Salimbeni
- Istituto Nazionale di Geofisica e Vulcanologia, Bologna, Italy
- F. Tilmann
- Institute for Geological Sciences, Freie Universität Berlin, Malteserstr. 74–100, 12249 Berlin, Germany
- F. Tilmann
- GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
- P. Środa
- Department of Seismic Lithospheric Research, Institute of Geophysics Polish Academy of Sciences, Warszawa, Poland
- J. Vergne
- Institut Terre & Environnement de Strasbourg, University of Strasbourg, Strasbourg, France
- DOI
- https://doi.org/10.5194/essd-15-2117-2023
- Journal volume & issue
-
Vol. 15
pp. 2117 – 2138
Abstract
We use seismic waveform data from the AlpArray Seismic Network and three other temporary seismic networks, to perform receiver function (RF) calculations and time-to-depth migration to update the knowledge of the Moho discontinuity beneath the broader European Alps. In particular, we set up a homogeneous processing scheme to compute RFs using the time-domain iterative deconvolution method and apply consistent quality control to yield 112 205 high-quality RFs. We then perform time-to-depth migration in a newly implemented 3D spherical coordinate system using a European-scale reference P and S wave velocity model. This approach, together with the dense data coverage, provide us with a 3D migrated volume, from which we present migrated profiles that reflect the first-order crustal thickness structure. We create a detailed Moho map by manually picking the discontinuity in a set of orthogonal profiles covering the entire area. We make the RF dataset, the software for the entire processing workflow, as well as the Moho map, openly available; these open-access datasets and results will allow other researchers to build on the current study.