Articles | Volume 11, issue 2
https://doi.org/10.5194/se-11-607-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-607-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
23 Apr 2020
Research article |
| 23 Apr 2020
| 23 Apr 2020
Correlation of core and downhole seismic velocities in high-pressure metamorphic rocks: a case study for the COSC-1 borehole, Sweden
Felix Kästner
CORRESPONDING AUTHOR
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany
Simona Pierdominici
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
Judith Elger
GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany
Alba Zappone
Department of Earth Sciences, ETH Zurich, 8092 Zurich, Switzerland
Jochem Kück
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, 14473 Potsdam, Germany
Christian Berndt
GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany
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Cited
14 citations as recorded by crossref.
- Anisotropic velocity models for (3-D) seismic imaging of the Lower Seve Nappe in Jämtland, Sweden F. Kästner et al. 10.1093/gji/ggab339
- Elastic anisotropies of rocks in a subduction and exhumation setting M. Schmidtke et al. 10.5194/se-12-1801-2021
- Pressure, temperature and lithological dependence of seismic and magnetic susceptibility anisotropy in amphibolites and gneisses from the central Scandinavian Caledonides M. Bazargan et al. 10.1016/j.tecto.2021.229113
- Impact of sub-basalt thrust systems on the Faroe continental shelf for the late Paleoproterozoic–Cenozoic tectonic evolution of the margin. J. Koehl et al. 10.12688/openreseurope.18284.2
- Attenuation of Seismic Waves in Partially Saturated Berea Sandstone as a Function of Frequency and Confining Pressure N. Tisato et al. 10.3389/feart.2021.641177
- Seismic anisotropy of mid crustal orogenic nappes and their bounding structures: An example from the Middle Allochthon (Seve Nappe) of the Central Scandinavian Caledonides B. Almqvist et al. 10.1016/j.tecto.2021.229045
- Core‐Log‐Seismic Integration in Metamorphic Rocks and Its Implication for the Regional Geology: A Case Study for the ICDP Drilling Project COSC‐1, Sweden J. Elger et al. 10.1029/2020GC009376
- Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone imaging T. Leydier et al. 10.1016/j.tecto.2021.229005
- Navigating the space of seismic anisotropy for crystal and whole-Earth scales A. Gupta et al. 10.1093/gji/ggaf134
- Can laboratory ultrasonic measurements on core plugs reproduce results obtained from sonic well logging in carbonates? A. El-Husseiny et al. 10.1016/j.jappgeo.2022.104745
- Application of Toroidal Coils to Obtain Electrical Resistivity of Core Samples: Mathematical Modeling M. Epov et al. 10.18599/grs.2024.3.16
- Impact of sub-basalt thrust systems on the Faroe continental shelf for the late Paleoproterozoic–Cenozoic tectonic evolution of the margin. J. Koehl et al. 10.12688/openreseurope.18284.1
- SAPHYR: Swiss Atlas of Physical Properties of Rocks: the continental crust in a database A. Zappone & E. Kissling 10.1186/s00015-021-00389-3
- Cross‐Scale Seismic Anisotropy Analysis in Metamorphic Rocks From the COSC‐1 Borehole in the Scandinavian Caledonides F. Kästner et al. 10.1029/2020JB021154
13 citations as recorded by crossref.
- Anisotropic velocity models for (3-D) seismic imaging of the Lower Seve Nappe in Jämtland, Sweden F. Kästner et al. 10.1093/gji/ggab339
- Elastic anisotropies of rocks in a subduction and exhumation setting M. Schmidtke et al. 10.5194/se-12-1801-2021
- Pressure, temperature and lithological dependence of seismic and magnetic susceptibility anisotropy in amphibolites and gneisses from the central Scandinavian Caledonides M. Bazargan et al. 10.1016/j.tecto.2021.229113
- Impact of sub-basalt thrust systems on the Faroe continental shelf for the late Paleoproterozoic–Cenozoic tectonic evolution of the margin. J. Koehl et al. 10.12688/openreseurope.18284.2
- Attenuation of Seismic Waves in Partially Saturated Berea Sandstone as a Function of Frequency and Confining Pressure N. Tisato et al. 10.3389/feart.2021.641177
- Seismic anisotropy of mid crustal orogenic nappes and their bounding structures: An example from the Middle Allochthon (Seve Nappe) of the Central Scandinavian Caledonides B. Almqvist et al. 10.1016/j.tecto.2021.229045
- Core‐Log‐Seismic Integration in Metamorphic Rocks and Its Implication for the Regional Geology: A Case Study for the ICDP Drilling Project COSC‐1, Sweden J. Elger et al. 10.1029/2020GC009376
- Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone imaging T. Leydier et al. 10.1016/j.tecto.2021.229005
- Navigating the space of seismic anisotropy for crystal and whole-Earth scales A. Gupta et al. 10.1093/gji/ggaf134
- Can laboratory ultrasonic measurements on core plugs reproduce results obtained from sonic well logging in carbonates? A. El-Husseiny et al. 10.1016/j.jappgeo.2022.104745
- Application of Toroidal Coils to Obtain Electrical Resistivity of Core Samples: Mathematical Modeling M. Epov et al. 10.18599/grs.2024.3.16
- Impact of sub-basalt thrust systems on the Faroe continental shelf for the late Paleoproterozoic–Cenozoic tectonic evolution of the margin. J. Koehl et al. 10.12688/openreseurope.18284.1
- SAPHYR: Swiss Atlas of Physical Properties of Rocks: the continental crust in a database A. Zappone & E. Kissling 10.1186/s00015-021-00389-3
Latest update: 19 Jun 2025
Short summary
Knowledge about physical properties at depth is crucial to image and understand structures linked with orogenic processes. We examined seismic velocities from core and downhole data from the COSC-1 borehole, Sweden, and calibrated our results with laboratory measurements on core samples. Despite a strong mismatch between the core and downhole velocities due to microcracks, mafic units are resolved at all scales, while at sample scale, strong seismic anisotropy correlates with the rock foliation.
Knowledge about physical properties at depth is crucial to image and understand structures...
