Articles | Volume 11, issue 2
https://doi.org/10.5194/se-11-607-2020
https://doi.org/10.5194/se-11-607-2020
Research article
 | 
23 Apr 2020
Research article |  | 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, Simona Pierdominici, Judith Elger, Alba Zappone, Jochem Kück, and Christian Berndt

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Felix Kästner on behalf of the Authors (03 Mar 2020)  Author's response   Manuscript 
ED: Publish as is (11 Mar 2020) by Michal Malinowski
ED: Publish as is (11 Mar 2020) by CharLotte Krawczyk (Executive editor)
AR by Felix Kästner on behalf of the Authors (12 Mar 2020)
Download
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.