Cross‐scale seismic anisotropy analysis in metamorphic rocks from the COSC‐1 borehole in the Scandinavian Caledonides.

Kästner, Felix, Pierdominici, Simona, Zappone, Alba, Morales, Luiz F. G., Schleicher, Anja M., Wilke, Franziska D. H. and Berndt, Christian (2021) Cross‐scale seismic anisotropy analysis in metamorphic rocks from the COSC‐1 borehole in the Scandinavian Caledonides. Open Access Journal of Geophysical Research: Solid Earth, 126 (5). e2020JB021154. DOI 10.1029/2020JB021154.

[thumbnail of Supporting information] Other (Supporting information)
2020jb021154-sup-0001-supporting - Supplemental Material
Available under License Creative Commons: Attribution 4.0.

Download (2MB)
[thumbnail of 2020JB021154.pdf]
Preview
Text
2020JB021154.pdf - Published Version
Available under License Creative Commons: Attribution 4.0.

Download (5MB) | Preview

Supplementary data:

Abstract

Metamorphic and deformed rocks in thrust zones show particularly high seismic anisotropy causing challenges for seismic imaging and interpretation. A good example is the Seve Nappe Complex in central Sweden, an old exhumed orogenic thrust zone that is characterized by a strong but incoherent seismic reflectivity and considerable seismic anisotropy. However, only little is known about their origin in relation to composition and structural influences on measurements at different seismic scales. Here, we present a new integrative study of cross‐scale seismic anisotropy analyses combining mineralogical composition, microstructural analyses and seismic laboratory experiments from the COSC‐1 borehole, which sampled a 2.5 km‐deep section of metamorphic rocks deformed in an orogenic root now preserved in the Lower Seve Nappe. While there is strong crystallographic preferred orientation in most samples in general, variations in anisotropy depend mostly on bulk mineral composition and dominant core lithology as shown by a strong correlation between these. This relationship enables to identify three distinct seismic anisotropy facies providing a continuous anisotropy profile along the borehole. Moreover, comparison of laboratory seismic measurements and electron‐backscatter diffraction data reveals a strong scale‐dependence, which is more pronounced in the highly deformed, heterogeneous samples. This highlights the need for comprehensive cross‐validation of microscale anisotropy analyses with additional lithological data when integrating seismic anisotropy over seismic scales.

Document Type: Article
Keywords: seismic anisotropy, electron‐backscatter diffraction, core measurements, COSC
Research affiliation: HGF-GFZ
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Main POF Topic: PT3: Restless Earth
Refereed: Yes
Open Access Journal?: No
Publisher: AGU (American Geophysical Union), Wiley
Projects: SPP 1006
Date Deposited: 06 Apr 2021 13:15
Last Modified: 07 Feb 2024 15:40
URI: https://oceanrep.geomar.de/id/eprint/52221

Actions (login required)

View Item View Item