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.

Elger, Judith , Berndt, Christian , Kästner, Felix, Pierdominici, Simona, Kück, Jochem, Almqvist, Bjarne S. G., Juhlin, Christopher and Lorenz, Henning (2021) 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. Open Access Geochemistry, Geophysics, Geosystems, 22 (3). e2020GC009376. DOI 10.1029/2020GC009376.

[thumbnail of Figure] Other (Figure)
2020gc009376-sup-0001-figure - Supplemental Material
Available under License Creative Commons: Attribution 4.0.

Download (534kB)
[thumbnail of Figure] Other (Figure)
2020gc009376-sup-0002-figure - Supplemental Material
Available under License Creative Commons: Attribution 4.0.

Download (21MB)
[thumbnail of Text] Other (Text)
2020gc009376-sup-0003-text - Supplemental Material
Available under License Creative Commons: Attribution 4.0.

Download (889kB)
[thumbnail of 2020GC009376.pdf]
Preview
Text
2020GC009376.pdf - Published Version
Available under License Creative Commons: Attribution 4.0.

Download (5MB) | Preview

Supplementary data:

Abstract

Continental collision causes deformation in the crust along shear zones. However, the physical and chemical conditions at which these zones operate and the deformation processes that enable up to hundreds of km of tectonic transport are still unclear because of the depth at which they occur and the challenges in imaging them. Ancient exhumed collision zones allow us to investigate these processes much better, for example at the COSC‐1 borehole in the central Scandinavian Caledonides. This study combines data from the COSC‐1 borehole with different seismic measurements to provide constraints on the spatial lithological and textural configuration of the Seve Nappe Complex. This is one of the few studies that shows that core‐log‐seismic integration in metamorphic rocks allows to identify the spatial distribution of major lithological units. Especially gamma ray logs in combination with density data are powerful tools to distinguish between mafic and felsic lithologies in log‐core correlation. Our results indicate that reflections along the borehole are primarily caused by compositional rather than textural changes. Reflections in the Seve Nappe Complex are not as distinct as in greater depths but continuous and several of them can be linked to magmatic intrusions, which have been metamorphically overprinted. Their setting indicates that the Seve Nappe Complex consists of the remnants of a volcanic continental margin. Our results suggest that ductile‐deformed middle crustal reflectivity is primarily a function of pre‐orogenic lithological variations which has to be considered when deciphering mountain building processes.

Document Type: Article
Keywords: COSC‐1, Core‐log‐seismic integration, central Scandinavian Caledonides
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
Date Deposited: 07 Jan 2021 09:14
Last Modified: 07 Feb 2024 15:28
URI: https://oceanrep.geomar.de/id/eprint/51430

Actions (login required)

View Item View Item