uu.seUppsala University Publications
Change search
ReferencesLink to record
Permanent link

Direct link
Seismic anisotropy in the Morcles nappe shear zone: Implications for seismic imaging of crustal scale shear zones
Uppsala University, Disciplinary Domain of Science and Technology, Earth Sciences, Department of Earth Sciences, Geophysics.
Show others and affiliations
2013 (English)In: Tectonophysics, ISSN 0040-1951, E-ISSN 1879-3266, Vol. 603, 162-178 p.Article in journal (Refereed) Published
Abstract [en]

Microstructures and textures of calcite mylonites from the Morcles nappe large-scale shearzone in southwestern Switzerland develop principally as a function of 1) extrinsic physical parameters including temperature, stress, strain, strain rate and 2) intrinsic parameters, such as mineral composition. We collected rock samples at a single location from this shear zone, on which laboratory ultrasonic velocities, texture and microstructures were investigated and quantified. The samples had different concentration of secondary mineral phases (<5 up to 40 vol.%). Measured seismic P waveanisotropy ranges from 6.5% for polyphase mylonites (similar to 40 vol.%) to 18.4% in mylonites with <5 vol.% secondary phases. Texture strength of calcite is the main factor governing the seismic P wave anisotropy. Measured S wave splitting is generally highest in the foliation plane, but its origin is more difficult to explain solely by calcite texture. Additional texture measurements were made on calcite mylonites with low concentration of secondary phases (<= 10 vol.%) along the metamorphic gradient of the shear zone (15 km distance). A systematic increase in texture strength is observed moving from the frontal part of the shear zone (anchimetamorphism: 280 degrees C) to the higher temperature, basal part (greenschist facies: 350-400 degrees C). Calculated P wave velocities become increasingly anisotropic towards the high-strain part of the nappe, from an average of 5.8%in the frontal part to 13.2% in the root of the basal part. Secondary phases raise an additional complexity, and may act either to increase or decrease seismic anisotropy of shear zone mylonites. Inlight of our findings we reinterpret the origin of some seismically reflective layers in the Grone-Zweisimmen line in southwestern Switzerland (PNR20 Swiss National Research Program). We hypothesize that reflections originate in part from the lateral variation in textural and microstructural arrangement of calcite mylonites in shear zones. 

Place, publisher, year, edition, pages
2013. Vol. 603, 162-178 p.
National Category
Geology Geophysics
URN: urn:nbn:se:uu:diva-205827DOI: 10.1016/j.tecto.2013.05.025ISI: 000324450100013OAI: oai:DiVA.org:uu-205827DiVA: diva2:642707
Available from: 2013-08-23 Created: 2013-08-23 Last updated: 2016-01-05

Open Access in DiVA

No full text

Other links

Publisher's full text

Search in DiVA

By author/editor
Almqvist, Bjarne
By organisation
In the same journal

Search outside of DiVA

GoogleGoogle Scholar

Altmetric score

Total: 234 hits
ReferencesLink to record
Permanent link

Direct link