Widening of Hydrous Shear Zones During Incipient Eclogitization of Metastable Dry and Rigid Lower Crust—Holsnøy, Western Norway-Reference-Cited by-同舟云学术

Widening of Hydrous Shear Zones During Incipient Eclogitization of Metastable Dry and Rigid Lower Crust—Holsnøy, Western Norway

Published:2021-03 Issue:3 Volume:40 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Kaatz Lisa¹^ORCID,Zertani Sascha¹^ORCID,Moulas Evangelos²^ORCID,John Timm¹^ORCID,Labrousse Loïc³,Schmalholz Stefan M.⁴^ORCID,Andersen Torgeir B.⁵^ORCID

Affiliation:

1. Institute of Geological Sciences Freie Universität Berlin Berlin Germany

2. Institute of Geosciences Johannes Gutenberg‐Universität Mainz Mainz Germany

3. Institut des Sciences de la Terre Paris Sorbonne Université UMR 7193 Paris France

4. Institute of Earth Sciences University of Lausanne, Géopolis Lausanne Switzerland

5. Department of Geosciences Centre of Earth Evolution and Dynamics (CEED) University of Oslo Oslo Norway

Funder

Deutsche Forschungsgemeinschaft

Norges Forskningsråd

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020TC006572

Reference72 articles.

1. The tectonic significance of pre-Scandian 40Ar/39Ar phengite cooling ages in the Caledonides of western Norway

2. Evidence for hyperextension along the pre-Caledonian margin of Baltica

3. Subduction and eduction of continental crust: major mechanisms during continent-continent collision and orogenic extensional collapse, a model based on the south Norwegian Caledonides

4. Eclogitization of lower crustal granulites by fluid migration through shear zones

5. Austrheim H.(1998).Influence of fluid and deformation on metamorphism of the deep crust and consequences for the geodynamics of collision zones. InWhen continents collide: Geodynamics and geochemistry of ultrahigh‐pressure rocks(pp.297–323). Dordrecht: Springer.

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