Variation in Magnetic Fabrics at Low Shock Pressure Due to Experimental Impact Cratering-Reference-Cited by-同舟云学术

Variation in Magnetic Fabrics at Low Shock Pressure Due to Experimental Impact Cratering

Published:2019-08 Issue:8 Volume:124 Page:9095-9108
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Agarwal Amar¹^ORCID,Kontny Agnes²^ORCID,Kenkmann Thomas¹^ORCID,Poelchau Michael H.¹

Affiliation:

1. Institut für Geo‐ und Umweltnaturwissenschaften Albert‐Ludwigs‐Universität Freiburg Freiburg Germany

2. Institute of Applied Geosciences Karlsruhe Institute of Technology Karlsruhe Germany

Funder

Deutsche Forschungsgemeinschaft

Alexander von Humboldt-Stiftung

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JB017128

Reference65 articles.

1. Relationships among magnetic fabrics, microfractures and shock pressures at an impact crater: A case study from Lockne crater, Sweden

2. Shock pressure estimates in target basalts of a pristine crater: A case study in the Lonar crater, India;Agarwal A.;Geological Society of America Bulletin,2016

3. Agarwal A. Poelchau M.H. Kenkmann T. 2019.Kinked biotite as a strain marker in experimental impact craters in gneiss. in: Lunar and Planetary Science Conference.

4. Alternating augite-plagioclase wedges in basement dolerites of Lockne impact structure, Sweden: A new shock wave-induced deformation feature

5. Lingunite-a high-pressure plagioclase polymorph at mineral interfaces in doleritic rock of the Lockne impact structure (Sweden)

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