Quartz and cristobalite ballen in impact melt rocks from the Ries impact structure, Germany, formed by dehydration of shock‐generated amorphous phases-Reference-Cited by-同舟云学术

Quartz and cristobalite ballen in impact melt rocks from the Ries impact structure, Germany, formed by dehydration of shock‐generated amorphous phases

Published:2020-11 Issue:11 Volume:55 Page:2360-2374
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Trepmann Claudia A.¹^ORCID,Dellefant Fabian¹,Kaliwoda Melanie²,Hess Kai‐Uwe¹,Schmahl Wolfgang W.¹²,Hölzl Stefan³

Affiliation:

1. Department of Earth and Environmental Sciences Ludwig‐Maximilians‐University 80333 Munich Germany

2. Mineralogische Staatssammlung Staatliche naturwissenschaftliche Sammlungen Bayerns 80333 Munich Germany

3. RiesKraterMuseum Staatliche naturwissenschaftliche Sammlungen Bayerns 86720 Nördlingen Germany

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13590

Reference38 articles.

1. Diaplectic labradorite glass from the manicouagan impact crater

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3. Raman microprobe (RMP) determinations of natural and synthetic coesite;Boyer H.;Physics and Chemistry of Minerals,1985

4. Establishing a 14.6 ± 0.2 Ma age for the Nördlinger Ries impact (Germany)-A prime example for concordant isotopic ages from various dating materials

5. Thermal history of impact melt rocks in the Fennoscandian shield

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