The nature of the groundmass of surficial suevite from the Ries impact structure, Germany, and constraints on its origin-Reference-Cited by-同舟云学术

The nature of the groundmass of surficial suevite from the Ries impact structure, Germany, and constraints on its origin

Published:2004-10 Issue:10 Volume:39 Page:1655-1683
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:

Author:

OSINSKI Gordon R.,GRIEVE Richard A. F.,SPRAY John G.

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1945-5100.2004.tb00065.x/fullpdf

Reference84 articles.

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2. Petrofabric examination of the main suevite of the Otting Quarry, Nördlinger Ries, Germany;Bringemeier;Meteoritics,1994

3. Structural controls on the solubility of CO2 in silicate melts. Part I: Bulk solubility data;Brooker;Chemical Geology,2001

4. 40Ar/39Ar laser probe age determination confirms the Ries impact crater as the source of glass clasts in Graupensand sediments (Grimmelfingen formation, North Alpine Foreland basin);Buchner;International Journal of Earth Sciences,2003

5. Thermal history of impact melt rocks in the Fennoscandian shield;Carstens;Contributions to Mineralogy and Petrology,1975

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