Evidence for a spatially extensive hydrothermal system at the Ries impact structure, Germany

The ~15 Ma, 26 km diameter Ries impact structure in south‐central Germany was one of the first terrestrial impact structures where evidence of impact‐associated hydrothermal alteration was recognized. Previous studies suggested that pervasive, high‐temperature hydrothermal activity was restricted to...

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Veröffentlicht in:	Meteoritics & planetary science 2017-02, Vol.52 (2), p.351-371
Hauptverfasser:	Sapers, H. M., Osinski, G. R., Flemming, R. L., Buitenhuis, E., Banerjee, N. R., Tornabene, L. L., Blain, S., Hainge, J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Alterations Calcite Clinochlore Craters Dynamical systems Ejecta Hydrothermal systems Smectites
Online-Zugang:	Volltext
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