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Dolomitisation and brecciation along fault zones in the Cantabrian mountains

Dolomitisation, brecciation, and dedolomitisation occurring in fault zones in the Variscan fold and thrust belt in the Cantabrian Zone (Northern Spain) in three different tectonic units (Ponga, Picos de Europa and Esla) have been investigated and compared. Cementation patterns are similar in all uni...

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Hauptverfasser: Grimmer, Jörg O. W. (VerfasserIn) , Bakker, Ronald J. (VerfasserIn) , Zeeh, Stefan (VerfasserIn) , Bechstädt, Thilo (VerfasserIn)
Dokumenttyp: Article (Journal)
Sprache:Englisch
Veröffentlicht: June 2000
In: Journal of geochemical exploration
Year: 2000, Jahrgang: 69/70, Pages: 153-158
DOI:10.1016/S0375-6742(00)00122-9
Online-Zugang:Verlag, Volltext: http://dx.doi.org/10.1016/S0375-6742(00)00122-9
Verlag, Volltext: http://www.sciencedirect.com/science/article/pii/S0375674200001229
Volltext
Verfasserangaben:J.O.W Grimmer, R.J. Bakker, S. Zeeh, T. Bechstädt

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