Paleo water–rock interaction determined through isotopic...

Paleo water–rock interaction determined through isotopic tracing (Sr, O, C, U) in fracture-fill minerals: Evidence from the Vienne granitoids (France)

Négrel, Philippe, Casanova, Joël, Bourguignon, Anne
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Volume:
34
Language:
english
Journal:
Applied Geochemistry
DOI:
10.1016/j.apgeochem.2012.11.010
Date:
July, 2013
File:
PDF, 3.50 MB
english, 2013
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