Strontium and oxygen isotope decoupling in the Hercynian Trois Seigneurs Massif, Pyrenees: evidence for fluid circulation in a brittle regime
- 1 January 1990
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 104 (3) , 332-347
- https://doi.org/10.1007/bf00321488
Abstract
No abstract availableKeywords
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