Research Article
Fluid Dynamics in a Thrust Fault Inferred from Petrology and Geochemistry of Calcite Veins: An Example from the Southern Pyrenees
Figure 9
(a) Crossplot showing the δ18O and δ13C compositions of the calcite cements, host rocks, and fault rocks (carbonate matrix from the cataclasite). Cretaceous marine limestone values (green box) are from [53]. (b) δ18O values of the calcite cements versus δ18O values of the related host rocks.
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