Fluid Dynamics in a Thrust Fault Inferred from Petrology and Geochemistry of Calcite Veins: An Example from the Southern Pyrenees
Table 1
δ18O, δ13C, and 87Sr/86Sr isotopic signature of the calcite cements, fault rocks, and host rocks. The ,δ18Ofluid, and precipitation temperatures obtained from clumped isotopes are also included. Fw means footwall and Hw means hanging wall.