δ¹⁸O, δ¹³C, Δ₄₇ (clumped) and ⁸⁷Sr/⁸⁶Sr isotopic compositions, and trace element concentrations of calcite veins pervading the Troodos pillow lavas
Calcite veins pervading the pillow lava section of the Troodos ophiolite document fracturing and fluid flow through the oceanic crust. Their δ¹⁸O, δ¹³C, Δ₄₇ (clumped) and ⁸⁷Sr/⁸⁶Sr isotopic compositions, and trace element concentratios (laser ablation) provide insights into the fluid composition from which they precipitated and the precipitation temperature.
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