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Supplemental Material: Sr-Nd-Ca isotopic variations of Cenozoic calc-alkaline and alkaline volcanic rocks above a slab tear in Western Anatolia, Turkey

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journal contribution
posted on 2023-06-12, 13:34 authored by Hao DengHao Deng, et al.

 Supplemental Text S1: Corresponding detailed descriptions of the analytical methods. Figure S1: (a) SiO2 versus Na2O + K2O classification diagram from Middlemost (1994); (b) Zr/TiO2 versus Nb/Y classification from Winchester and Floyd (1977); (c) SiO2 versus K2O diagram. Figure S2: Variation diagrams of δ44/40Ca values versus LOI contents. Figure S3: Variation diagrams of CaO, Al2O3 and Eu/Eu* versus SiO2 for the Gördes dacites. Figure S4: Variation diagrams of SiO2, Nb/Nb* and La/Smcn versus 87Sr/86Sri for the Gördes dacites. Figure S5: Variation diagrams of MgO, TFe2O3, CaO and CaO/Al2O3 versus SiO2 for the Kula basalts. Figure S6: Variation diagrams of SiO2, La/Smcn, Nb/Nb* versus ɛNd (t) and 1/Sr versus (87Sr/86Sr)i for the Kula basalts. Figure S7: Variation diagrams of La/Sm versus Sm/Yb. Figure S8: Selected cathodoluminescence images and U-Pb concordia diagrams of analyzed zircons of dacites. Table S1: SHRIMP U-Pb data for zircons from Gördes dacites. Table S2: Major and trace elemental compositions of dacites and basalts. Table S3: Measured and recommended trace element concentrations (ppm) for AGV-2, BHVO-2, BCR-2 and RGM2. Table S4: Whole rock Sr-Nd compositions and calculations of basalts and dacites. Table S5: (a) Modeling calculation of Ca isotope fractionation during partial melting of spinel peridotite, (b) modeling calculation of Ca isotope fractionation during partial melting of garnet peridotite, and (c) modeling calcium isotope fractionation during partial melting of garnet pyroxenite. 

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