Crustal-derived CO<sub>2</sub> production from plutons in carbonate is driven by shallow metamorphic decarbonation not assimilation
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Data tables S1 through S7 that accompany the following paper submitted to <i>Geochemistry, Geophysics, Geosystems</i> (DOI will be provided once available).Table S1: Bulk-rock major element (wt.%) and trace element (ppm) composition for hand samplesTable S2: <sup>87</sup>Sr/<sup>86</sup>Sr isotope compositions for bulk rock powdersTable S3: Oxygen isotope (d<sup>18</sup>O ‰ VSMOW) compositions for bulk rock powders and clinopyroxeneTable S4: Carbon (d<sup>13</sup>C ‰ VPDB) and isotope (d<sup>18</sup>O ‰ VSMOW) compositions for Quatsino limestoneTable S5: Electron Probe Micro-Analyses Phase CompositionsTable S6: Laser Ablation Inductively Coupled Mass Spectrometry Phase CompositionsTable S7: CO<sub>2</sub> mass and flux calculations<br>
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Morris, Rebecca创建时间：
2024-01-23
