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(Supplemental Materials, Table 5) Major and trace elements compositions of al...
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(Supplemental Material, Table 7) Temperature data from probes inserted in cra...
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(Suppplemental Materials, Table 4) Location and depth of rock samples collect...
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(Supplemental Materials, Table 2) Observations from images collected by the r...
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(Table S2) Age determination of corals from the Tasmanian Seamounts
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(Table S8) Amphibole-plagioclase thermometry reconstruction for Pito Deep sam...
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(Table S7) Epidote compositions of Pito Deep samples
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(Table S6) Amphibole compositions of Pito Deep samples
Mineral formulas were recalculated on the basis of 23 anhydrous oxygens, using the 15 NK procedure of Robinson (1982). -
(Table S5) Chlorite and chlorite-smectite compositions of Pito Deep samples
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(Table S4) Clinopyroxene compositions of Pito Deep samples
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(Table S3) Plagioclase compositions of Pito Deep samples
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(Table S2) Summary of petrographic charactersitics of Pito Deep samples
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(Table S1) Bulk rock compositions of selected sheeted dikes of Pito Deep
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(Table 2) Lead isotope analyses for selected Pito Deep Rift samples
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(Table 1) Recalculated major element compositions of Pito Deep Rift dikes and...
Major element values recalculated after converting Fe2O3 to FeO. Analytical totals have been conserved in the recalcluation. -
(Table 1) Major and trace element composition of Pito Deep Rift dikes and lavas
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(Appendix) Petrographic information, trace element and Sr isotope ratios of P...
Fluid flow through the axial hydrothermal system at fast spreading ridges is investigated using the Sr-isotopic composition of upper crustal samples recovered from a tectonic... -
(Appendix A) Sulphur isotope ratios of upper crust samples of the sheeted dyk...
The behaviour of seawater sulphate in hydrothermal systems at intermediate- to fast-spreading ridges is investigated using new analyses of the d34S, sulphur concentration and...
