Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle

This repository includes dataset used in the following article:Oyanagi, R., Okamoto, A., Satish-Kumar, M., Minami, M., Harigane, Y., Michibayashi, K. (2021) Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle, <i>Communications Earth &amp; Environment</i>. <br><br>Contents<b>thermoLT600bat.dat</b> : Thermodynamic dataset for Geochemist's Workbench.<br><br><b>result_ReactionPathModeling(FigureS5).xlsx</b> : Summary of the reaction path calculation used in Supplementary Figure 5.<br><br><b>X-ray CT data.zip</b> : X-ray CT data of serpentinized peridotite in DICOM format. These data are used in Figure 2d in the paper.<br><b>X-rayCT_movie.avi</b> : Field of view is 3 mm diameter. Dark gray part is serpentine. Light gray part is aragonite. Their intermediate is olivine. White part is spinel and magnetite.<br><b>Supplementary_Table_1.xlsx: </b> <b> </b>Microsoft Excel spreadsheet of the supplementary table 1.<br><br><b>Supplementary_Table_2.xlsx: </b> <b> </b>Microsoft Excel spreadsheet of the supplementary table 2.<br><br><b>Supplementary_Table_3.xlsx: </b> <b> </b>Microsoft Excel spreadsheet of the supplementary table 3.<br>