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Trace element compositions of the clinopyroxene from andesites from the Kueis...
This dataset reports in situ trace elements of clinopyroxene of andesite from Kueishantao, north of Taiwan, China. Trace element compositions were obtained with LA-ICP-MS at the... -
Serpentine and brucite compositions of serpentinites from IODP Expedition 366
Number of cations based on 7 O. Abbreviations: cpfu, cations per formula unit. -
Orthopyroxene compositions of serpentinites from IODP Expedition 366
Number of cations based on 6 O. Abbreviations: cpfu, cations per formula unit. -
Clinopyroxene compositions of serpentinites from IODP Expedition 366
Number of cations based on 6 O. Abbreviations: cpfu, cations per formula unit. -
Olivine compositions of serpentinites from IODP Expedition 366
Number of cations based on 4 O. Abbreviations: cpfu, cations per formula unit. -
In situ elemental, Sr isotope composition of plagioclase and elemental compos...
This dataset reports in situ major and trace elements, Sr isotopic ratios of plagioclase and in situ major and trace elements of clinopyroxene of andesite from Kueishantao,... -
Mineral geochemical data of serpentinites from the Mariana serpentinite mud v...
Mineral geochemical data of drill core serpentinites from the Mariana serpentinite mud volcanoes (IODP Exp. 366), including major element and fluid-mobile element (Li, B, Rb,... -
Major element compositions of the clinopyroxenes from andesites from the Kuei...
This dataset reports in situ major elements of clinopyroxene of andesite from Kueishantao, north of Taiwan, China. Major element compositions of Cpx were obtained with a JEOL... -
In-situ Sr isotopes for plagioclase from andesites from the Kueishantao islan...
This dataset reports Sr isotopic ratios of plagioclase of andesite from Kueishantao, north of Taiwan, China. Sr isotope ratios of Pl were measured by a Neptune Plus MC-ICP-MS... -
Spinel compositions of serpentinites from IODP Expedition 366
Number of cations based on 4 O. Abbreviations: cpfu, cations per formula unit.
