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Ferric saponite and serpentine in the nakhlite martian meteorites

Hicks, L. J., Bridges, J. C., Gurman, S. J.(2014). Ferric saponite and serpentine in the nakhlite martian meteorites. Geochimica et Cosmochimica Acta, 136, 194-210. https://doi.org/10.1016/j.gca.2014.04.010

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Datasets

numbertitleMethodsvariables analyzed
1Compositions of Lafayette apatite and siderite and NWA 817 terrestrial calciteSEM, CALCF, TOTAL, MnO, FeO, P2O5, CaO, SiO2, Cl, Na2O, CO2
2Compositions of saponite and serpentine phyllosilicates in Lafayette, and amorphous vein deposits across the nakhlitesXANES, EMPFeO, MgO, SO3, CaO, MnO, SiO2, Al2O3, TiO2, TOTAL, Cl, Fe2O3, P2O5, Na2O, K2O
3Six Fe-silicate standards and two Fe-silicate nakhlite grains with Fe-K XANES 1s!3d pre-edge absorption centroid positions and their known or calculated Fe3+/ΕFe ratiosXANESFe3_SUMFe
4Fe-K XANES measurements (eV), Fe3+/EFe ratios and Fe–O bond lengthsXANESFe3_SUMFe

Methods

method namelaboratorymethod comment More details are available for the following variables
CALCULATEDUNKNOWNfor CO2 value only, calculated by difference of probe analysis from 100 wt% oxide
ELECTRON MICROPROBEOPEN UNIVERSITYCameca SX100 measurements made using TAP, LTAP, LLiF, LPET, and PET crystal spectrometers, a 10 um defocused beam, at an accelerating voltage of 20 kV, and beam current 20 nA
SCANNING ELECTRON MICROSCOPEUNIVESITY OF LEICESTERPhilips XL30 accelerating voltage of 20 kV and beam current of ~1.0 nA
X-RAY ABSORPTION NEAR-EDGE STRUCTURE SPECTROSCOPYUNKNOWNeV

Samples

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