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COUPLED 142ND–143ND EVIDENCE FOR A PROTRACTED MAGMA OCEAN IN MARS

Debaille, V., Brandon, A. D., Yin, Q. Z., Jacobsen, B.(2007). COUPLED 142ND–143ND EVIDENCE FOR A PROTRACTED MAGMA OCEAN IN MARS. NATURE, 450(7169), 525-528. https://doi.org/10.1038/nature06317

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Datasets

numbertitleMethodsvariables analyzed
1Sm-Nd isotope values for shergottitesCALC, TIMSE_Nd142, E_Nd143(T), Sm147_Nd144
S1Sm-Nd isotope and concentration data for Martian meteoritesICPMS-ID, CALC, TIMSSm, Nd, E_Nd142, E_Nd(T), E_Nd143(T), Nd143_Nd144, Sm147_Nd144
S2Nd isotopic compositions measured in this studyTIMS, CALC, ICPMS-IDNd146_Nd144, E_Nd150, E_Nd143(T), Ce142, Nd142_Nd144, E_Nd143, Nd143_Nd144, Nd148_Nd144, E_Nd142, Nd150_Nd144, E_Nd148, Nd145_Nd144

Methods

method namelaboratorymethod comment More details are available for the following variables
CALCULATEDUNKNOWNN/A
INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRY ISOTOPE DILUTIONUNIVERSITY OF CALIFORNIA - DAVISNu Plasma
THERMAL IONIZATION MASS SPECTROMETRYJOHNSON SPACE CENTERnine faraday cup Triton Nd143_Nd144[IR], Nd142_Nd144[IR], Nd145_Nd144[IR], Nd148_Nd144[IR], Nd150_Nd144[IR]

Samples

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