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The calcium isotope systematics of Mars

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F15%3A00000131" target="_blank" >RIV/00025798:_____/15:00000131 - isvavai.cz</a>

  • Result on the web

    <a href="http://www.sciencedirect.com/science/journal/0012821X" target="_blank" >http://www.sciencedirect.com/science/journal/0012821X</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.epsl.2015.08.016" target="_blank" >10.1016/j.epsl.2015.08.016</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The calcium isotope systematics of Mars

  • Original language description

    New Ca isotope data from a suite of Martian meteorites provide constraints on the Ca isotope composition of the Martian mantle and possible recycling of surface materials back into the mantle. A mean ?44/40Ca of 1.04 ? 0.09? (2SD) is estimated for the Martian mantle which can also be taken as an approximation for Bulk Silicate Mars. This value is identical with the estimates for Bulk Silicate Earth, and the inner Solar System planets can therefore be considered homogeneous with respect to Ca isotopes. The Ca isotope composition of two Martian dunites varies by ?0.3? despite strong chemical and mineralogical similarities and this difference can be caused by the presence of carbonate, probably of pre-terrestrial origin, implying a protracted period of the existence of CaCO3-rich fluids and sufficient amounts of CO2 on the surface of Mars. The variability of ?44/40Ca within the groups of shergottites and nakhlites (clinopyroxene cumulates) cannot be related to partial melting and fraction

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DD - Geochemistry

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/GA13-22351S" target="_blank" >GA13-22351S: Combined use of novel and traditional stable isotope systems in identifying source components and processes of moldavite formation</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2015

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Earth and Planetary Science Letters

  • ISSN

    0012-821X

  • e-ISSN

  • Volume of the periodical

    430

  • Issue of the periodical within the volume

    November

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    9

  • Pages from-to

    86-94

  • UT code for WoS article

    000363070600009

  • EID of the result in the Scopus database