Martian low-temperature alteration materials in shock-melt pockets in Tissint: Constraints on their preservation in shergottite meteorites
Author:
Funder
NSERC
Canadian Space Agency
Caltech
University of Alberta
ICP
MS
JPL
NASA
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference62 articles.
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2. Raman spectroscopic properties and Raman identification of CaS-MgS-MnS-FeS-Cr2FeS4 sulfides in meteorites and reduced sulfur-rich systems;Avril;Meteorit. Planet. Sci.,2013
3. Petrology and trace element geochemistry of Tissint, the newest shergottite fall;Balta;Meteorit. Planet. Sci.,2015
4. The Tatahouine diogenite; mineralogical chemical effects of sixty-three years of terrestrial residence;Barrat;Meteorit. Planet. Sci.,1999
5. No Martian soil component in shergottite meteorites;Barrat;Geochim. Cosmochim. Acta,2014
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1. The source craters of the martian meteorites: Implications for the igneous evolution of Mars;Science Advances;2024-08-16
2. Isotopic and trace element data of Tissint indicate a homogeneous strewn field, mobilization of Sr, REE, and Pb during shock metamorphism, and limits on the incorporation of martian surficial materials in impact melt glass;Geochimica et Cosmochimica Acta;2022-06
3. Survey of impact glasses in shergottites searching for Martian sulfate using X-ray absorption near-edge structure;Geochimica et Cosmochimica Acta;2021-11
4. What Martian Meteorites Reveal About the Interior and Surface of Mars;Journal of Geophysical Research: Planets;2020-12
5. Hydrogen Isotopic Variations in the Shergottites;Geosciences;2020-04-17
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