Baddeleyite microstructural response to shock metamorphism in three enriched shergottites and implications for U–Pb geochronology-Reference-Cited by-同舟云学术

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Baddeleyite microstructural response to shock metamorphism in three enriched shergottites and implications for U–Pb geochronology

Published:2024-02 Issue: Volume:366 Page:267-283
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Sheen A.I.^ORCID,Herd C.D.K.^ORCID,Staddon L.G.,Darling J.R.^ORCID,Schwarz W.H.^ORCID,Tait K.T.^ORCID

Funder

Canadian Space Agency

Natural Sciences and Engineering Research Council of Canada

Science and Technology Facilities Council

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference90 articles.

1. Symplectites derived from metastable phases in martian basaltic meteorites;Aramovich;Am. Min.,2002

2. Beaty, D. W., the iMost Team, 2019. The potential science and engineering value of samples delivered to Earth by Mars sample return. Meteorit. Planet. Sci. 54 S3–S152.

3. Timescales of shock processes in chondritic and martian meteorites;Beck;Nature,2005

4. Pb-isotopic evidence for an early, enriched crust on Mars;Bellucci;Earth Planet. Sci. Lett.,2015

5. A Pb isotopic resolution to the Martian meteorite age paradox;Bellucci;Earth Planet. Sci. Lett.,2016

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