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. 2024 Dec 3;121(49):e2416680121.
doi: 10.1073/pnas.2416680121. Epub 2024 Nov 22.

Metamorphism in a wet Martian middle crust

Affiliations

Metamorphism in a wet Martian middle crust

Richard Palin et al. Proc Natl Acad Sci U S A. .
No abstract available

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Conflict of interest statement

Competing interests statement:The authors declare no competing interest.

Figures

Fig. 1.
Fig. 1.
Petrogenetic grid showing metamorphic mineral assemblages stable across Martian pressure–temperature–depth ranges relevant to the work of Wright et al. [modified after (4)]. Zeo—zeolite facies; PrA—prehnite actinolite facies; PP—prehnite pumpellyite facies; PA—pumpellyite actinolite facies; GR—greenschist facies. Mineral assemblages are indicated by ACF diagrams and abbreviations are actinolite (Act), chlorite (Chl), laumontite (Lm), lawsonite (Lws), pumpellyite (Pm), prehnite (Pr), and zoisite (Zo). The red square represents the chemical composition of Martian basalt (9).

References

    1. Wright V., Morzfeld M., Manga M., Liquid water in the Martian mid-crust. Proc. Natl. Acad. Sci. U.S.A. 121, e2409983121 (2024). - PMC - PubMed
    1. Wade J., Dyck B., Palin R. M., Moore J. D., Smye A. J., The divergent fates of primitive hydrospheric water on Earth and Mars. Nature 552, 391–394 (2017). - PubMed
    1. Scheller E., Ehlmann B., Hu R., Adams D., Yung Y., Long-term drying of Mars by sequestration of ocean-scale volumes of water in the crust. Science 372, 56–62 (2021). - PMC - PubMed
    1. McSween H. Y. Jr., Labotka T. C., Viviano-Beck C. E., Metamorphism in the Martian crust. Meteorit. Planet. Sci. 50, 590–603 (2015).
    1. Zen E. A., Prehnite-and pumpellyite-bearing mineral assemblages, west side of the Appalachian metamorphic belt, Pennsylvania to Newfoundland. J. Petrol. 15, 197–242 (1974).

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