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Silicic volcanism on Mars evidenced by tridymite in high-SiO(2) sedimentary rock at Gale crater

Tridymite, a low-pressure, high-temperature (>870 °C) SiO(2) polymorph, was detected in a drill sample of laminated mudstone (Buckskin) at Marias Pass in Gale crater, Mars, by the Chemistry and Mineralogy X-ray diffraction instrument onboard the Mars Science Laboratory rover Curiosity. The tridym...

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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: Morris, Richard V., Vaniman, David T., Blake, David F., Gellert, Ralf, Chipera, Steve J., Rampe, Elizabeth B., Ming, Douglas W., Morrison, Shaunna M., Downs, Robert T., Treiman, Allan H., Yen, Albert S., Grotzinger, John P., Achilles, Cherie N., Bristow, Thomas F., Crisp, Joy A., Des Marais, David J., Farmer, Jack D., Fendrich, Kim V., Frydenvang, Jens, Graff, Trevor G., Morookian, John-Michael, Stolper, Edward M., Schwenzer, Susanne P.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2016
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC4932983/
https://ncbi.nlm.nih.gov/pubmed/27298370
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1607098113
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