Fe-oxide concretions formed by interacting carbonate and acidic waters on Earth and Mars-Reference-Cited by-同舟云学术

Fe-oxide concretions formed by interacting carbonate and acidic waters on Earth and Mars

Published:2018-12-07 Issue:12 Volume:4 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Yoshida H.¹,Hasegawa H.¹²^ORCID,Katsuta N.³,Maruyama I.⁴^ORCID,Sirono S.⁴^ORCID,Minami M.⁵,Asahara Y.⁴^ORCID,Nishimoto S.⁶,Yamaguchi Y.⁴^ORCID,Ichinnorov N.⁷,Metcalfe R.⁸

Affiliation:

1. Material Research Section, Nagoya University, University Museum, Nagoya, Japan.

2. Faculty of Science and Technology, Kochi University, Kochi, Japan.

3. Faculty of Education, Gifu University, Gifu, Japan.

4. Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan.

5. Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, Japan.

6. Nagoya City Science Museum, Nagoya, Japan.

7. Institute of Paleontology and Geology, Mongolian Academy of Science, Mongolia.

8. Quintessa Limited, The Hub, Henley-on-Thames, Oxfordshire, UK.

Abstract

We propose a new model for the Fe-oxide concretion formation on Earth and that can also explain the early martian history.

Funder

JSPS

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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