Zinc and germanium in the sedimentary rocks of Gale Crater on Mars indicate hydrothermal enrichment followed by diagenetic fractionation-Reference-Cited by-同舟云学术

Zinc and germanium in the sedimentary rocks of Gale Crater on Mars indicate hydrothermal enrichment followed by diagenetic fractionation

Published:2017-08 Issue:8 Volume:122 Page:1747-1772
ISSN:2169-9097
Container-title:Journal of Geophysical Research: Planets
language:en
Short-container-title:J. Geophys. Res. Planets

Author:

Berger Jeff A.¹^ORCID,Schmidt Mariek E.²^ORCID,Gellert Ralf³^ORCID,Boyd Nicholas I.³,Desouza Elstan D.³,Flemming Roberta L.¹,Izawa Matthew R. M.²^ORCID,Ming Douglas W.⁴^ORCID,Perrett Glynis M.⁵^ORCID,Rampe Elizabeth B.⁶^ORCID,Thompson Lucy M.⁷^ORCID,VanBommel Scott J. V.³^ORCID,Yen Albert S.⁸

Affiliation:

1. Department of Earth Sciences; University of Western Ontario; London Ontario Canada

2. Department of Earth Sciences; Brock University; St. Catharines Ontario Canada

3. Guelph-Waterloo Physics Institute; University of Guelph; Guelph Ontario Canada

4. Astromaterials Research and Exploration Science Division; NASA Johnson Space Center; Houston Texas USA

5. Cornell Center for Astrophysics and Planetary Science; Cornell University; Ithaca New York USA

6. Aerodyne Industries, Jacobs JETS Contract; NASA Johnson Space Center; Houston Texas USA

7. Planetary and Space Science Centre; University of New Brunswick; Fredericton New Brunswick Canada

8. Jet Propulsion Laboratory; California Institute of Technology; Pasadena California USA

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JE005290/fullpdf

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