Effects of Environmental Fe Concentrations on Formation and Evolution of Allophane in Al‐Si‐Fe Systems: Implications for Both Earth and Mars

Author:

Du Peixin1ORCID,Yuan Peng12ORCID,Liu Jiacheng3,Yang Yixuan12,Bu Hongling4,Wang Shun12ORCID,Zhou Junming12,Song Hongzhe12,Liu Dong12,Michalski Joseph R.3ORCID,Liu Chengshuai4ORCID

Affiliation:

1. CAS Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

2. University of Chinese Academy of Sciences Beijing China

3. Department of Earth Sciences The University of Hong Kong Hong Kong China

4. Guangdong Key Laboratory of Integrated Agro‐environmental Pollution Control and Management Guangdong Institute of Eco‐environmental Science & Technology Guangdong Academy of Sciences Guangzhou China

Publisher

American Geophysical Union (AGU)

Subject

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

Reference86 articles.

1. The paleolacustrine evolution of Juventae Chasma and Maja Valles and its implications for the formation of interior layered deposits on Mars

2. XAFS Study of Fe-substituted Allophane and Imogolite

3. New analysis of the Mössbauer spectra of akaganeite

4. Beaty D. Abbud‐Madrid A. Boucher D. Bussey B. Davis R. Gertsch L. et al. (2016).Description of water resources on Mars that have the potential to become reserves as part of a human exploration zone: The m‐wip study part 1. InPaper presented at the Space Resources Roundtable Golden CO.

5. Akaganéite (β-FeOOH) precipitation in inland acid sulfate soils of south-western New South Wales (NSW), Australia

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