Experimental constraints on the evaporation of partially oxidized acid-sulfate waters at the martian surface-Reference-Cited by-同舟云学术

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Experimental constraints on the evaporation of partially oxidized acid-sulfate waters at the martian surface

Published:2009-02 Issue:4 Volume:73 Page:1205-1222
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Tosca Nicholas J.,McLennan Scott M.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference71 articles.

1. Geochemical modeling of water–rock interactions in mining environments;Alpers,1999

2. Extreme acid mine drainage from a pyritic massive sulfide deposit: The Iron Mountain end-member;Alpers,2003

3. Thermodynamics in Geochemistry: The Equilibrium Model;Anderson,1993

4. The atomic structure and hydrogen bonding of deuterated melanterite, FeSO4.7D2O;Anderson;Can. Mineral.,2007

5. Meridiani Planum and the global hydrology of Mars;Andrews-Hanna;Nature,2007

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1. Photooxidation of Evaporative Ferrous-Ferric Sulfate Brines under a Martian CO₂ Atmosphere;ACS Earth and Space Chemistry;2023-12-19

2. Mineral Indicators of Geologically Recent Past Habitability on Mars;Life;2023-12-15

3. Raman spectroscopic documentation of Mars analog basalt alteration by brines;Icarus;2022-10

4. Mars as a time machine to Precambrian Earth;Journal of the Geological Society;2022-06-07

5. Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate;Communications Earth & Environment;2022-02-01

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