Elevated olivine weathering rates and sulfate formation at cryogenic temperatures on Mars
Sulphate-rich sediments have been taken as evidence of surface water on Mars. Here, the authors show that cryo-concentrated brines chemically weather olivine minerals forming sulfate minerals at up to −60 °C, showing that cryogenic weathering and sulfate formation can occur under current Martian con...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2017-10-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-017-01227-7 |