Mössbauerite; polytypes in Tatkul Lake (Russia) marls and evidence in a Murray River reservoir (Australia)
M¨ossbauer spectroscopy characterizes “Green rust related minerals†of the foug`erite group within the hydrotalcite supergroup (Mills et al. Mineral. Mag. 76(5), 1289–1336, 2012) in locations on Earth quite different from the original studies done in a temperate climate such as Brittany- Franc...
Published in: | Hyperfine Interactions |
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Main Authors: | , , , , , , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer Netherlands
2018
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/200157 https://doi.org/10.1007/s10751-018-1497-z |
Summary: | M¨ossbauer spectroscopy characterizes “Green rust related minerals†of the foug`erite group within the hydrotalcite supergroup (Mills et al. Mineral. Mag. 76(5), 1289–1336, 2012) in locations on Earth quite different from the original studies done in a temperate climate such as Brittany- France, Western Europe. Two examples are described, the gley at the bottom of Tatkul Lake in South Urals (Russia), which is representative of permafrost conditions, and a gley at the bottom of Yanga Lake, a reservoir in the Murray River catchment (NSW-Australia), which is representative of warm and desert conditions. Complementary information is obtained from XRD patterns. |
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