Glen Torridon Mineralogy and the Sedimentary History of the Clay Mineral Bearing Unit [PDF]
Clay minerals are common in ancient terrains on Mars and their presence at the surface alludes to aqueous processes in the Noachian to Early Hesperian (>3.5 Ga). Gale crater was selected as Curiositys landing site largely because of the identification of
Achilles, C. N. +26 more
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Clay minerals evidences for coldn-warm fluctuations in the Early Silurian. [PDF]
Zhang Z +5 more
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Soil mineralogy and potassium forms distribution and release in some calcareous soils of the Darab Region, Iran. [PDF]
Javan M +3 more
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Bioinspired Lignin-Aluminosilicate Composite for CO<sub>2</sub> Storage. [PDF]
Koo JW +11 more
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MSATT Workshop on Chemical Weathering on Mars [PDF]
The topics covered with respect to chemical weathering on Mars include the following: Mars soil, mineralogy, spectroscopic analysis, clays, silicates, oxidation, iron oxides, water, chemical reactions, geochemistry, minerals, Mars atmosphere, atmospheric
Banin, Amos, Burns, Roger
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Physico-chemical behaviour and microbiological suitability of residual smectitic soils mixed with two mineralized waters for therapeutic and dermocosmetic applications. [PDF]
Valente A +5 more
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Oxygen isotopic evidence that Gale crater, Mars, was home to an Early Hesperian water reservoir that underwent significant evaporation. [PDF]
Hofmann AE +16 more
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The spectroscopic, chemical, and photophysical properties of Martian soils and their analogs (MERC, phase 2) [PDF]
A series of variably proportioned iron/calcium smectite clays and iron loaded smectite clays containing iron up to the level found in the Martian soil were prepared from a typical montomorillonite clay using the Banin method.
Banin, Amos, Orenberg, James
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Controls of Geological Factors on H<sub>2</sub> Adsorption in the Subsurface. [PDF]
Li X, Walters CC, Zhang T, Sun X.
europepmc +1 more source
Origin and Evolution of Clay Mineral and Its Impact on Shale Oil Enrichment: Insight from Qingshankou Formation, Songliao Basin, NE China. [PDF]
Kang Y +6 more
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