Palygorskite from Padasjoki, southern Finland
K. Lindqvist, I. Laitakari
Bulletin of the Geological Society of Finland · 1981
doi:10.17741/bgsf/53.2.003 (opens in a new tab)
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Abstract
Monoclinic palygorskite with the unit cell a0 = 12.689 Å, b0 = 17.845 Å, c0 = 5.119 Å and ß = 91.22° has been found at Padasjoki, southern Finland. The mineral is thought to be of hydrothermal origin. Monoclinic symmetry is connected with an ordered Mg-Al substitution, although owing to the low Δd121‒121 value observed a low degree of ordering is suggested.
Abstract licence: CC BY-NC
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