2005
DOI: 10.1103/physrevb.71.052409
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Unconventional magnetic transitions in the mineral clinoatacamiteCu2Cl(OH)3

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Cited by 110 publications
(101 citation statements)
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“…20). In contrast, the off-stoichiometric so-called paratacamites of formula Zn x Cu 4 − x (OH) 6 Cl 2 assume partly frozen states at LT, with two magnetic transitions finally observed at 18.1 and 6.5 K for the end member (x = 0), clinoatacamite 4,[21][22][23] . The tendency to magnetic order in paratacamites may be induced by interplane couplings through Cu defect spins at the Zn site between the kagomé layers, as well as the likely presence of a sizable Dzyaloshinsky-Moriya term.…”
Section: Discussionmentioning
confidence: 99%
“…20). In contrast, the off-stoichiometric so-called paratacamites of formula Zn x Cu 4 − x (OH) 6 Cl 2 assume partly frozen states at LT, with two magnetic transitions finally observed at 18.1 and 6.5 K for the end member (x = 0), clinoatacamite 4,[21][22][23] . The tendency to magnetic order in paratacamites may be induced by interplane couplings through Cu defect spins at the Zn site between the kagomé layers, as well as the likely presence of a sizable Dzyaloshinsky-Moriya term.…”
Section: Discussionmentioning
confidence: 99%
“…13,17 In Fig. 1, we show the 16-site periodic cluster of the pyrochlore lattice that we will use in ED.…”
Section: Approximate Models For Clinoatacamitementioning
confidence: 99%
“…13 These sites are distinguished primarily through the Cu-O-Cu bond angle, with an average angle of about 96 • for bonds involving a Cu1 site and an average angle of about 118 • for bonds within the Cu2-Cu3 distorted kagomé plane. (While the distorted lattice structure leads to some further variation within these averages, the differences are small compared to the difference in average angles for the in-plane and between plane cases.)…”
Section: Approximate Models For Clinoatacamitementioning
confidence: 99%
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