The validity of the structural model of antigorite based on the occurrence of four- and eight-membered tetrahedral rings is confirmed. The quality of crystals, single-crystal X-ray and synchrotron diffraction, lattice geometry, HRTEM interpretations, and coordination chemistry still provide evi¬dence in favor of these refined structures. The arguments used to invalidate this model and support an alternative one based on the occurrence of tetrahedral six-reversals only and octahedral sheet offsets do not hold.

Capitani, G., Mellini, M. (2008). Rationale for the existence of four- and eight-reversals in antigorite. AMERICAN MINERALOGIST, 93(5-6), 796-799 [10.2138/am.2008.2538].

Rationale for the existence of four- and eight-reversals in antigorite

CAPITANI, GIANCARLO;
2008

Abstract

The validity of the structural model of antigorite based on the occurrence of four- and eight-membered tetrahedral rings is confirmed. The quality of crystals, single-crystal X-ray and synchrotron diffraction, lattice geometry, HRTEM interpretations, and coordination chemistry still provide evi¬dence in favor of these refined structures. The arguments used to invalidate this model and support an alternative one based on the occurrence of tetrahedral six-reversals only and octahedral sheet offsets do not hold.
Articolo in rivista - Articolo scientifico
antigorite, crystal structure, serpentine
English
2008
93
5-6
796
799
none
Capitani, G., Mellini, M. (2008). Rationale for the existence of four- and eight-reversals in antigorite. AMERICAN MINERALOGIST, 93(5-6), 796-799 [10.2138/am.2008.2538].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/10281/12455
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