Changes in the cell parameters of antigorite close to its dehydration reaction at subduction zone conditions

Tingting Shen
Tingting Shen
Cong Zhang
Cong Zhang
Jing Chen
Jing Chen
Jörg Hermann
Jörg Hermann
José Alberto Padrón-Navarta
José Alberto Padrón-Navarta
Li Chen
Li Chen
Jun Xu
Jun Xu

AMERICAN MINERALOGIST, pp. 569-582, 2020.

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Abstract:

The unit-cell parameter a of antigorite (usually expressed as the polysome m value) has been determined as a function of temperature (T) and pressure (P) in the range of 600-650 degrees C, 25-45 kbar in weeklong piston-cylinder experiments. A well-characterized natural antigorite (with m = 16 and less abundant m = 15) was used as a starti...More

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