Antao S M, Hassan I
The Canadian Mineralogist 48 (2010) 1225-1236
Temperature dependence of the structural parameters
in the transformation of aragonite to calcite,
as determined from in situ synchrotron powder X-ray-diffraction data
Locality: Cuenca, Spain
Note: T = 398 C
Note: P = 101 kPa
_database_code_amcsd 0017844
4.9731 8.0384 5.8236 90 90 90 Pmcn
atom x y z Uiso
Ca .25 .4132 .7561 .019
C .25 .7614 -.0619 .038
O1 .25 .9196 -.0838 .038
O2 .4713 .6866 -.0974 .038
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