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 = 420 C
Note: P = 101 kPa
_database_code_amcsd 0017845
4.9744 8.0432 5.8300 90 90 90 Pmcn
atom x y z Uiso
Ca .25 .4132 .7563 .020
C .25 .7615 -.0617 .039
O1 .25 .9194 -.0837 .039
O2 .4709 .6865 -.0968 .039
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