The crystal structure of calcite III

被引:68
作者
Smyth, JR [1 ]
Ahrens, TJ [1 ]
机构
[1] CALTECH,DIV GEOL & PLANETARY SCI,SEISMOL LAB,PASADENA,CA 91125
关键词
D O I
10.1029/97GL01603
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The crystal structure of calcite III has been deduced from existing high pressure powder X-ray diffraction patterns, based on the assumption that it is a displacive modification of the calcite I structure. The structure is monoclinic with space group C2 and a Z of 6. There are two Ca and two C positions, and five O positions, and atom coordinates have been refined by distance-least-squares methods to give reasonable octahedral coordination for Ca and parallel, planar CO3 groups. Unit cell parameters refined from a published powder diffraction pattern at 4.1 Gpa are: a = 8.746(8)Angstrom; b = 4.685(5)Angstrom; c = 8.275(8)Angstrom; and beta = 94.4 degrees. The structure has a calculated density of 2.949 Mg/m(3) at 4.1 GPa which is less than that of aragonite at this pressure and consistent with early piston cylinder studies. This implies that calcite III is indeed a metastable intermediary between calcite I and aragonite.
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页码:1595 / 1598
页数:4
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