• journal_title：American Mineralogist
• Contributor：Richard M. Thompson ; Xiande Xie ; Shuangmeng Zhai ; Robert T. Downs ; Hexiong Yang
• Publisher：Mineralogical Society of America
• Date：2013-08-01
• Format：text/html
• Language：en
• Identifier：10.2138/am.2013.4435
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：98
• issue：8-9
• firstpage：1585
• section：Articles

Tuite, the high-pressure γ-form of the Ca₃(PO₄)₂ system, has been synthesized from chlorapatite at 15 GPa and 1300 °C using a multi-anvil apparatus. Its crystal structure was determined with single-crystal X-ray diffraction. It is isostructural with palmierite, with space group R3̄m and unit-cell parameters a = 5.2522(9) and c = 18.690(3) Å. The structure of tuite is characterized by three distinct polyhedra, PO₄, Ca1O₁₂, and Ca2O₁₀, that are translationally interconnected in the sequence of PO₄-Ca2O₁₀-Ca1O₁₂-Ca2O₁₀-PO₄ along the c axis.

Comparison of the CaSiO₃ and Ca₃(PO₄)₂ polymorphic systems shows a striking resemblance in the evolution of atomic packing arrangements as the polymorphic density increases. In both cases, the Ca atoms are progressively incorporated into the (Ca+O) close-packed monolayers, consistent with the hypothesis that close packing is a consequence of volume decrease as density increases. Based on this observation, we predict a possible high-pressure post-tuite phase.