我国云南江城氯氧镁铝石的研究
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On koenenite from Jiangcheng, Yunnan, China
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    Koenenite[4NaC1·4 (Mg, Ca)CI2·5Mg(OH)24AI(OH)3]from syrinite ore deposit, Jiangcheng, Yunnan is light yellow in color, and becomes dark brown due to weathering. It is foliate with cleavage {0001}perfect. The specific gravity is 1.82-2.08, after soaking iii water it reduces to 1.97.The hardness is 2.06-2.1. No=2.529, reddish brown. Ne=1.557, colorless. Ne-No=0.028.It shows weakly, biaxial 2V<10°. The X-ray powder pattern of the mineral has strongest lines; 5.45(90),3.25(50),2.812(100),2.380(70),2.130(60).Koenenite consists of two trigonal substructure layers; [Na4(Ca, Mg02Cl12]4-and[Mg7AL4 (OH)22 ] 4+.The CI-lattice unit cell has parameters; a=4.070A,c=32.646A,v=541.23A,space group Ram. The OH-lattice unit cell has parameters; a=3.051A,c=10.882A, v=101.132A3,space group P3m1. The structure of koenenite, as viewed along c axis is one of regmarly alter- hating NaCI-like chlorine and brucite-like OH double layers. All possible octahedral sites are randomly occupied by the metal ions. The strongest lines of the X-ray powder pattern for the material formed by soaking koenenite in water are; 7.73(90),3.835(100),2.570(70),2.285(80), 1,935(80)、1.526(80),1.495(70),1.316(50),1.269(60),1.200(50),0.975 (50).The unit cell parameters a= 3 .048A,c=23.190A,v=186.578A3,space group R. Chemical analysis of a water absorbed product after soaking koenenite in water gave: SiO2 0.63,Fe203 0.96,A1203 23.98,Ca0 0.18,Mg0 32.49,Ms0 0.17,H20 25.30, Cl 15.52,sum 99.23%,leading to the formula, [Mg7Al4(OH)22[Cl4.H20].

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刘金定,刘群, 1984. 我国云南江城氯氧镁铝石的研究[J]. 岩石矿物学杂志, 3(2):131~137.
, 1984. On koenenite from Jiangcheng, Yunnan, China[J]. Acta Petrologica et Mineralogica, 3(2): 131~137.

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