Jonesite
	Krivovichev S V, Armbruster T
	American Mineralogist 89 (2004) 314-318
	The crystal structure of jonesite, Ba2(K,Na)[Ti2(Si5Al)O18(H2O)](H2O)n:
	A first example of titanosilicate with porous double layers
	Locality: Benitoite mine, New Idria District, San Benito Co., California, USA
	_database_code_amcsd 0003405
	10.618 25.918 8.6945 90 127.633 90 P2_1/m
	atom x y z occ Uiso
	Ba1 .49799 .517595 .24430 .01207
	Ba2 .00154 .47576 -.24868 .01449
	K1 .2822 .2500 -.2510 .70 .049
	Na1 .2822 .2500 -.2510 .30 .049
	K2 .7146 .2500 .7472 .50 .027
	Na2 .7146 .2500 .7472 .10 .027
	K3 .7884 .2500 .7294 .40 .147
	Ti1 .2682 .57478 -.2123 .0121
	Ti2 .2604 .43091 .2752 .0128
	Si1 .8767 .60395 .4844 .0107
	Si2 .3469 .38986 -.0279 .0146
	Si3 -.1248 .38956 -.0289 .0085
	Si4 .6392 .39499 .5151 .0110
	Si5 .3978 .31321 .2522 .395 .0127
	Al5 .3978 .31321 .2522 .395 .0127
	Si6 .1075 .31288 .2618 .395 .0082
	Al6 .1075 .31288 .2618 .395 .0082
	Si5A .6085 .3115 .2516 .105 .010
	Al5A .6085 .3115 .2516 .105 .010
	Si6A -.1106 .3130 .2263 .105 .010
	Al6A -.1106 .3130 .2263 .105 .010
	O1 .0389 .5708 .5886 .0190
	O2 .7016 .4275 .4129 .0170
	O3 .1938 .3924 -.2584 .0185
	O4 .7971 .3896 .7423 .021
	O5 .2928 .4247 .0767 .0140
	O6 .2639 .3382 .2754 .75 .0204
	Wat6 .2639 .3382 .2754 .25 .0204
	Wat7 .7684 .3346 .2853 .79 .028
	O7A .7375 .3350 .2119 .21 .010
	O8 .5782 .3377 .4279 .79 .0060
	O8A .6326 .3306 .4396 .21 .010
	O9 .9123 .6623 .5668 .0260
	O10 .0265 .4274 .0767 .0163
	O11 .2874 .5099 -.1701 .0212
	O12 .5023 .4084 .0088 .0210
	O13 -.2466 .4081 .0079 .033
	O14 .3521 .3286 .0357 .79 .018
	O14A .4339 .3349 .0531 .21 .010
	O15 -.0603 .3296 .0429 .79 .011
	O15A -.0970 .3352 .0616 .21 .010
	O16 .4929 .4239 .4839 .0201
	O17 .7585 .5739 .5114 .023
	O18 .2568 .4970 .2743 .0278
	O19 .4074 .2500 .2796 .79 .013
	O19A .5727 .2500 .1993 .21 .010
	O20 .1147 .2500 .2868 .79 .023
	O20A -.0981 .2500 .2655 .21 .010
	Wat21 .4920 .3247 -.2570 .72 .043
	Wat22 .5011 .2500 -.2472 .26 .040
	Wat23 .6266 .2500 .0420 .40 .040
	Wat24 .9570 .2820 .7019 .28 .040
	Wat25 .7256 .2500 -.0068 .36 .066
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