o/o NOTES AND NEWS per cent and the species name sal6eite to the half in which P)As in atomic per cent. A specimen near the phosphate end of the series has been analyzed (Thoreau and Vaes, 93, p.96; Mrose, 950, p. 58), but no specimens near the arsenate end of the series have been analyzed' A' semiquantitative spectrographic analysis of the New Mexico material (by C. S. Annell, of the U. S. Geological Survey) indicated AszOr in the greater-than-0-per cent bracket, but PzOs was not observed in any bracket down to a sensitivity limit of 0. per cent. The amount of material present in this specimen was not sufficient for a quantitative chemical analysis. The r-ray powder pattern of novacekite differs from the patterns of sal6eite and arsenian sal6eite only by its slightly larger unit-cell dimensions. The unit-cell dimensions of arsenian sal6eite ate ao:7.05, co:t9.87 A and of novacekite, ao:7.0 L, co:0. h. Optically this material is anomalously biaxial negative with a:'65, A:.6I, t:.6, and V 5 to 0'. This specimen is pleochroic with X colorless, Y pale yellow green, and Z pale yellow green. Its specific gravity is 3.7. The mineral fluoresces bright lemon yellow in both short and long wavelength ultraviolet radiation. This work was completed as part of a program undertaken by the u. s. Geological Survey on behalf of the Division of Raw Materials of the Atomic Energy Commission. Rnrnnnxcrs FnoNnnr-, Clrlnono (95), Studies of uranium minerals (IX): Sal6eite and novacekite: Am. Mi,neral.. 36. 680-686. Mnosn, M. E. (950), Studies of uranium minerals (III): Sal6eite from schneeberg, saxony: Am. Mineral'.,35' 55-530. Tnonreu, J.,.lNo Vans, J. F. (93), La sal6eite, nouveau min6ral uranifdre: soc. belge 96ol o gi,e B ul'.,, 96-00. ARROJADITE IS A FERROAN DICKINSONITE D. Jnnoiua Frsnnn, Department of Geology, (Jnittersi.ty of Chicago, Chicago 37, Illinoi,s. While working on classifying my r-ray powder films of the pegmatite phosphate minerals, it was recently noted that arrojadite from the Black Hills and dickinsonite from Branchville, conn., yielded substantially identical results. In her recent paper (3) Mrs. Lindberg compared the powder photos of arrojadite with those from a number of other pegmatite phosphates, but not with two films. dickinsonite. Figure shows prints from my
NOTES AND NEWS 677 Tasm. Cnnurcer, ANervsrs Dickinsonite Arrojadite KzO CaO NazO MnO FeO Fe:Os Mgo LirO SnOz AIzOr PzOs HrO F Insol..5.5 7.6 3.58 3.5 tr 07 J9.)/.65.58.80.O9 7.37 3 83 96 none 0. 0.89 r.63 0.8 3.73.0 7. 3.83 IZ. JJ l -o/ 0.0 0.78.8 A r.7+.6 6.0 5.78 8. none.0 0.09.66 0.00 0.9 0.80 0 \n.o0 r.5 5.53 5.69 7.6.67 5.5.33 5.05 9.8 none.39.50 85 0.8 tr.5 38.6 3.3 0 73 5.0 0.69.7 0.66 Total Less O: 99.93 00. 78 loo 0.3 99.89 O0. o3 99 87 99.66 -. Dickinsonite, Branchville, Conn. Wells, Am. Jottr.Sci.,39,3 (890)' 3. Dickinsonite, Poland, Me. Gonyer, Am. Mineral., 5' 38 (930).. Arrojadite, Black Hills. Lindberg, Am. MineroJ.,35' 69 (950). 5. Arrojadite, Black Hills. Headden (see Lindberg). 6. Arrojadite, Serra Branca. Guimardes (see Lindberg, p. 68). Table lists chemical analyses of the two minerals taken from the literature. Particular attention is called to nos. 3 &, since they represent the only available modern analyses of fresh material. These are very similar if it is noted that MnO*FeO:.08+0.08. Crystallographic data taken from Wolfe () and Mrs. Lindberg are as follows: T.trl,n Space Group bo Co Volume Meas. Grav. Dickinsonite C /c 6.7o Arrojadite C /m 6.60 9.95.69 0"+l' 3968 3.55 0.0 3.99 93037', 398 3. The only serious discrepancy is in the B-angle;the writer expects to do single crystal work to check these values.
678 NOTES AND NEWS Frc.. X-ray powder photos, Fe radiation (Mn filter),.6 mm. diam. camera, natural scale. Some of the lines are numbered as in Table 3.,-Arrojadite, Nickel Plate Mine, Black Hills, South Dakota. The crushed sample (prepared from a specimen in the Headden collection of Harvard university) was kindly supplied by M. L. Lindberg of the U. S. Geological Survey. D-Dickinsonite, Branchville, conn. The sample is from yale university (Brush coll. f3090) through the courtesy of Professor Horace winchell. rt consists of dark green platy crystals lining a small',rrg in lithiophilite (altered to sicklerite near the vug).
NOTES AND NEWS 679 T,tsre 3. Atnoyaorrn X-uv Dera (Snn Fro. ) Lindberg (3) I z.t.t 7.6.8 3 7.6 [t.9 7.s9 00 0rI J 7.r 6.5 6.8 6.5 0 5.93 5.93 5.96 5.90 00 03,3 5.5..5U 5.8 03,0I 300 5.0.99 5.0.96 00,0 7 la.58.3 3.8 3.58 (Skip one faint line) 8 9 J I 3. 3.33 3 3.0 3.33 0 6 3. J.IJ 7 3. 3.8 t 3 0 3.0.85 0 3.037 5.86 t 5 8.77.7 5.766 9.703.68.59 (skip faint lines) 6 ll 8 d.56.58. 5.553.505.rs * spacings measured by Leon Atlas;indices computed by A. A. Forslevusing thetechnique of Bloss () and the ctjll data of Lindberg (3). t 0 is an impossible reflection according to the gpace group criteria of Wolfe () for dickinsonite from Poland, Me.; so are 03 and 03. f These two indices are impossible reflections according to space group criteria,
680 NOTES AND NEWS The formulas given (using one of the alternatives listed by Mrs. Lindberg) are as follows: Dicki.nsoni,te System II 78 (from Wolfe) [HzNao(Mn, Fe, Ca, Mg)a(POu)" HrO] Arrojodi.te System II 680 Lindberg [Na(Fe", Mn")s(POr)r] [(Na, K);(Fe, Mn, Ca)6(POr),(F, OH).HrOl These will be discussed in a later report. The optical data () agree in showing a---->lbl, a very large V, and fordickinsonite Bn [d]: +5', while for arrojadite galcl: f ";indices of refraction are a bit higher in arrojadite, as is to be expected from its higher iron content. It is concluded that the name arrojad.ite should be dropped in favor of ferroan dickinsonite, since the latter term has a 7-year priority. l{ote: The indices and calculated spacings listed in Table 3 are erroneous, since they are based on an incorrect unit cell. wolfe has chosen the correct cell, but his numerical results are slightly small;b is05o5,. RrlrnnNcns. Bross, F. D. (95), Rapid determination of interplanar spacings for trimetric crystals: Am. Mineral., 37, 588-599.. Dora's Svsmu ol MrNnna.r.ocv, Vol. If, 9Sl. By C. palache, H. Berman, and C. Frondel. New York. 3. LrNournc, M. L. (950), Arrojadite, huehnerkobelite, and graftonit e: Arn. Mineral, 35, 59-76.. Worlr, C. W. (9), The unit cell of dickinsotite: Am. Mineral,.,6. g3hz. Mrreonrrrcs: Tnr Jounxar, ol rrn MrmoRrrrcAl Socrnry AND THE Iwsrrruru: ol Mareonnrcs of THE Umrwrsrrv or Nnw Mrxrco From the time of the inception of the Meteoritical society in 933, its /fares and contributions were published regularly in the monthly magazine, populor Astronomy, until December, 95, when that periodical was discontinued on the completion of its sgth volume. By arrangement with the university of New Mexico and by unanimous vote of the council of the Society, a new publication entitled Meteoritics: The Jootrno.l, oj the Meteorilicol soci.ety and. tlrc Institute of Meteoritirs oj the uniaersity oj New Mexico was established, and its premier issue, consisting of 5 items and 3 pages, appeared in December, 953, as Volume, Number, Whole Number, 953. Meteori'tics is to be issued at least once but not more than four times a year. rt is expected that eventually the journal will become a quarterly. Each volume is intended to contain from 0 to 3ffi pages. The Editor of the Meteoritical society, Dr. Frederick c. Leonard of the university of california, Los Angeles, is the Editor of Meteor'itics, and the Director of the rnstitute of Meteoritics of the universitv of New Mexico. Dr. Lincoln La Paz, is the Associate Editor.