SCIENTIFIC ABSTRACT GRIGORYEV, B.S. - GRIGORYEV, D.F.

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SCIENTIFIC ABSTRACT
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GRIGOR'YEN) B.S. Ostriakcrvls letter to Lenin. Vest. oviazi 25 no.4:30-32 Ap 165. (14IRA 18:6) GRIGORITIV B,S.* GRIUSKIN, T.N.; MININ, A.K. "Aal. 0 I Use of a conveyer for laying out yarn* Teksteprom. 16 no.12:43- 44 DI56* (J4LRA 10: 1) (Yarn) (Conveying machinery) GRIGORIYEV, B.V., kand.tekhn.nauk Mechanizing the assembly of threaded joints. Aveprome 26 no.8:16-21 Ag 157. (*chins-shop practice) (MIRA 15:4) GRIGORIMO B,V,, kand.takha.muk Screwing-in of threaded Pins- Av.prom. 26 no.8.-84-85 Ag 157- (14M 15:4) (Screwdrivers) GRIGORIYEV, B.V.; KIPEAMAN, S.Ya.; IVANOV, G.F.; RYABIUOK, A.G., red.; TELYASHOV, R.Kb., red.lzd-va; GVIRTS, V.L., tekhn.red. (Now method of anode mechanical working of metals with a band] Novyi spoeab obrabotki metallow metodom anodnogo to- chenlia lentoi. Leningrad, 1963. 15 P. (Loningradakii dom nauchno-takhnicheakoi propagandy. Obmen perodovym opytom. Seriia: Elektrotekhnologicheskla protsoosy I ustroistva, ro.8) (MIRA 17:4) 'a. _z:- '!-'T;~1' GRIGOR'YF,V, D-V-; KIPFRMAN, S.Ya.; IVANOV, G.F. Anode belt machining. Mashinostroitell no.3:30-32 Mr '64. (MIRA 17:4) C--r Oa lhe volva of 1110 intofn4f wooldid4f isillng of hianks fawr mmamh6fanos ( n R-josikn), Trudi' -d-V-14-fs. lckhnm inta no. 22, 111-116, 1954; Rev. no. 163~j Rol. Z6. -Mekt. 1956. An attempt is made to determine theoretically the residiud tFe sea in a strip dwing rolling, in relation to g6t valt*,,4 Ave r3oll ~exsute. On the basis of a series el assump'tiong,We Ae- focMation of the fibers in the foiling direction is ar,-401iwrely degetmined by Ifooke's 14w, V. A. Lomakin, USSR /-7-7 cowsoly q/ Relrralivnyi zkuryall Tranvlatior4 cowlesy Ministry ol Sapply. England T I~T, CRIGORIYZV B. V. (Cand. Tech. Sci.) "Some Problems of Diapbragn Corrugation." in book Some Problems in the Modem Technology of Instrumentmaking, Moscow. Oborongiz, 1957. 126 p. Moscow. Aviationnyy tekhnologicheskly institut. In this article the author discussed problems connected with pressure and forces developed during the process of forming corrugated diaphragms. No references are given. - , z , - . ,1. ,~ i. . . GRIGOROYIV, B.T., Imnd.takhn.nauk ~ft low-wopmWe. I I I About A.N.Gavrilov's article. Priborostroenie no.10:17-19 0 '57. (N In 10: 11) 1. Glawnyy Inshener Smuchno-inaledovateliskogo Institute tekhnologit I organisateit ppolsvodstva avintsionnoy promyshlennosti. Onstru"A Industry) (Autosatic control) GRIGORIYEV, B.V., kAndidat tekbnlchaskikh nauk. Problems in corrugRting membranen. Trudy KATI no.31,:84-96 '57. (MIRA 10:10) (Sheet-metal work) V111."Mcclauiization arid Automatlon of Production in F(,u:idrJcL;. 1. Mechanizatlon and automation of' processes for obtaining blanks an(I parts from liquid metal. 'a'. Cast- Ing in forms. 3. Casting In shell molds. It. lnvestment cactine'. 5. Casting In ceramic and -Iry-sand molds. 6. Centrifugal casting. 7. Compression molding. 8. Knocking down molds; cores; and cutting off and finiching castings." kutbriation and Mechanization of Production Processes in Instrument Manufacturi-ng, Moscow) Mashg1z) 195b. 591 P. PURPOSE: This book Is intended for engineers, technicians, and scientific per- sonnel concerned with mechanization and automation of production processes in Instrument manufacturing, and for students arid teachers of this subject in vuzes. (1RI(;CRty-'.7r T; A( IV. LIMVITEV) A. A. (Cand. Ucl.); FEldK"Cil') SHIPEYMil Yu. G. (Cand. Tech. ScL.); XIV. "Extunpleu of MeelvLnization arid Automation of 1nvtmui:crit-part,,. Manufneturing Processes," Automation wid Mechanization of Production Processes In Instrument Manufacturing, Moscow, Mashgiz, 1953. 591 P. PURPOSE: This book is Lntended for engineers, technicians, and scientific per- sonnel concerned with mechanization and automation of production processes in instrument manufacturing, and for students aria teachers of this subject in vuzes. ;1. ~;. ~i'~I:'A. Tu"". . ~ 7 1 k XVI. "Means for the MCCh[LlJiZUtIOn Of Assembling Operation,,," Auto-vition and Mechfinlza- tion of Production Processes in Instrument Manufacturing, Moscow, Masligiz, 1958. 591 P. PURPOSE: This book Is Intended for engineers, techniciluis, turd scientific per- i;oruicl concerned with mechanization and automation of production procesces in instrument manufacturing arid for students and teachers of this subject in vuzec. CHMYSIM. Aleksondr Vasillyevich; YAKHIN, Abran Borisovich [deceased]; 0 ,qgl-(iQH!.111,-B,V,,-Icand.tekhn.nauk, roteenzent; AUDRMV, V.A., kand.tokhn.nauk, red.: YELISETEV, H.S.. red.izd-va: CHMOTA. Z.1., tekhn.red. (Introduction of automatic programmed control of operations on motal-cutting machines] Avtometizateiia obrabotki na metallorezhu- shchikh stankakh a primeneniem programmnogo upravleniia. Koskva, Goo.nauchno-takhn.izd-vo mashinostroit.lit-ry, 1959. 194 p. (MIRA 12:11) (Metal cutting) (Machine tools--Nuncrical control) (Automatic control) BULOVSKIT, Favel Ivnnovich: GRIGORIYEV, B.V., knnd.tekhn.nauk, rateenzent; CHANTS , . ., inth., red.; BOGOMOLOVA, M.P., izdat.red.; ROZHIN, V.P., tekhn.red. [Designing the technological process of assembling instrumentaj Oanovy poutroaniis takhnologichookogo proteases sborki, priborov. Moskva, Gos.1zd-vo obor.promyshl. 1959. 245 p. (MIRA 12j10) (Instrument industry--Management) Main objective to th* development of atitomation. Izobr.1 rate. no.7:1-2 JI 159- (14IRA 12:11) 1. GlavrWy Inshener Nauchm-leeledovatellsicogn inntituta avistalonnoy tokhnologile (Automation) S/536/59/000/040/002/005 to62/9435 AUTHOR; Candidate of Technical Sciences TITLE: The accuracy of manufacture of manometric elastic deformation elements PBRIODICALz Moscow. Avistsionnyy tekhnologicheskiy institut. Trudy. No.40. 1959. Yoprosy tekhnologii priborostroyeniya, PP-55-70 TEXT: The accuracy of manufacture of manometric elastic deformation elements involves accuracy of dimensions and geometric form and also the maintenance of the required elastic and allied properties of the materials of construction. Formulae are quoted giving the relation between applied pressure and the deformation of the element for different manometric membranes and tubes. The formulae show that the deformation is a function of applied pressure. The form of the relation between pressure and deformation depends upon the geometric shape and dimensions of the element and the properties of the material. The deviation of these dimensions and properties from their nominal values affect the relationship between pressure and deformation and, therefore, the maintenance manufacturing Card 1/2 S/33f)-/59/000/040/002/005 The accuracy of manufacture ... zo62/9435 tolerances on these quantitiesare essential in the production of anometric elements. Formula@ are quoted for various elements iving the effect of variation of dimensional and elastic : parameters on the deformation of an element for a particular nominal deformation. The formulae are derived by the methods of approximation or partial differentiation. They are claimed to be new. In addition to the above sources of error, other parameters must be considerod. In an elastic deformation element it in desirable that the characteristic should be smooth, that the element should have minimum remanent deformation and hysteresis and maximum static and dynamic strength. An essential role in ensuring the accuracy of elements is played by the preparation of the material used in construction. Selection of suitable methods ensures uniformity and stability of characteristics. Method* of assembly or elements affect their accuracy but this problem is not considered in the paper. Professor Y.I.Peodoslyev is mentioned for his contribution in this field. There are 4 figures, 4 tables and 1 Soviet reference. Card 2/2 Accwsion xR, A?4o22349 S/OU7/6h/ODO/003/0030/0032 AUTH015s, Grigorlyev, B. Vej Kiparm", S. Ya.; Ivanov') Go Fe TITLM Anode grindine with a belt SOURCEs Hashinostroitelit no. 3, 1964, 30-32 TOPIC TAGSt metal cutting, anode grindingo electromechanical machiningp electric are machining, titaniump stainless steel ABSTRAM Belt anode [;rinding of conductive materials was investigatod using the apparatus shown in Fig. 1 on the 9=103ure. The part (2) turns between centers and is connected to the positive terminal of a Me supply. A continuous steel belt (1) is connected to the negative terminal. An electrolyte consistirk; of a colloidal solution of liquid glass (Wa20 * n5i02 + rril.0) is continuously introduced between the belt and the part,, forming a film which is removed by the belt. ~--cs formed in this region melt out the material. The test apparatus permitted work on sapplos B-50 ma in diamtor and 30-400 mm long, The voltage was 24-30 V. and the current ranged between 120 and 100 amps for titanium and was 300 amps for stainless steel. The method was found practical for preliminary machining (7-9 class finish) Card 113 ACCESSION NRt AP4022349 of very Ivird metals. The possible time saving was demonstrated by turning a 25 x 25 x 60 mm heat-resistant steel sample to a 15-mm dianoter cylindar in a lathe. Thds process required 15 minutes. The sam. result was attained by anode rrinding in only 40 seconds. Origo art., host 7 figuros. ASSOCIATION: none SUBI-EITTEDs 00 SUB CODE t M Card 2/3 DATE ACQt OBApr6l, NO REF SM 000 EINCL 1 01 OT riMs 000 ACCESSION NR. AP11022349 it Fig. 1. Scherutic of apparatus ENCU)SVRE; 01 I- belt,, 2- part, 3- brushes, 4- head spindle, tail stock, 6- rheostat., 7- Conerator, 8- vindine. Card 313 AUTHUR: SOV/130-58-12-18/21 TITLE: Automatic Dogs for Gripping Metal (Avtomatichoskiye kle3hchi dlya zakhvata metalla) PERIODICAL: Metallurg, 1958, Nr 12, pp 38-40 (USSR) ABSTRACT: The author describes a new design of dogs (Fig 1, with which two of the three soaking-pit cranes of the heavy- section mill of the im. A.K. Serova (im. A.K. Serov) metallurgical combine have been fitted. The soaking- pit lids have been modified (Fig 2) to enable them to be lifted by the new dogs. The introduction of this equip- ment has facilitated and accelerated metal handling at the soaking pits, freeing 16 men for other work. A further improvement, the mechanization of rotation of the dogs, has been incorporated in a set recently built and tested (Fig 3). This was found to have some removable Card 112 , Automatic Dogs for Gripping Metal SOV/130-56-12-lb/21 defects and improved handling efficiencies still further. There are 3 figures. ASSOCIATIONs Metallurgical Combine imeni A.K. Serov (Met&UUrgicheskiy kombImt im. A. K. Bero. ) Card 2/2 ~# 's I .. . I I 'A!~'i j, : (.!r--,n9ter . - e-trlc trmvellin,7 crAnos t~, roilin.- co~:irct '-epriW. - 'I, . - i4 ~` - .,, , 7. . '. .,7 ',141-~j42 ~' # 56 . I 1r:,,) ! - iv, i !-Xiii %provs. I 3parings OiAchirtry)! t~'rqneo, - . etc . ) GRIGORITIV, B.Tso; LITESHEV, A.I.;IVAIINIKOV, X.Ta., apizootolog. - , MO.-Sm. -,". Ilimination of tuberculosis in cattle in Kursk Provinca collective farms. Veterinarils 34no.11:81-83 N '57. (MIRA 10:12) l.Voteriwwnyy otdel kurskogo oblastnogo upravlentya sel'skogo khosyaysiva. 2.Nachallnik veterinarnogo otdela (for Grigorlyev). 3.Zaveduyushchiy spizooticheskim otdolom oblastnoy vetbaklaboratoril (for Uteshew). (Kursk Province--Tuberculosim In animals) QLIGMIYBV, D.A., kaod1dat takhalchesklkh mauk; TROIMIY, Te.A., kandidat Ve-MIErneekikh sauk, laureat Stallaskey preall. Precast this wall prostreseed bridge span structure@ with Oreoe*& olmps. Bet.1 shol.-bot. se.33106-109 Jo 155. (KLMA 9: 1) (Bridge construction) (Comrsto. Prestressed) BLIMOV, I.Ye., tokhnik; GRIOMIYIV, D*A*, kandidat tekhnicheskikh nwik. -- wwww- Centralized manufacture of retaforcement bundles for bridge spans made of prestrested reinforced concrete. Bet.1 zhel.-bet. no,3: 100-103 Mr 156. (KM 9:7) (Bridge@. Concrete) (Prestressed concrete) BLINIOV, N.Yo., tokkalkA GRIGORIYIV, D.A., k&ndi&nt tokhaicheakikh aaak. Device for n&klag reinforcement bundles. Trasep.strei. 6 no.12ill- 13 D 956, WaA 10:3) (Prestressed concrete) (Aridge~. Cancr*to) --7, -4q~ . ..... A ~4; SOV/124-57 7-8-102 Translation froin: Referativnyy zhurnal. Mckhanika, 1957, Nr 7, p 1-1 ' (USSR) AUTHOR- Grigor'yev, D. A TITLE- Investigation of the Performance of Th in -wa lied Reinforced -concrete Girders Containing Prestressed Longitudinal Reinforcements and Stirrups (IssIcdovaniye raboty tonkostcunykii zliclezobetonrivkh balok s predvaritellno napryazhennymi prodot'noy armaturoy i khounutamil PERIODICAL: Tr. Vses. n.-i. in-ta transp. str-va 1956, Nr 11), Pp 110 170 ABSTRACT- The author demonstrates the expediency of using thin~walled reinforced- concrete girders for the span s!ructures ct railroad hridges He cat culates both the lateral force required -o cause !he failure of such a girder and the lateral force that WOUld result in the formations of cracks, and then compares the two sels ci forces The possibility is investigated of applyin to prestressed girdt-rs the formulae proposed by M. S. Burishanskiy IMaterialy konteretifsti TsNIPS fTrans Note, should read "TsN11PSA (Papers Presented at the Conference of the Central Scientific Research Institute of Industrial Structuresl, Moscow, Gos izd-vo lit. po stru -vu i a rkhitekture, 195 11 for calculating the Card 112 lateral strength of beams made of ordinary reinforced concreic To SOV/124 57-7,8402 Investiliation of Oie Performance of Thin- walled Reinforced- concrete Girders (cort evaluate the stiffness of the girders, the author uses the calculation procedures evolved by V~ 1. Nturashev fTreshchinoustoychivost' , zhestkost i prochnost zhele z0betora (The Strength, Stiffness, and Resistance to Cracking of Reinforced Con- crctc)- Moscow, IvIashstroyizdat, 19501 and by Ya M. Nemir,,-,-skiv fhlatcrialv konferentsii TsNIPS (Papers Presented at the Conference of the Central Scientific Research Institute of Industrial Structures), Moscow, Gos, iz(i-%,o )it po st r- vu i arkhitckturc, IQ511. For the purpose of evaluating the arnount of allowable shear stress in reinforced- concrete members subjected to lateral compression, sbear 4ests were run on 22 specimens According to the atithor these specimens were so shaped that there were no normal stresses whatever presen, in the shear plane; the iailure pa-ern, however, hardly -bears this out. The author concludes that thin- walled reinforced- concrete girders with prestressed longitudinal reinforcements and stirrups are highly cracking-- resistant, %-cry rigid, and %cry strong. His Cal culations, performed with the Borishanskiy forii-iulac, yielded satisfactory results, V A. Gastev Card 212 C, l< BERG, O.Ta., )mnd.tekhn.nauk-, GRIGN lYZV, D.A., kand.tekhn.nauk Use of reinforced concrete In bridge construction. Trudy TSNIIS TrWy TSNIIS no.27:7-77 158. (MIRA 11:7) (Bridges, Concrete) I i ir 1: 1 FIT Tr FTITTTTAiL AN 000 400 $00 00 UP.--u trIp"Kili too 00 v 6-0-8-v-w 60-6 v 6 -U-"- TT" 6 4 0 6 v 4 a -9 a - w- V-0--m- 09 1 A I I r I , It 11 6 0 ), At A " A A 1 V" 0 1 r 6 a 1 0e A - -J- 0 U.g I o 40 00 of Tho egia, *I &Nwists, chisciste and timmadem-Ovido cOm- far If petedsW6001111cWtalwAt"61 --wommicas. It. I'. (Ilistvi*m Mine. W. to#,# mililiful. so. 3V-431IR XVI-41)(110M.-A review td the literature anti of a Ihejww-lKV4jvfftAimvtAA1I1c h h l f o, t. rum w olimadw-ce (alkirtallerre) in The Ortificiel "W 10611cawillow peas .0 r l 14ewni. One in the label gig them evierti into the "INA IMA. 0 It A 1. CI aw WO. in nurit. nwrely .4 S" "Wntiml opevilm-0 0: j! twidwr - formalwal III nowa.. R. 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TbccIm-.jpfof%t1m%t4tnu%- Vitt we not ermitly Afferieff by the prewswe.4 MAirk In dtoinns of Nwitt. F, %%wh 0 IF 11 ._A So 1400 G!LALLURGKAL L1111841101111 CLASUPIC411" &S11 1!1Qmj .10 ativ at jt I-T-1- mot Sarwo It 1119101941114 109 go 0 Is a mw it .0 - - - - - M 0 0 0 0 0 0 0 0 Ole 0 0 o 0 a a o a 0 0 to 0 0 a o I-00 .00 Coo go see "go aof fee ttee Woo ! 0000009000000: 1 0 w0, "0"' bow l a A I fil kk C M W O i r I 00 it 00 a N F wart ft O d, L; pig **W to tkpw I" ummolfte and 4iftmi sate. r hl W* t lum bi a thm 1b o = 00 o omma t y, 4 1 C enordAm so abosul Iand will 0 L = 4 . Ow Wide IWVWM 60 8 - 4 Wt.. it INS. S#kM* 11T Sr. 1 that aU Ow Alitle w" d b I ;w e l a od y lwI ~ tkomad Ibm wMaways= 'e hit am. 1" 1 10 tao %& go d. . . thre"k4dambertbon (taws. ar4w writh im As doe Joe a** 00 zoo bANO tiso saaaw go 0.0 Clad 41161, soc 4-.' '4' - - ow 01* 0 J ; ; 1 ; 0 a I v a 1 9 p 9 a i No An a I a ad 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 i O 0014 0 o 0 0l o 0 a 1 0 0 0 0 0 0 0 : ti 0 0 0 1 0 0 0 v 9 0 0 0 0 0 0 0 * ! ! A hit PIl us U. go. ft vmA A,11 L a I I ? 4 1 1 Y 11~. A t X-I-k J. a a ' co"Wasip"hk imt%!rm of WO&W MAW 11 -00 oved. ,;e I -00 f I inten l A d I h l 1l l h f r of it I' ffi e awl .%l o mu ite iN Givil " .1 vy t wits (I JJ. 117,11111") *a* sul,*Irfl I.* so'nk"Ileffor and .00 00 IF rfyotel Gotimlysis. 0, - I W. 0. - 1,644'. the .,46411 00 devialk."s fTewn the frioults 01 lkmi is &t"1 (Urig trf. (" J 14, 2W7) we prulislily due to the ittrwrier.4 imptivit.- -00 00 1 A opmokwOric study pyr the following valit" I.* the an~ 0*1 (1)(110) (liM - WAV, (21t.llfil till), - ' 1' 7' 1- f 1 01 1 I 1 M M .00 mit- ,% 1 . 1 A 4 ill , its civitilmiril with 1 00 00 J ll.mvis atid Carty 3 tritetwes 00 00 as -Go 09S 00 KIM 00 : of 00 00 100 go --06 00 to 41111 F it it a Of a a a 4 0 0 0 0 0 0 0 0 0 0 Of 00 00 9 so 00'a 00 10, n,- *Iwdp- ill dw d do IMWM bar JOKW#~ a I A, ellwyesicit urgintwe cwwocoew ;4409 .10 6.T 406 4666#14-1 -m-a7i~b u AV 1o0 J'Al- 0 0 0 0 go 0 Ir"of - +"a, A'41 0 0 0 0 0t a 600 609941041 else go 0 0 0 -10 pw--* 0 a a ~9* 40 0 0 -00 -0 * .00 Ago* no* see goo* too see Ii, i, I- i 0 0 0 0 0 0 0 0 0 0 0 21 0 0 0 0 0 0 0 0 6 0 0 0 0 0 0 0 a) -01L 01 1., lk 11 a 1 8 0 Is 1. 0 14 Is tj 0 a a ft a 1 8 " 1~ 11 st a a .1 at P a a 4 12 to a As W 6 1. 1 0 U a a r 4 a 1 8 a 1"'0e i f v # 0 Ito &&Plot at #I.## A A in we Moms Of (he synthetic P(Tpatats.. ' - R /A ePrat. v Mvii As . '41, as. No. 2. t lose. %I%. UtInt. ev.1111. A'v tt%.I% 411-1 94:9111114 Me 010COHY CV%l%LA1Id- 1114' In"IWC '4 00 water in the twnpgj. IA Amphilsilis Wea, jtCu U11.1cu-11- 4 mated anti *he nfA espersord in the rhint. Itlitioul" - 00 e this grisup. On the busis til Ow ripil. s-ray a new ptnelf (lots. claq,116=4 ami 44 view Is" Orimutawd on tht-OwI14 "Nsmituts(K1.4 t t t k l1 h m ta tipAs ow i amplialiales and the role W wagrr w 00 ,he lattice structure of asupfulmoics and call fit. *u6mituN I.y the crystalkwherst. analugs (1-* ajI,j Cli. %If c%pts. f..f iti, sjrutlartic glat,pri. of smphilmlt~* can 1w di"It-d iut,i3 --00 ;nsdin Stimps: (I) the synths-sis from lh~ "dtv*' nicIts iu hc slwncv ul stairs, Food C1 jur still un.4ve.1 l".-Ause All a elpt). r"1111# are either "hiful IN dch"itcly unuti-fAc. 00 0 ("ry. 12# the hydiatim-intal eynthirsis and IN prepa. -4 o" sc4&,)- s ~ ds nwo of F cqntt tb l t l f . wi ervi e% ar a runs ainip p INAI anti pylustnes) PrWISK-ed a IUD. (d illit-W(vint I.- results. (a) tipts. 400 the fissions 14 Alliplubult ttringlasul nt. *9 with othrr welistaw" (turpt walvi. F and 4:1 and 111, 6 light vaktik substatum roxis as 1101)0) pritilutird (14mistful W. R. lienn 4 10, 1 L a afI&L1,6*44CAL UTROPOWN CLOSIMPICONO a I- . Ise. ' I t - o am. Oak . 1 s S I I K so . 4 a. , S ONJ s i Is : : am Its well iceman IBM 1 0 0 0 0 0 0 6 0 0 0 0 0 0 0 0 0 0 0 0 0 0 a 0 0 0 o 0 0 e 0 0 0 0 0010 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 *1* 00 0 of 0 0 0 0 * 0 0 @**Sol 004 so A 00 -4i 00 00 1** 00 00 00,11 00 SO a ~~ &I v 11 " a . 91 0 0 of of A A -4, Ile* fiverimor in Inlawakilical and pol"Okocal 08porriments. itepwially in me amphiboles. rv witorPul. 121. ". :it" Refoodt /hot low, No. 5. V. if I I l V11414ININ. air U-4 fix %potww1ug ee -00 ".11 Not. ttw -Y"Ils~l 00 Ar,~ hot IIw* "nows vsjx~l agernal 414 is. willd. lof lfw t,V1111WO. (of MuNrIalis " n'" Poo =00 is it" . 1-:11, ti an inok-jortubritt cumtounrut w oil IN f-vim l I f - all "Stif moul replemsommit. in "Nut ra.~ III%, I- to 0 Illillpf1wil 14 Frialni to low irpiww"Irlit If #I fill, I.." It. - 99 pl. silly io P - 0 4w v #1 Cl a% owtil as in P - Oil 41 istid P 111I.-Cf. The pit -mow. til Fin natural amphiloil- aml mic.8% stolofmortt, Ile nor tow ftw sy"ItSifir pfrip's. 44 11- goo milivra1% to, -Adloorliefts, for 11W tvallpleir trplarr"I"It -4 fllf~ 4Wh F anekqp of ()JJ~Mjg "jljkj&I% art Ilk.1f see . 411-*-1 noosticl %tructure. Ill the iynthcw~ 4 int-val, F .&if 6- umv) x% 11) a lutodanwitial port oml ill,- mirm-fal. Zoo its WI~ ry%t. lmstlk~ P jflay~ an 2"414,1wiltio,"I pArt. oil' (or frVia-ifts the Oil cloilp ill milicta6 goo 131 a- it ;IN-*I (of the tiff group in (he ri-1114111. food now"k anti (I at a milwaligins rrjrvjf~ &jiml lee for of) J "thef MMK*t 'W"11- W. R 11"m 1 -09 goo A IS. ILA MAIALLW061CAI too 00 mw a .1 re I IS or Ill w It a n is as SAO A I tot Ole 0 0 0 0 0 6 a 0 0 9 0 0 0 0 0 0 0 6.0 0 0 0 0 0 a 0 0 0 0 0 0 fill 0 0 0 0 00 0 a 0 0 0 a 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 * 0 0 0 We 00 0 - see go** off* 00 -00 so -00 00 -00 .NOW Id~IkO In Wathatic miss, 1) 1'. Calvwrt 00 7 lee / , 7o,,jjr I%o, 11. 1. 4 NIM. A- an shl in imviltenwind the 11for 14,1.. fl, 09 -0* 1011- t14 lite tile -4 -11%1VW141.8Af,W1,- -0~ 1, A - '00 .4 %Vi %.. 60 t-T 'Mt I be .4 .00 Olowth of litah trillp 11- MotAl"l. I t-i. %ith P in,frad 14 the Oil gemir s. trfr-t-I to 00 V c lee . wpf.'W~ .00 00 '00 00 ZOO 00 see 0* zoo .00 .11ALk"(.KAk LIT106TIOt (tatifIcAlK. 00 it to "1 1, 0 0 0 0 0 Goo* 00 0 a 00000 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 41 0 0 0 0 0 0 0 1-my iv?~slkpOm 44 @y ampUbW* pre M11111111 ~ DIPIP911114111P. C.11104,11'11V AND. N. 11*61" R" Ivy Iss.4"a py"'s ITIL, n.111%meml &.happramiltonto"hvidws The two vir"Saw pha=,a: mphihnif of the lrvnK*ilr lytw sorl Otk"e (tow" Tbr oyntlectic amphilx* ha. fl: t"Wil~ml 14F.Ca, *r -4y"thrlie. 6- Ahm 21 WIN$ dibul. VO .:Zkj -,~A, a m Ara" 1b d adown d Imew om an == Om m d i= soma D. 11. ( C4PKWV m` A. V. Kolw6bi lCo", smW~ Mat Sev lf.R,S~S. 1041, IL $,I mi. W. R. A. V rRomb d 111111111111IL"Womft loss rv asid 0. W, A 9 mixtufe of h-bko& mW Hs ,"At OL 767-720). ti I a of ow ph . 0 tit 11, The wwIj contal-d rnks of tW 010611.1. ,it. (U) unisn"I Int-11-1- " m... ib. ISO.'a It 1tw old" rut IT%" go it its) Tue of Ow .I, 'fyst&'* ,adt'air I 1 4 "Itrijigowth 411 thr I 1n; I&I ty COWLV. which MAY IV "u" t" lh' stru MIOCNIA. bO. It a 001 1:00 4k :0 00 'o 1~ a A -Ims"ISM91) 1"1061911 lly'd-imnlift.. Wit fiv 00 1 41 1 A%41sjaulw -plus 00 00 00 00 00. 00 00. 00 00- 00- V.1 2 OL # I f 0 00 0 0 0 0 9 0 0 A I Or 1. 12 N Ll Is 11 a a a Q a 43 a at* 1 'A so A 0 V T'Q LM AW '47511 w C j o* f . pr4 . 1 oNjo ; d i S S W A 41 U M S - ortsi . Sr . . . . . 4 )(Iss Entoligh). Flomof (19 r wlif kstlsllr~ va rinml 141 the 1 . 11l hli l ' 4 u d v y y o p b (usin KAI Pfflkl to C iN . cruc & e g. y at The cmnv4wwuts K AIN ar-I Aoti 340 M so . . , ~ (taliva in obe m0o cartgPoisdi to the famula given 7 :3 . 4 .11. SbUTV) lc�Wtbtf Who . tNwws k4m. C(%,. NIII ond pairt ul the XII.;w'"v`vIA.6svd. at cl cindine. was Obtalrbed as uskst svies having air area see 00 0 in I0 Mq. MM. With N, - I.M4 Oki N, - I RIM % -A =vw fle " 44 "Iti Pam"ll wom l l l t% 11 m c m vv %, an w " y 0 nmwwlinicsymmtttytAnaturapb6vn)ite. catelnuitt". 400 "*no. when studying light mk*s In Istornstones. it) 4"1 coo : "Mit"'Sit 04OW" ee wit". W. I's-fly e 00 1~49 dat U 0" Ow 00 o1, 10, Ow let 0" 0404 uses : tl .00 0 0 * 0 000 00 00 0 0- '900 see I Imes Joes, 2-1-64 G.. is, w - , ; - - ' -m; -i 4- -W-i-a 4 3 9 1 f~lr- Ike Ill I IA 1: : 10 Geese : : is 000 00 0000 0 so 0 leiulto of rravlt,Alrr~ I Shjr~ilr Of Cr/3'.113 I-. r-Ini of alp'-,v l1r. tlv- n-kr- AVv (Coimmt. re- I.: The r%iult.; of 1'ravit-Wonal sh'Ifti;r if ir. v-in3 a:4, :rx-m6irL~1 -*-;i 3.-rinx- linr of u;;n---r rocA crystal face3 wiVi ;.inuie arlstals, fra.a-nL3 oP ro--: t:r- y and olhmr ~vin r-'nurals; (2) the exi3t.-,lco of areA.; Q.* Cry,~Atl f~Cll which ,nmv,~ --on. protectul from Vie u-,ovoi pr=!sa; (3) --vii--nc,? o,.' thv jxi.;Wnct a*' convection cure-.-nU In th-e &q. 3olation fillinj: Vie v,.:ini ;~,Tk!ctinr tlu.- naLur--~ a.,' tho rock surPAce. A I new result of 1:ravitatiou;d 3-artinF, a~ tte ~xli- tence of suspenled crystals, was discovere-J, in a;. fratmv-nt of r0::.,, cf-j3*--Il with in:lusions of fiorou3 rimphibole (oyssolite at.,j prochlorite). it. j. L. o 0 0 It .6 1#4a AL itv 4 0 A c MMOUC OW. Wm cv. DmAWy Ab 11MM C m#. f0s, se,a : ( (fit Kos"); d. C.A. J0 ha la i 00 v l: 6111"CT s aCl I til = di b lw6ft a d um y w 4 A 4 F . c. s. m % 11 hl 094" 14 11,N .~snsn 00 00 AIL! a. d. . IstitillilY etumi VIN& 811-ItIl StIALLURGICIst. LITI[RATWIR CLASSIPOCATIC. ia" I. '01--ss so I' 11, cl,,N44 U'dill Kato itill ,D:::::i*eooooeooooe 0000-00 0 0 0 9 all 0 900 00 0 a "CO , .00 - V. A. (Ilauchev aud 1). Nailk .1w,S S.M. 66, .11% us V RS.% ". --N.o -,, 11,1n. : 2w.- SAIIIIC 11,AILIMtW j141. 11111`1111941LAlt' ~ 00 itr, tins so rd ol age Th, Fr tinjivitt al,14-ar. t.. i. (d. C.A. 26, 11,17' log roe :0 0 see 200 t:00 1,09 too ff--l V *?A Is of I .. 0 A 1 .4 oo*:Oe . I I IQ It It 114'o - 1 0 0 a it 6 10 a loll Aluma kv er: a A a A-_I_,a a- v v I a.,..i 00 A fly 4p J40,049141 go 00 A 00 o0 *o .00 *0 00-0 I i 00 rom tty and colmonb 01- MO. a :00 ! 00 Ms. 1"A I'lewlwf 100 09 ji iiij 1047). ,4 sell g :: 1 00 goo lilloalwo tt&twpuklww I of i 0 p to a 01 a a 4 a 4 a " 00000i 00000000000004 0 0 0 0 Gio 0 0 0 0 0 0 0 0 0 0 0 0 4 ;.Igoe logo AR S 1 0 0 - - of a we a $194 00000000006000 00 U 0 0 0 0 0 0 0 0 1 0 0 0 0 & 0 OA GRIGOReW, D. P. "'Certain Manifestations of tne Influence of Gravitational Force on ~.he iormaticn ard Distribution of fUnerals in Dopusits. Zr:) Vceross Mine ralogiche Skogo cb-Va, ,.'o 2, 1946 (152). (Ijeteorologiya i Gidrologiya, No 6 Nov/Doc 1947) so: U-3216, 3 Apr 1953 GRIGORIYEV, D. F. "The 130th Anniversary of the Russian lUltieralogical ~,*aciety,ll The American Mineralogist, vol. 31, No, 11-12, pp 601-2. 19". Contains infomition on the Mneralogical Society of the U,';SR 0141 ONE m# me = m 009 dew W 0 08 av. FAL Vs `0 1 0641. 6 VID 00: 100 00 1 1 400 so- se, so goo too too see we* Isla" age on m NAIAD% ati- i J i d 9 1 it rn 1 ~ 61 q a 0 *TO : : 90:1 4 4400*964449904100*0 *0600000 01, 0 : : l 00*0000 e IOU -70 aim a 0 e = - GRIGOR-YE-19 D. P. ~/ftq one origin or mimftiaslo D. jp. ariew-yev, n pp OftlakI Tserassiyakago Mineraloglabaskqp Obsk- dmtvle NO I So author chooses as his wthad for studying the WSOU of Alumls sm mutbatim at an us ammufas 4t wlgln of +49 alaeml,, wtvAybg the alumls th,41i. MIT" for this pm7me. so Considers the paetic 81W Iblah we In the formation, of the mixercu, =a slalm to establish, ths history of ainft-als frcm thaft arigin to ~th* ~t of tb*lr chma or gem 'AMR I'A WO/Quartz Apr 1947 Mineril depooits wEpit&XIC ()wergrowth of Quartz on Feldspar," D. P. Grigoriev, I. I. Sbafranovskly, 8 pp *Zap We Min Ob" Vol IM, No 4 ftu&Ies of intergrovths of quartz an& feldspar fr= the Schetocbnays Tam In Transbalkal, lit" D. P, 74 Oct 1947 Geology INIzieralogloal ftatim of the Ural Geological Society.' Do P. Origorly"', Cherter, Miss or Soo, 1 p "Uptski Teeronly MIneralo Obsbobest" Series 2, Part LMM No 3 DIscus"m briefly ime"Ims of Ural Geological Society hold 22 Air 1947 and 5 May 1947. Dismisses s=e of the artlebw submitted for Jud~6ent; also imtIons articles subodOed at 22 Nay 1947 session. - j Oct 1947 TOMID010a *Wes for the Imscalature of Minerals by Their -Chmical ca"Itim,'" D. P. Grigorlyev, 6k pp *Zaplokl Tserosely MIneralo Obehahest" Series 2., ftrt LMM, so 3 NW different methods of naming minerals load to general omfusim, Author oubmits method of rAndng varl6as minerals accaMLIM to their chemical ocupoel- tion. 'Given oxemples to pmve the value of the nev method. 5M3 th j OC .9bornik, i:c:ti'j~-,jjj r _lid rune, 5-, (Let*piri 'Z~hur7-,%l 1-1:,,kh -tAely, PAAM7 Minerals Jul 48 "Chaloobornlte and the Brolution of Its Mineral FOrM9,0 Prof D. P. Origoroyer, li pp "Pr1roda* No 7 Various factors bring about evolution Of mineral form- BrIefly describes effect Of temperature in producing those evolutions. Discusses characterls- tics of Cures 2 and CU2.7684.9 and various geological actiong which change these two different mineral form into chalcoboralts. ORICORIYEV, D. P. Prot t"W)WImerals Oct 48 Slates Structural Analysis wAtcikic Structure of lawswitop" pre D. P. (kr1gorlyev, 1 p mWiroda" So 10 Pmence of rAvemite in U determilned only ro- coutije Woohnikov discovered ravemite-chlorldo slates an Vxyl-Thsh River In southern 'Urals. typical chmical, forma1a and atomic structure of I oral'based, an plans of seeond, pinscold. CorftInm vater of hydration In Its cbmical sake-up,, vb1ch can be loolated, =47 at tomperetwe of 7000. 9r"rm FA 17[49M~ ", .: . It. I i " , , ~j . I-. j. I n wo r 'tudy Of In c,.!,!,,,ncti"n ""th cx-!~rimx 17,1 ref;,!-,rch (?f d L ruly 14, 1048, 9-27 27 1,,ems C : U-385'), 16 lny'li 3utey, Gravois of Cowl vullsavis in thif PY fire.Ism iosposits I the Northern Ural /dfitsin I-ovv:, Ifiv,so,d #7,.1.i Vi 11,00 %% title /it 41141 lot) OK-%-ur only as Vissler. It, 4,0 KAtris. j-.J. Willa Ilse I-Ville for bislies of the \-011111ifli VfAl, Cis I% 411-til-I in :4 rich Wit" tit is Ile. so IT 111MOY sh,il-livitir. Itown h.1rov lio. VAMI'lle tCo,I,,CjOq sr CuAre.1%). ik,u,I;rSd, the liller fare nlinrrxl Inter. ro,ting txvauw of its ;-trjllrli%tn with the synthetic compil. CusleSs too Meruits anti LAindard (C.A. 31, 4MIA). Enafg1te is very lure; furonite *all latuatinite am dovilit. fill- 71* MCIANX=tiC rew"i0ill in the PW(klC OM SM ;I'Lll-lefited by the Mi., litsovio i's low It-f-sy h4gr-na. Alki this, gooll of their issitensittles. The ltmrrKg (d All thd ChaffUsisehl" for graphite In or"'n"t? cast*. Ilse much thilow"t stroscesioW FANITICtefS. anti the jilase,xv of Any coalition" Issoamistift som slathfACite to StAptilte being about that Illypashtsob lh~l a We'" a' intefffiethAtt COMptill. MAT gialpt. " M a"i6cial crMn- by a swldcn hearing to Wgb Illinois, ba--. is dowc. _ in nature a clittact awlsomVials, ACtiVe. Ouchill Of ITAPhitr me formoril Is the and Illith may pow In griphile cir"tals. Stock a womy Avivie r4tind See" 14, P. of. I he coke product km fma cosses; the 1. skip. is Cghly 98911MINtAllt fill the stnioctian of title eqM. $ssittotis - des"41, - -.IIIial. With %'IV F"m cultattile 411 Y41hilif# in Ilse p14.? of thfil,31-vill, I hs, wtwo to at the -Anw 111114- a "fuhn'ttit in Of (from 0 to llf)%). still A decTrow in Fe otrul 8 Mis, Litter frinn X5 to 20%). The jmfvgrn~ pvfitr.h&I,-.tfC and! pyrrimille-hor"ite, tic Am "forbidden": theivicWto the pulasr"foopo, art. In RTnetAl irittleird tit 2 so 3 typic.41 oilli-hot, I- ,it Its, I* III,,, in tits illagnin For-Cti-lll Thr fliff4tooWMAlk- ChIfIlloo At, &1W Amw"Poinkil by torso. riLinforto Joring the Is,-11.41to which air in spremosont With the vr4 taws too I-iMgvrn IC.A. IS. 21). anci it%. phyti.-chms. prinip" gtiv,-n bi, Ko"hinpisil ( 10AW lot the ITActaw. during else snark. Cycle, Cu land S jut obf litirstrilt,11 In the 041111, While PC 1. 4 .0 .1.1 yate"sativally 110ninsitril fris"I lost 1-fini.6tv high. J.r, 111i as listialls"o. *I'lw %,,,I ti( Ilse it" fa.mitt. am and Irronnic enters "SAY be r"l-n0dio low Ow rath. r sick diffemnorts tol the dtjg~o- M it. Os - Gogn-loom 6. stullotuAl tirposiloo, Asset air stors defc! toy little 140fooss Smilar froottlarlik-0 life its thr a" of the Altai. not luctiv .4 the CAuraovot. Its the S. Ural the author dilwithed chalropyrite veins in Itytitc loodissso SpisdiftntlY Of gWtA%OfnSt$C origin. In PVTI1C tor", soplaoskrite anti jpBlrn&tc air metat,imustir nutterAlsiA. tioris; the metal fluccirmion is Zn-Cu-Ph. Them are aloto clither typrs of deposits which. however, show the %Artw =Is "a.. with Fr ~ujfide%. Cil nIrS 11111 A Itni-IVAI d FV 7 -T -L, D. *Ome Rundred Seventy-Five Yews of mineraloff In the Mining Imetituto,w D. P. GrIgorlyev, Active Xlemp Acad Sol UM!-Chalr of Mineral, Leningrad 0 Order of Lenin Mining lost, 8 pp "Zopiski V-S Mineral Obehoh" Part 77, No 3 Witten In honor of the 175th anniversary of the rmnding or the lmtltuto.Smslm convened 1 Now 108. Briefly traoss the hIstcry of the activities of the awe MustrIous am6srm. ii4 USSR/Academy of Science* Geologists Sep 50 $4 New problems of Genetic Minera!o6,- Prof D. P. "Priroda" No 9, pp 22-30 Reviews history of development of genetic miner- alogy and features distinguishing Soviet f foreign genetic mineralogy. i~' Mentions the follow- ing persons as contrilbuting greatly to the develop- ment of the science in the USSR: G. G. Leimsle3s, Leningrad/Moscow, I. I. Shafranovskiy, Leningrad; G. 1. Vertushkov, Sverdlovsk; N. P. Yermskov, V.O.; A. V. Shubmikov, Leningr&d/Moscow; G. L Vazbutskiy, 2ku Leningrad; Ye X. Lazlko, Moscow; S. W. Ivanov, Sverdlovsk; P. S. Vadilo, Kishinev; G. G. Grush- kin, Tashicint; A. Te. Karyakin, Leningrad; N. Yu. Idornikova, Moscow; I. V. logansen, Leningrad; S. A. nudonko, Ieniagrad; and P. F. Ivankin, Frunze. DANA, Jawn Dwight; DANA, Alward Salisbury; RIKOW, V.I., [translator]; POPOV. G.M., [translator]; NENIIDTA, A.V., Etranfilatorl; FRM- KLMMTSKIY, V.A., (translator]; GRIGORITNT, Dope, redaktor; BAIASHOT. L.Ss, redaktor; NIJLIYUWVA, AOT77TWnicheskir redaktoro (The system of mineralogy. Translated from the Inglichl Sistems mineralogii. Pereyod e angltiskogo V.I.Mikheeva i dr. Pod.red. D.PoGrigorlerva. Moskva. Izd-vo inostrannoi lit-ry. Vol,l Iseconi half. Oxydes and hydroxyls) 2-1 polutom. OkIsly i gidrookiely. 1951. 419 p. (KUU 8:5) (Mineralogy) L ameg Dwight; DA.NA, idward Salisbury; BAIA HOVA, M.N., [transWorl; GRIGOROYIWA, NoPe, [translator]: MIUMM, V.I., (translator]; 3HuzMVS1IT, I.I., [translator]; aELGORIYZT. D.P.. redaktor; BALMOV, L.S., redaktor; ILITIN, takhnieheenrIFIftktore (The system of mineralogy. Translated from the Inglishl Sistess, ad- neralogii. Perevod a angliiskogo M.N.Balashavoi, i dr, Moskva, Izd-vo inostrannoi lit-rr. Vol.l. [first half. Blements. sulfides. oulfosaltal 1-i polutom. Blementy, sullfidy, sulfosoli. 1951 607 p' (mineralogy) (XIBA 8:5) CP 14416961); W C.A.46.67rq- The first formation a crymal mucirme In dctd. by the folsys.-cloem. complitlopme of the medium from whirh it is A d"ailloct 41mrsoolon Is given to) crystal wth from The wage of a vein. with a fabric Arm 1PZ 14 ,b, A velims of the Ural in quarts-or"Ir-c"Wite Whiets. Tooranclary, -omp Is of crystals on facts of in- divWu& of an Wor goorristirms and an fragnients (thal- c s). with porallid adlics. tic.. Is tinplomoted. An et Of thmor principles is given for llw regular inorr - groparth of IW" different Crystal SANWO. e.g. 11(4umitr tm Flivolom bromill; gruw1h tie a furciff" PhAme loaptled bripoem t.. WU of growth of The hat is ultra Indicated by flif. fritut hoWic The 'Nifflltd "th Of One CryStA 111TAMP to a bad drimoth on thor properties of the substrounj Ales (tug Isentinvorphic st"Ktiores) an a polarity M crystalks. graphic Alto. The op. of The nut ki formed ton A Virin WAII. ror.. is disrus" Amending to Korniga:,ger ups ipl~s for alpine ralmeral deptaits. with staiist" c scamopp. The pormiltnotic mcbetars, fur The veins of Stitt Crutrall Allso Air given Am quant. tutupirs, whk-h mAy be tilendni rvrn its mineral growth pbenumma In nxtriples rtsulis. W. P. GRIGoll I rxv, Lt Cc n,-,-E- 5,~, Dec em'.77- GRIGORIY19V, D.P. Now requirements o: mineralogy In relation to experimental work on the origin of minerols. (In: Soveshchanie po ekspertmentallnoi mine- ralogii I petrografti. 4th. Koscow, 1952. Trudy, Koskva, 1953. NO-2, P-15-21). (MIRA 7:3) 1. Kafedra mineralogil Leningradekogo ordenoy Lenina I Trudovogo Krasnogo Znaneni gornogo inatituta. (Kineralogy) GRIGORIUV, D.P. Genesis of botryoldal, or metacolloidal aggregates of minerals. Zapiski Ysesoyuz.Hineralog. Obahchestva 82, 7-21 153. (MLRA 6:4) (CA 47 no.17:8591 953) 1. GRTGORIYEVt D. P. 2. U5SR (600) 4. Min-ralogy 7. Origin or calcareous, or metacolloid, collomorphic aggregates of minerals. Zap. Vass. min. ob. - va 82, No. 1, 1953. 9. Monthl List of Russian Accessions, Library of Congress, April -1953, Uncl. 1. ORTCOWYEVO, n- P.; SMLITANTNCV, N. A. 2. USSR (600) 4. Mineralogy - Classification 7. Classification scheme of minerals In the "Course program 'mineralogy' for specialty of geology and mitieral prospecting." Zap. Vses. min. ob-va 82, No. 1, 1953. 9. Monthl List of Russian Accessions, Library of Congress, April -1953, Uncl. 51WILiNOVSKIY, I.I., deyotvitellnyy chlen; MlKUI-AV, V.I., deystvitellnyy cnlen; QRIGORIYAV. D.P.0 deystvitellnyy chlen. Work of A.N. Zavaritakii in crystallography. Zap.Vaes.min.ob-va 82 no,2: 105-108 153- NLRA 6:6) (Crystallography) MOE Tyzv, I). P. 8=/Geophysice - Druse 21 Mar 53 "Two Types of Druse Minerals,"'D. P. Grigor'yev and N. D. Kapitonov,Lenii3grad Mining Inst DAN SSSRI Vol 89, No 3, pp 543-545 Distinguish two types of druse: 1) accretional druse and 2) recrystallized druse. The first type is fre- quently formed in hydrothermic seams and in filler strata; the second type is formed in the cavities of mny mineral rocks. Both types are often found jointly, out formed at different times under different conditions. ?resented by Acad A. A. Polkanow. 272T36 DANA. James Dwight; GRIGOR'YNTqD.P*, rodaktor; GRIGGRITIVA, N-P.Ltrans- latorj; ZRAKMMTfo--t.](:',-"iiaaktor; SHAKVALOV, V.I., tokhnichoskiy rodaktor. LThe system of mineralogy. Translated from the SWiehj Siatema si- noralogil. Perevod a anglitakogo. Vol. 2. ft. 2. LSol*satoo and tollurates, selealtse and tiellurites. chromate@. phosphates. &room&- too and vanadates, antimonatea; antimoultes and arsoultee. vanadium Oxymalts, molybdates and tungetates, organic compoundej Solonaty I tolluraty, solonity I tollurity, khromaty, fonfaty.areenaty I van&- daty, antimonaty; antimonity I arsonity. oketooll vanadita, molibda- ty I vollframaty, orgenicheakie soodinonlia. Pod red. D.P.Grigorle- va. Moskva, Isd-vo Inostrannot lit-ry. 1954. 589 p. kRhU 7:10) (Mineralogy) GRIGORIUV. D.P., doystvitelinyy chlen. a, Records of the Uzbekistan Department of the All-Union Mineral- ogical Society, no-3. Zap.Vssu.min.cb-va 83 no.1:80 154. (KLRA 7-3) (Mineralogy--Periodicals) GRIGORIYU , D.P. Records of the Usbeldotan Branch of the All-Union Mineralogical societys ne.6. SRp.Tw~s.mIn.6b--ro 83 no.2:175 154. OaRA 7:7 ) (Usbekistan-Mineralogic&I societies) (Mineralogical Socie- ties--Usboklstan) 7, qCoru, In --nrl of t L s! r4,neoiL., ,f It In# irti It 'At. 71% !nt~ U- IL -~FiFt. ,t Upo. mlnemlro, (.,-Vti, 811, No 3, ~)P 1 The i,uth,)r cutvildorv the cryeti-111m,tion of v-in mineri-1.ti, irinly ,,u.-~rt7, In filled voitis. In tl.e crysti-Iliveition of qutirtz In open fis- surep, he distint-ulahek three ettiges: (1) in the -Iret Et...C4, the ~-rowth of the Indiviaupl. dirsordered oriented crysttle occurs; (2) In th, qe:Cnd vt~-ge thp. rr.,wth of rPn.* cryst;la In rtc~or~i~ncF- the of [-eomptri~: eelocti,,n occurss with eradwil filli-Ifif t"le cryutvIs ur, Er.wing to~&rd (,ne tn(jthpi--, vnC1 (1) In tht, tLir,A fitip.e or,'.y crystilF, thit nre strIctly ~;erpvrldieublr U) OIL! of thf, vvin cvnerow, there beii.e i,o conci!~tiuns moni-, such cj*y~t:lq; cE~13-y they c;-r, Lrow ind.efinitely lonC (tlho ratrCe of ', s ri, 11 v 1- c ol,,Law~ r f fyree; tpr). All tia-pt, vzt;Efts posseo cpIntlim6ur, pr..CC1k;S of Cr.-Stttlli7p- tion, which cnn teri!-imtte tit tiny of them depeidir. or. c - i I ne. No :;, 1955) Su:). :,z~- '~81, 7 Oct 53 15-57-4 -4546 Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 4, p 79 (USSR) AUTHOR: Grigorlyev, D. P. k a 170'a TI TLE: Some 7otews"on tkahwesutppearance of Chemical ;.1teration In Minerals (Neskollko zamechanly o, yavleniyakh khimi- cheskogo, izmenenlya mineralov) PERIODICAL: Zap. Uzbokist. otd. Vses. minoralog. o-va, 1955, Nr 8, pp 85-104 APSTRACT: Wo types of relations between minerals and their alter- ation products are distinguished: pseudomorphous trans- formation and development of replacement structures with reprecipitation. In pseudonorphous transformation, the solid products of the reaction are formed directly at the site of the reaction and crystallization. They are confined to the volume and form of the altered mineral. During replacement with reprecipitation, there is Card 1/3 more material then the 15-57-4-4546 Some Notes on the Appearance of Chemical Alteration (Cont.) replaced mineral can contain and some material is deposited around the mineral. In Investigating the mechanism of alteration, it Is necessary to distinguish between the mechanisms of introduction and removal of material, and also to recognize the mechanism of the chemical reaction itself. When solutions react with minerals there is a transfer of substance through the Interstices between grains, through pores, or In the crystalline substance itself. The author divides the chemical reactions, originating during alteration of minerals, into simple (combining reactions and dissociating reactions) and complex (representing different combinations of the simple reactions). Reactions of chemical alteration occur directly in minerals. In the crystalline structure of the mineral, during this process and with the mineral retaining its fundamental arrangement, atoms are either added, or removed, or replaced (atoms of small size are moved along Interspaces, expulsion is achieved only by larFe atoms). The comolete alteration of a mineral proceeds in two stages: solution of the mineral and the formation of a combination insoluble under the existing conditions. Cases are 'Known Card 2,3 15-b'7-4-4b46 Some Notes on the Appearnnco of' Chemical Alteration (Cont. ) of replacement developing Irregularly, exhibiting a selective character. Such occurrences tire associated with the distinctive features of the -ninerals themselves, their crystalline structure, and their internal constitution--zoned or 3egmented arrangements. Chemicul reactions without ch~-nge in volume are common, especially in metasomatism. The rule of equal volumes1s true only in pseudo- morphous change. The preservation of outer form snd size of a mineral is sometimes accompanied by a chanCe In volume by remov&l of material, fresh precipitation, and the formation of cavities Lind pores. An Increase in volume may also occur by newly formed material. All volumetric features should be kept In mind during study of' the chemical changes In minerals. The &uthor furnishes examples, Illustrating difforent occurrences of chemical alteration of minerals. Card 3/3 T. A. Ya. C,RiC,-OR ~E A UM/ Geology-Stalactitic formations Card 1/1 Pub. 86-26/39 Authors I Grigorlev) D. P., Prof. Title Stalactites with dissolved ends pericdical t Priroda, 44/1, 114-115, Jan 1955 Abstract I A study is made of stalactites as indicators of geological action. Be- sides the usual stalactites and stalalpites of limestone there are in- stances of their being formed of other materials such as goethite. A study of the shape of stalactite ends, which are partly dissolved can determine the direction of the plumb line during their formation. The time and character of the shifting of parts of the earth's crust can be indicated exactly by stalactites that are inclint,! from their origi,lal position. IllustrAions. Institution t Leningral Kineral Institute Submitted too.. -I-, _~__ -,, GRIGORIYEV.D.P. ,.. ___, V.I.Vernadakil md present-day mineralog7. Zno.Vses.xin.ob-va 84 no.2:136-142 155. (ULRA e:10) (Verandskil. Vl#uUmir Ivanovich. 1863-1945) I! k 4 , ? I VIRTUSHXOY,G.N.; GRIGURIYEV,D.F. , Konstantin Konstantinavleh Matveev; 1875-1954. Zao.Vses.min.ob-va 84 no.2:251-252 '55. (KLRA 8:10) (Natveov, ilonotantin KonstRntinovich, 1875-1954) GRIGCRIYNV.D.P. What to ugenotic mineralogy?" Zap.V~os.nIn.ob-v& 84 no-3:377-378 155. (KLRA 8:11) (Mineraloa) GRIGORIYXV, D.P.; GANCHIVA, L.K. Parallel columnar calcite from Pitkyarants. Zap*Toeoominoeb-va 84 ne.4:443-445 055. (KM 9:2) 1.laf*dra mineralegii Loningradskego gornege instituta. (Pitkyaranta-Ulcite) BELTANDV, N.Y.; GRIGORITIV, D.P.; SHAFRAMOVSKIT, I.I. 111- - - - In memory of B.IA,Osadchov. Up.Tess.,ain.ob-,wo. 84 no.4004-505 '55. (MI&A 9:6) (Omadchav, Boris IAkeylevich, 1912-1954) q P. (010 (L' y f-\j Do R. USSR/ Minerals Pub. 22 38/51 Authors I Gri[:orlyove Do Poo and Gomzulova, 1. Yn, Title Parallel-Co uartz from Avar Koysu sources in DoCestan Periodical j Doke All SS.M' 101/2, :339-342, Mar 11, 1955 Abstract j Mineralogical data are presented regarding the parallel-columnar quartz extracted from the Avar Koysu sources in Dsgestan. The cry- stallogrophic orientation of quartz hexahedrons in parallel-columnar blocks is described. Nine references: 8 USM and 1 German (1928- 1953). Drawinr_sl illustration. Institution t Mining Institute, Leninj:rad Presented byi Academician Do Is bheherbakovs November 30, 10,54 15-57-1-397 Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 1, p 64 (USSR) AUTHOR: Grigorlyev, D. P. TITLE: The Nature of "Colloidal" Minerals (K ponimaniyu pr1rody "kolloidnykh" mineralov) PERIODICAL: Vopr. mineralogii osadochn. obrazo-.raniy, Books 3-4. Llvov, Llvovsk. un-t, 1956, pp 107-108. ABSTRACT: There are two types of individuals: crystalline and amorphous. Crystalline individuals are generally found in so-called "colloidal" minerals. "Colloidal" minerals are characterized by the size of the indi- viduals that constitute them and by the presence of a dispersed medium. Inasmuch as "colloidal" minerals consist of crystalline individuals, it is incorrect to use the term "colloidal minerals." The author proposes that one should speak only of colloidal aggregates of crystalline minerals. It is also incor- Card 1/2 rect to refer to "colloidal" finely dispersed aggregates The Nature of "Colloidal" Minerals (Cont.) 15-57-1-397 and to amorphous minerals that have no dispersed phase. There are intermediate aggregates between colloidal and finely dispersed, and also between colloidal and microaggregates or macroaggregates. There are thus mixtures of colloidal and other aggregates. Card 2/2 T. A. YR. b 7 - ~j - -17 13 ,ransIntion rDm-, '.~D-17, Nr A' T 7, L E- 3rlentlflc of Professor 1. 1. Shafranovskly (Cn -713 -11'lftleth i-irt!-.~iav and the Tvienty-Fiftn Anniversary oC 711s 3cteritific and' Pedago-icul ActivIty) 17'auc~nyye. m. L14- 11 trudy pro'Lessora 1. 1. Shafranovskogo (IV, svyazj s 50- letlyem so dnya roziideniya I 25-lettyu.-, naucirinoy I pedagogiche3~:,-)y deyatellriostlf P'7'Tlj ODIC AL: '.Uncralor.. sb. Llvovak. L;col. a-vo Tri un-te, 19b6, Nr 1-3, pp 369-~77:2. APSTRACT: Scientific works of 1. 1. Fhafranov3kiy center mainly In the field of tl-i(,- morphology of crystals and minerals, and p-a-t1culd-Ily in the problem at' the correlations of the cr-.-,-ltuls wit*n the conditions of their formation. StUdy1n;- the alll.-A questions of the morphology of crystals an'-.* -)V 3tvactural crystallography, he'inferred ~'.ard 1/2 the existenct. of 1103 structural crystallographic 15-57-b-5713 Scientific Works of Professor I. I. Shafranovskiy (Cont.) varieties of simple forms. I. I. Shafranovskiy worked extensively on the problems of crystalline morphology of zircon, quartz and diamond and uncovered a number of new laws in this field. on the basis of this research he came to the conclusion that the "law of zones" (i.e., the law of great circles In crystallography, which plays a fundamental role in the geometry of polyhedrons of crystal p,rowth) must be supplemented by the law of coniform surfaces (i,e,, the law of small circles which appear mainly in the geometry of diffusion forms). A series of I. I. Shafranovskiy's published works is devoted to the history of crystallography and mineralogy, and especially to the evaluation of the scientific legacy of Ye. S. Federov. At present I. I. Shafranovskiy holds the Chair of Crystallography at the Leningrad Mining Institute. Card 2/2 D. I. G. 7~ GIUGOILI.UV 4A(., professor. OGIgantIc potholem.* ]Prtrod& 45 n0.12:112 D 056. (NM 10:2) 1. Loningradekty gorayy Inatttut. (Potholes)