SCIENTIFIC ABSTRACT GAPCHENKO, M.V. - GAPICH, V.I.

Document Type: 
Document Number (FOIA) /ESDN (CREST): 
CIA-RDP86-00513R000514310006-1
Release Decision: 
RIF
Original Classification: 
S
Document Page Count: 
100
Document Creation Date: 
November 2, 2016
Document Release Date: 
July 19, 2001
Sequence Number: 
6
Case Number: 
Publication Date: 
December 31, 1967
Content Type: 
SCIENTIFIC ABSTRACT
File: 
AttachmentSize
PDF icon CIA-RDP86-00513R000514310006-1.pdf2.74 MB
Body: 
I lQ I I I a 11 if I? to Ii ai ItU11 ?. a1, k 11 1. ti v AA C-A L-J--A * A--I-JL.-L aIt I AA 0 Lf it it 1I:r. b. ./ , , -". 00 Ii II f, 00 . 00 00 40 .4H. Od,tY jknlj AU CXCC%4 (.1 Afirr scidifyinS whb IICI titrave with o.1 N tin-ulliie. I,-,c flar foothr ulut, had ' ' ll, ..I I It" jw(tvIltitik irdblerke (fit th, 1c,olic N'.011 1111PIMICS thr disidatioll 4 th. mllfitr. Ilv 11'. -$ K. at .00 'If I hc air. Kam"It 00 400 00 00 -00 00 00 400 .00 00 S S L A L1 .1TALLUP41C&S. UUMATIM CLASSWICATIC" 0 ""'a" too 00 it - u 8 AV .0 it, AM I s 2 ew 0 v w 34 A) 0 0 0 0 4; 0" J 0 0 0 0 0 0 0 0 0 0 0 0 0 0 **Soo 0 0 000 0 0 0 0 0 0 61 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 41 0 0 0 0 0 0 0 0 0 0 0 00 so so 0 W 0 W T- 9 a To W a a to a W 4FIN-Iftw'm a SW V wig W W v W W v or -W or We _v _w W-w 0 0 00 a t is Is 11 is 11 11 to p a )o A M age a r At AL -A-X- r -aa 1-1 I-L-AA r. a4m 1, 1 A 6 I vato @o o0olot -09 00 00 f 00 00 A 00 00 00 09 a 00 #1 -06 Um W Mvdnt Ww"m OW as valummete C 490"NAma- .00 d" 4d own sn"mob. m. V. (1wbmku OW o. (I. the amtnt*.%An. of le n1tri, tvxntxl,. knit) a FrknmeM A&A. fill the dask with Coo and "I a NNI- -00 IM% exce" of a t1trated "n. of V, * atmve that rvt:t@-vd -00 for reofiKtiom. Continue paming the C(h and afttr b min. 00 titrate the exce" V- with fiffic slum In the [it e pf 6 infran:tw as indicatnir. The ind"tm tmcn AmId X =00 such t6t I drop of the V* @ u4n. obt-Kild lie %ufficicnt to t re 0 dccultwise2 h,lqtl,t tuffice to rftt,wr the cohcathmi. '11w nt"h,xi cam coo t,e u@t to det. mitmphrnal, nitrimniline and pkiac @sd within the range of 0.5-141 mg. It. Z. Kamich 64TALLUNGICAL LITINIATUAt CLOMPKATION b u 0 of oc W q 0 0 0 0 Fee coo 400 we* ties coo too too .6. do. all Itt F-1 ---- 0-9, an I 1 0 tot 0 o I IF 0 1 a a I v IN $If a a It a "7 n I is 0 0 0 0 0 0 .0 0 0 a 0 0 0 0 4 a 0 0 0 0 0 so 0 0 a 0 0 0 Ito MOM 36 1 Ito T-W a L . a F N 6*0fal ONOCIORS ..c -VCorot,#$ '.V1. -00 7 (7x_ -00 gog to *0 gas Douctwe of ce"m Will, 0-741 N1. V., c-aw-; FrOrlit"I O*z I Ise -r jus intemiye greets va"a- 9*0 16'", Ttw Fractim is Priective and makm it pc,-Isihlr to ,Ivtvvt Cu in HOAc tnedium its Ow Pre- (it all mciall Soo ru-tpc Ce. An. As and uttivakut Its. As sail fit -hould 1 C d rid. u 0 and the t. firit reintivcd hy ppin. swith dil. 1 in The filtrate. Ka"110% too Igo* &Im-tLA NAML~AL 1.111411011 C1,45WICATOW Ago a too I I -4 181640 At Ov CIA 1114411 Ow 4ftw All u 9 AV 10 is I V j W p I I 0 a Is a a 9 a it a 19 an It a An a as a It 0 1 V Of I dl 6 3 a r o I 41 0 0 41 * 0 : 0 * 0 0 0 0 0 0 41 0 0 0 If 0 * S 0 0 0 0 0 0 0-411 0 * 0 0 000 a 000000606 s o* 's Goootomf*6660*06 *31 A A- c a a F RROCE-541 AftO PNCPC&f,Ci ACtC o* oo 00 go 00 *00 lei "'fm Ow, Gwhe@k 300 09 swim. M. V. each" go ).-Jft-ntmw Ot Nilt w" N 00 of C', b, 00 A.A-PodeoraY 00 jtfjAk9VI(fICA& LfTf.4TUMf_ CLASS)OKAIKU ;71 0 111) W-Os--T -Ail a 4 IS 1w 0 w M10 a I !In 1 41 A 9 A;-IL A I A X 1 9 7, 00 00 a 111 ly 11 "1 s oxxvilivm$ll; U be a 11 U 11 0 a Al 41 &1 a ago jw@ 1100 of Olval"I WA@VAGII%Iltl ail 1119,10601 In voloolelflo **all" M. V. U41kboilt., jis Sill)II).-koll: i art given ola the use of thrilled talka. al Mol " * to reduce mittv, &rA nilrooto puuln -00 to amino compils. ThiG 6 lollowed by titration of the Ca" Mo with analsoctium Intel alum in the prelance of mitiltykne him as an intikictor. The fallownis 4cirm. were made. Picroe deod. Add a 11 -3-fold e%cvq^ at %to %An. to the olunple. stAil plitaing in CL%. add 2-3 divM of -00 Indocatur 2-3 min. tatle, and thrate the vxml, Mo. Cap- -00 fivros. Pr@fuvv 6 Ito, Itator - 1-m slivvit, met-I r%,vlyl -tvvroil lite that ah. Ithould he adtictl to the %ample it) I ago toplit. -4 nit stmilthenyl b).Irtsi v Wenhir dutiotit lite d4dit, s4 the acid voln. tot %It*. PO OWJ Ca. the Fe Wa. ppiti. with uld,iouts slid the Co with The plits. were then dissolved in acetone and aliquot A " r age were iltrated with Met- vAn. 0. Z. Kam h crog .11 L A 84TALLUOSKAL LITIGATUN CLAtUPKAIME slow 1.10W .1. 43.. age a a 1-i-- a jb U a AV 10 11 0 v pcpttwa units 1911* Iceman I 0 0 to 0 0 0 0 0 4 0 4 sooooe*aeeoe :000004004 a see ago age see ago 00 .1,illaw to Joe v o1al It rd 0 -1 0 1 W go 9 do 4 3 a dW 0 6 0 0 0 0 0 0 X It U tj 14 Is 0 A a c 't F C R I IL L k t A-IL-Y--q I -k 90 4 .00C1111% ..0 INCOWA, @t Delartainatiou of potassium In tainefil (trIduers and sad@. X1. V. GaVcbenko and 0. G. Sheint,is. larmf- 00 96 *mine metboal (C.A. 35. UMAP) Is prolwywd for the detu. 0 of IC in simple and mixed fertiliten an.1 in .%ik. In the f i d f ili fi h i h t 0 00 xe ot- cAsco m ert zers, rit remove t e sul c.arul p ur PhU9iCACikl%4sIU&)W%: *Go with 400 ad. wAter. titter, and treat An Almjuot portion 90 with tnagnesiamixt. Filter after 10 min.. %-h with 2.5@ ' 00 Ni Is, ew-Ap. the filtrate wml wash waters to dryness. CAI -00 cine carefully to expel N11# malt 9, di"olyr in 0.11cf. and 1i '00 foranAlyms. An the cuw (it "Is, eu.,Aith lICI. add Nit, 09 %, until turbWity forms. then add tlrxq.wic MCC1, .4". 00 go to ppt. phosphoric acid. titter, wash with hot @ater. ev..p. h d fil h d l i 40 0 was trate an walem ta t e rynevq. ca c ne tocilO Nil, 0 , -.41ts, diAvAve in water, and u%e foran.klv@i%. Accur.acyof the ""thod 1. As g-Xt 4s JhAt obtain"I "ith the chlor@ -6 00 I'Luu..te M@th-l. It. K--h 004 i;00 -10 0 zoo @41jAL%,t*G4CAt. 1,11111411AIN CLOWK&TIC11 W, moo. tl@vllv- .10 (P.. got total" W--T--r r 4 - I P q U to so a It a a it v it It a It X 00000000000004 Olo :10 00000000000000.&-� BOO too Croo VO* 00 0 FW 0 2 a 1 3 0 v LO (U. 11 1 , I i A4, 1040COOS 0 00000*0! :' -* o Le -9 - -0-0 0 a 0 0 * 00 00660641, CA number. Nt. V. 11.1twhenko. Zm$hkaw Loh. 16. alo ctwnjml@. with a stinilard vAn. 4 TiCla afiffikmltit@ orr vn, rtmntvr"l with umnedy". RepLacrittenttATiCl,l)yl,iv;,knt V IWIT.it, titftion at r"ll tvlnp@ in the Abu-s"t "t RMICIle salt and the olUf Chkllgt iS VCfy VI@AT. %11,Vfh ts dis- Wilve-I in N IIAO. and is reducril by Zn.lfg. Tyj@cnl- analy.scA td sevcval dyes ctmfinns the app6valviLty of the fraptrut. 0. M. Koolat"30 Z @t P 7 Meiiiinuou '01 pbospbstes, In bc er -WMA XN@M116kol- Amch. Trudy atellh. -4iutract -In the .050, Nm 32j788. , bf 11 the fixotybditte - tin cd hat, for.tha Mimi -@-O 21: bet el 0 Ustakubidi,- @- solid collol n. of An,',d-Ary, jejatin layer of a phot o F, tb4inaturatlititi-&-nd lasts, for a I a time Th or Plates am ti@e& in,* Wn, of 0 'i6atilhiiij @xu C until tho AgUr - Is - ,, 'Placed4or 5@' 10,15"20 and." FAO,, and Snally Wei. w @bf-@ifeciitaUun th 'water. latm aft t -16 mi, hill - trd&W f6r. 10 to n. with. ' vio. ffatthtr Inacase. 20fix; @.Of @KjFd(CN)i untU W. lace'. wasb d dried. The Ion ed, min b , must be a IlZiis;i agalbst a natural 9"s 9 wfz t C., D. lConix GAPCF1 11',iD M, G.. @N,,,Invalid Otechestvenncy voyny (g. Kiyev); G rrva i Otechestyennoy voyny (g. Kiy*v); SAVIVSKIT 1, invalid Otechestvennoy voyrq (r.. Xiyev): KOLODOCHKA, B., Invalid Otechestvennoy voyny (g. Kiyev); KHOVANSKIY, A., invalid Otechestvennoy voyny (g. Kiyev). Beine order Into the ortanization of motor wheelchair repnir. Prom.koop. -to.6:24 Je 157. (MLRA 10:7) (Orthopedic apparatus) QW1_291W P-Ir-- JULTUE1. Z.M.; PIATONOV, K. I.; OREL-KRATUSHKIN. V.S.. FMIKOVA. K.P.: ICRYMY. T.L., redaktor; PAYWYA, K.K., tekhhi- chaskly redaktor LOCollective farm building" pavilion; a guidebook] Pavilton OPostroi- ki kolkhoinogo sela'; putevoditell. Moskva. Gos. Izd-vo selkhoz. lit-ry. 1956. 26 p. (KLRA 9.10) 1. Moscow. Tessoyuznaya sellskokhozyVstvennaya vystavical 1954- 2. Direktor pavillonov (for Platonov) (Moscow-Farm buildings-fthibitions) VOLKOV, Vladizair Fedorovich; CHICHEM, Aleksandr lvanovich;_gL@h 4-- A.A retsenzent; GEMMIUS, G.K.) reteenzent; NESUROV, Tu.F., '--==j nauchrqy red,; VIASOVA, Z.V., red.; KRYAKOVA, D.K.p tekhn. red. [Ship refrigerating machines and installations) Sudovye kholodill- rqe mashiny i ustanovki. Leningrad, Gos. soiuznoe izd-vo sudo- stroit. pro shl. 1961. 261 P. WIRA 15:2) "Iftefrigeration on ships) GAPMY:" G.S.:. GORODSIMO Mikhail Mikhaylovich Niew system of state agricultural produce procuraments on -collective farm 10 novoi sisteme zagotovok sellskokho- ziaistvenrqkh produktov v kolkhozakh. Moskva Gos.izd-vo polit.lit-ry, 1999. 93 P. 4MIA 15::Lo) (Produce trade) GAPBYZNOK, N.I., Geroy, Sovetakogo Soyuza, gvardii podpolkovnik Selecting the direction of approach to the target by bombers. Vest.Vozd.Fl. 40 no-7:13 18 JI '57. (MIRA 10:11) iBombing, Aerial) 86-58-4-6/27 AVTHOR: Gapeyepok, 11. J., Guards Col, Hero of the Sxrtet Union TITLE: Low-Altitude Operations of Bombers Against Railroads (Dvystviya bombardirovshchikcv s malykh vysot po zheleznym dorogam) PERODICAL: Vestnik vozdushnogo flota, 1958, Nr 4, pp 23-29 (USSR) ABG'MCT: The article deals with the low-altitude operations of bcabers against railroad junctions, rolling stock, bridges, and tunnelfi. The author is of the opinion-that attaclEs agsinst kbe railroaas fr(= low alti- tudes are more efficient than those from higher altitudes. This is so for the following reasons: The expected mean percentage of bomb hits from an altitude of 300 - JOC x- is'4.5 times higher than J'rom 6,000 m. I a altitude; the range of detection of low flying banbers by the enemy radar is shorter; the enemy AAA is capable of delivering fire against low flying aircraft at altitudes not lower than 300 M.5 the use of It ground-to-air" guided missiles is limited at low altitudes. Since the railroad junctions and stations are usually subject to ntrong enemy AA defenses, air attacks on trains can be carried out more successfully not while the trains halt at stations, but. on the tracks between stations. Card 1/2 Low-Altitude operations (Cont.) 86-58-4-6/27 The railroad bridges should be bombed on the first appr3ach with the use of either optical or radar bombsights. A bridge Is approached at a 15 - 30 angle in relation to its longer side. Tunnels can be put out of use by bombing their entrances -nxd exits. At lower altitudes than 200 m. good results can be expected by ricochetting the bombs into the tunnel entrance. The author pays much attention to the proper selee- tion. of approach direction to the terget. Under limited visibility conditions the railroad objectives am bombed frcm low altitudes with the aid of radar bomsights. The railroad junctions, stations, bridges, and high embankments have a good radar contrast, and thus the radar bomb- sight can often be used in searching for targets. Four diagrams. AVAILABLE- Library of congress Card 2/2 1. Low altitude bombing 2. Train bombing SIIISHOV LH. , POIXDVIIIKY Geroy 'ovetskogo Soyuza, kancLvoyennykh zauk 4i,'@ . IIII., polkovniZ Geroy Sovetskogo Soyuza, kand, V5-YUn-n-yRh nauk Session of a department in an aviation unit. Vest. Vozd. Fl. no.1006 0 161, (KM 15:2) (Aeronautics, Military) 4i 4 )1 jik :ui P:-.' 1; P', I V@ 6/( A40 1 'j/( x 'r) 4 /(x )94 V. S. -, Ay-.,.:-.LI u, Yti. A.; ;oIroIinn):iy, A.; !I.; *Ycklorov' V. IVIL110"r, A. M. ; J'@*.-'vl in:;kiy, "". A. VY:;oL:;*ruJy, Yu. A.; Za-mulkiy, V. I.I.; @3jatxov, V. V.;' f. V.; D. A.; Corm-mov, Yu. G.; 37.ialwimov, 1;. P.; V. V. :2. Class 42, '.'0. 104466 51--iounccd by "Nof tepribor.". ?actory Ad.'u@nistra-.ion of :.:oaUorsovn3a@kjioz (Zavod "Neftepribor" ;--,oz&prz;ovnaI-kho,-.a)7 lzolare'. prom obr--z tov zn, no. 15, !966, 94 -",Y):^ TAGS: nneirmolio@,,ic --tation, sciemolot;ic instrument '2"LIL, -'io Author Crrtif icate presents a --r-Asmic stmtion '6ontaiiiinC saim;dc -i.' '; 2i u --a- 'lloqraph, a maZaotic drum dc"ctor,, recordin- amplifier unitt, an oGc. a chawlel repioeluut4@on unit,' a control unit, a reproduction amplifier, a be, a dmm wit1h photoCrapChio paper, a retransmitting imit, pro a Oupply. To inercaaa the reliability when tranaf erring from* oporation, withl method o" rcflcc@cd waves to the method of refracted waves, a filter unit is connected be%-.rccn the first and second stages of the recording =plifiar unit. -Ccrd 1/2 UDCI 550-340i19! ACC KIZ: iL-iit and a reel typo ma@7iotic recorder are connected in series -.o I@hc of the recordinC; amplifier unit. For operation with the method of ;-efracto(i the fUtor WiLt @as frequency cutoffs of 7-30 hL, and for operation at z;aa--Ircqucncy cut-of.-L's of 20-50 hz. To increase the reliability of the recorded d,iza vith operation loy the mnthod of regulated directional reception, a switching -@@it, for tao chamiels to be summed, a static correction unit, and a su=inj unit are c@,-nnocted in scrica betwoon the maMotic drum recorder and the reproduction amplifier. "o increaze reliability vjhcn transforrin, T from operation with the mothod or re- --cd v.-aves to seismic lo-- n-, a frequency selection unit is connected between Lac multichz=nel borehole probe and the magnetic drum recorder. To improve the i quality of tho recorded ma-teriall an electron beam unit for introducirC static and e:lna:.-.-.c corrections is connected between the reproduction amplifier and the drum with oCrap]hic paper. S-U3 GOD.@; 00/ Slu-B"'i Dwra.. 05'jay65 Cof-6 GAPnEVq A.P. Conditions governing the formation and localization of talc with a low iron content in the Lesser Kara-Tau. Trudy IGEM no.63:103-129 ,61. (MIRA 14:9) (Kara-Tau--Tale) I GAFEUV@@. P-.-- - Low iron powdery ofgthe Lesser Kara-Tau. Trudy IGEM 1.10.48;144-160 161. @kfffM 15:1) (Kara-Tau--Tale) GAPErEV, A.F.; TABYLDIYEV, K.T. --- T Genesis and distribution of tale in the Lesser Kara-Tait (southern Kazakhstan). Zakonom. razm. polezn. iskop. 6:.,586-615 162. (MIRA 16t;6) 1. Institut geologii rudnykh mestorozbdaniy, petrograflio mineralogii i gookhimij AN SSSR. (Kara-Tau-Talc) andr Petrovic ; PF J P E@,_Ajekp h MOV, V.P., doktor geol.-Miner. nank, otv. red. '___ [New tale-bearing province of the Lesser Karatau: petrography, genesis, and characteristics of distribution] Novaia te.11ko- nofmaia provintsila kfLrebta Malyi Karatau; petrograftiz., ge- nezis., zakonorternosti razaeshcheniia. Moskva, Naukajp 1965. 1714 p. (MIRA 18-4.) GAFFfEEV, A. Z. and BUD IKOV., N. Ye. "Some of the Problems of Asiuring the Therapeutic and Prophylactic Service on Ships", Militar7-Medical Journal, No. 8, p 12, Aug 1955. GAPE=E, Boris Mikhaylovich; VILINER, S.L., retsenzent; SHURNOVA, (Taking apart, cleaning and reassembling wrist watches]Raz- borka, chistka i sborka, naruclmykh chanov. Moskva., Mashgiz, 1961 20 P. (MIRA 15:9) iClocks and watches-Repairing and adjusting) Boris 1-11kha lovich; MEFS, So*'crrcn @@F7L@-V,p .. 1 1 - Y@ , .1 1 - .. ..I avel Dmitriyevich; IOFJIIOVA, TS.B., red. LCleaning of clocks] ChIstka chasov. Nlojkva, Legkaia industrila, 3.965. 86 p. (FIR4 18:4) Innervation of the small intestine in ma slat. no.4:118-129 '58- . - (immus-immuTioN) Vap.morf-.Perif.nerv. (KIRA 13:5) GAPEYEV@ I.A. @ Development of the innervation of the amall section o-I the intestine in cats. Vop. morf. perif. nerv. aist. no-5:95-1-10'60. (MIRL 3423) (INTESTINv-3-IMRVATION) GAPEYKV, I.A. Development of the neural and cellular elemento of Auerbach's plexus of the small intestine in man. Vop. morfi,perif. nerve sist. no.6:1-16-133163. IIRA 16110) (MM4T&RIC PIMS) GAPEM, N. The coal Industry must have unified production standards Sote.trud 4 no.8:85-88 Ag '59. (MU 131-1) (Coal mines and mining-Production standards) GAPEYEV, N.; ISAIGHEVA, A.; SOFINSKIY, M. Uniform production norms for coal and shale mines. Sots. trud 6 no-4:92-95 AP 161. (KMA 16:7) (Coal mines and mining-Production standards) (Shale) I GAWEYEV. N.; ZOZULYA, A. __ A------- Z__@ "Flaming and introducing the technical production standards in mines.9 -71ftfisind by N. Gapeev, A. Zomaia. Sots.trud. 7 no.6:155-158 Je 162. (MIRA 16:2) (Mineral industries-Production standards) GAFEYEVJP N. Wages in mixed brigades in ko4l mines. Sots.trud 8 no.3:79-81 Mr 163. (MA 160) (Doneto Basin-Wages-Goal miners) C insh.; GXR M I, G.V., inzh. Precast reinforced concrete columns to be used in housing con'. structlon. Diul. strol. tekh. 14 no.9:-16-17 S 157. (MIRA 10:12) 1. Trest Chelyab metallmrs troy. (Columns. Concrete) SHCHURKINO M.; Responses of economic councils to the editors' requests. Gor. zhur. no.5s79 VT 162. (MIRA 16il) 1. Glavnyy inzhener Upravlenlys, gornometallurgicheskoy i khimicheskoy pron7shlennosti TSelinnogo soveta narbdnogo khozysystva (for,5hchurkin). 2. Zamestitell glavnogo inzh. Upravleniya mash*ostroitellnoy i metalloobrabatyvayushchey pron7shlennosti Orenburgskogo soveta narodb6go khozyaystva (for Gapayev). (Ore dressing) (Boring machinery) 3;y GAi:)@,N, S. T. I ,,.'aking use of natural cold for road con-tructiGn. F.oskva, Izd-vo dorozhno-tekhn. lit-ry, 1951. (IMIc 53-854) Collation of the original: 119 p. Microfilm T-14 GOWN, S.I., kandidat tekhnicheskM nauk. Using cofferdam piling In place of ordinar7 piles. Transp. stroi. 5 no- 10;26-27 D '55a (KIRA 90) (Piling (Civil engineering)) - GAPSM. B.I., kwdidat tokhnicheskikh nauk. - , A*V@N'I@f4` ftrtial, freeing of a ship's hull from ice by means of metal tank@. Rech.transp. 14 no.12 D '55. (NLRA 9:3) (%Ips-AsIntonance tuA repair) (Ice on rivers, lakes, etc.) GAPSYNT, S.I.. imndidat tokhnicheekth nauk. Now method for driving large dismeter metal piles. Strot. prom. 33 no.9:13-15 3 .155. (XLRA 9:1) (Piling'(Civil engineering)) - - *I. A--- kand, tekhn. nauk. Miminating the heaving of foundations. Transp. stroi. 7 no.12: 7-10 D '57. OURA 11:2) (Foundations) (Prozen grounde) GAPEYST, S.I., kand,tekhn.nauk - .,. -,u , Ili - .t, @ , ", Sw .,a. - Depth of foundations in permafrost areas. Transp. stroi. 8 no.10:19-20 0 158. (NIRA 11:11) (Foundations) (Frozen ground) kand. tekhn. naiik. - , Ibqmrimental investigations of antiswelling meauurea. Strai. Prim. 36 no.2:25-28 F 158. (KIRA 17 -, 2 ) (Foundations) (Soil otabilization) (Frozen ground) GAEU,YUV, S-I-.1cand.tekhn.nauk Culverts laid on raised supports and filtering rock cuohions. Transp.stroi. 9 no.1:44-45 Ja '59. (MIRA 12:2) (Culverts) @ G&nUV, 3.;.,ka tekhn.nauk . r4e 1@pes of structures built on waterways covered with lea during the winter. Tranap.strot. 9 no-3:29-30 Mr 159. (MM 12:4) (Bridges) (Culverts) (Ice on rivers, lakes. etc.) GLPZIW, S.I., kand.tekhn.nauk Tecbnical Specifications for Building in PermfrOBt ShOuld be revised. 2@@p.stroi. 10 no-7:46-47, 56 Jl 160. (KM 13:7) (Frozen ground) (Axilding-Contracts and specifications) PF',V=R, BNAW!, V@Ti"" riV'@"YT,:V,. Anihor's certiftcatei for Soviet tn-@nt.ionq. Strri. t.rubc-prov. 9 no.1u;35 0 164. (MIRA 18:7) tr-kh-n. naijk (.Ipnirw.-v?,', wocir,-n brilgas. Put I I pul no, 18:7) KUZOVLEVY G.M., inzh.;,PAPEYEV, S.p. Use of asphalt-concrete lining. Gidr. i stroi. 30 no-5:22-25 My 160. (Asphalt concrete) (MM 14-5) (Reservoirs) I I GAPBM, V. One can't do much with such textbooks. Okhr.truds. i sots. strakh- 3 no.2:37-38 7 160. (MIRA 13:6) 1. Tekhnicheskly Inspektor Leningradskogo oblsovprofa. (Industrial safety-Study and teaching) Safety engineering in working under winter conditions. Biul. tekh.inform. 5 no.2:26-27 7 '59. (MIRA 12:4) (Building-Cold weather conditions) (Industrial safety) GAFEYEV) Vladimir flikoleyevich; ENURNOV, N.A., red,; fTZGER, D.P., red. izd- red, (Forms and methods of spreading information on safety measures in construction] Formy i metody propagandy tekhniki bezopasnosti na stroitel'stve. Travmatizm i ago uchet. Pod obshchei red. N.A.Smir- nova. Leningrad, Leningradsk'i Dom nauchno-teklui. propagarAy 1960. 4;: P. (Bibliotechka stroitelia po tekhnike bezopasnosti no.2@ WiFu 14: 10) (Building-Safety measures) (Building-Accidents) GAPEYEV, V.N., inzh. Analyzing causes of accidents at construction sites in Leningrad. Bezop. truds. v prdm- 4 no. 5:17-18 My 160. (MIRA 14:5) 1. Tekhnicheskiy inspektor Lenoblsovprofa. (Leningrad-Building-Accidents) -GAPEYEV, Vladimir Nikolayevic@, inzh.; SMIRNOV, N.A., prof., red.; PAPIYEVP V.R., red.izd-va; BELOGUROVA, I.A., takhn.red. (Problems of aecident prevention in winter construction and assambly]Voprosy tekhoiki bezopasnosti pri proizvodstve strottellno-montazhnykh rabot v zimnee vremin. Pad obshchei red. N.A.Smirnova. Leningrad, Leningr. dom nauchno-tekhn. propagandy, 1962. 14 p. (Bibliotechka stroi- telia po tekhnike bazopasnosti, no.8) (MIRA 16:3) (Building-Cold weather conditions) 00. GA=W,-V3AWimIr-NikoU "ey ch SVIRNOV, N.A., prof., red.; , inzh.; , FREGER, D.P., red.izd-va; BEWGUROVA, I.A., tekhn.red. (Dissemination of information on accident prevention in construction. Recording and analysis of accidents]Propaganda tekhniki bezopa=osti na stroitellstva. Uchet i analiz travina- tizma. Pod obshcbei red. N.A.Smirnova. Leningrad, 1962. 35 P- (Loningradskii dom naucbno-tekhnichoskoi propagandy. Seriia: Bibliotechka stroltelia po tekhnike bezopasnosti, no.2) (Building-Accidents) (MIRA 15--12) GAPEYEV, V.V. Using the reflection method for studying the subsurface structure of the Bayram-Ali-Ropetek zone of uplifts. Nefte- gaz. geol. i geofiz. no-3t22-25 163. (MIRA .16:8) 1. Vostochnaya geofizicheskaya ekspeditsiya. ACCESSIM NR: A4,014861 S/0202/63/000/006/0030/004:L AUTHIORS: _ Gapeyov, V. - V.; GGYMan, B- X- TITLE: Spacial methods in the application of gravity cuid seismic exploration in southoastern Kara Kum t AN Turkn@. Izv. Seriya fiziko-tekhnicheskikh, khizdcheskilch i SOURCE: goologicheskildi nauk, no. 6, 1963, 36-41 TOPIC TAGS; gravity survey, seismic survey, temperature facttor, heat factor, zero point, nonlinear behavior ABSTRACT: Difficulties in accurate gravity surveying in southeastern Kara Kwna involve terrain problems in the desert region, sharp changes in tempereture, and other fact tors. The principal steady noise in gravity surveying is nonlinear, perhaps chancing in sign. This undesirable property is due primarily to blasts of he@t2 which subject the instrument to wide and, frequently, dangerous changes Gratur-a. These changes are especially bad during the summer months. in t omp Corrections for this nonlinear behavior of the zero point cannot always be made accurately by use of a second (control) gravimeter, which is subjected to tho same Ccrd.1/3@ ACCESSION NR: APLoi4861 sharp temperature changes. Erractic results are commonly obtained, Linear variations are possible only when the temperature changes are unif orm, and unidi- rectional, during certain intervals of the day. It is necessary to select such intervals., when temperature changes are rather constant,, and to work only during these times. Operation at night has proved to be especially useful because of the slower rate of temperature change, and this is particularly true for the sumaer months. The seismic technique employ-ad depends on both surface conditions and rock properties at depth. Subsurface conditions are generally satisfactor7 in this pai-t of Kara Kum,, several good reflecting horizons commonly being present, and two marker horizons being almost everywhere discernible. But surface difficulties are encountered in areas of barchan dunes and other f orms of shifting sand. Velocity values are irregular in sand., and the absorption of energy is excessive. Fx.peri-. irents have shown that proper grouping of detectors in special arrays gives reliable seismic data. Tests were made with arrays of 11 detectors arranged on a base of 45,, 60, 75, 100, and 125 m,, with distances between group centers of 30, 20, and 10 m. Best results were obtained for arrays on the longer base (100 m). A number of '@aulta and platform-type alk-ructures have been delineated with this toclu'iivo. Tho authors believe the refinements they propose are to be recommended for gravity and seismic surveys in sandy desert regions. Orig. art. has: 1 figilre, Card 2/3 ACCESSION Da: APL-024861 ASSGCIYTIOI!: Otudel geofiziki i seyswologii Ml Turkmenskoy SM (Depart moat ol' Geoplipics *ard Seis.-wlogyLN Turkmea SSR) SUB"MT'AM: 02;-'6b63 DATE AcQ: lgFab64 EXL: 00:@ SUB CODE: AS INO REF SOVs 000 OTIC. R: 000, Card 313 ALIYEV, I.M.; GAPEYEV, V.V.; KIRIYENKO, G.I. Prospects for finding oil and gas in the Bayramah-Repetek zone of uplift. Izv. AN Turk. SSR.Ser. fiz.-tekh., khim. i geol. nauk no.6:48-52 163. (MIRA 18tl) 1. Vsesoyuznyy nauchno-issledovatellskly geologo@-razvedoclmyy institut. V.V.; GRY"N, b,F- F-aspecta 'or flndirg p?as end :), @ --n tk-.e T:lkht.-i--S-.-.2rr rep,,' -n, llefteC-9z4 gacl. I geofiz. nc-.i,-4r.-42 't,4. (M.'RA 17,;j'; F 1. Vostocf@naya ckatte-littly-s fic..1 U-ra-.1001ya geologii I okhra,7y n(--ir pri -Iov-@,.,@ lln!.st.rov Tu:km"iskoy GAFEM L.M. Deep-seated structurer or -the Bayram-Ali-Repetek zone of uplifts, based on detailed selmde datIL. Geol. nefti i ass, 7 no @:9-16 My 163. fm 16: @ 1, Upravlenlye Vologii i okhrarq nedr pri Sovete Ministrov Turkmenskay SSR. Turkmnistan-GboloU, Structural) Mrbienistan-Sainda prospecting) GAPEYEV, V.Y,..; GEYMAN, B.M. Geophysics in studying the tectonics ot the Repetek salt domes. Sov. geol. 6 no.10:92-A02 0 163. (MIIUI 17:1) 1. Vostochnaya geofizicheskaya ekspeditsiya Upravleniya geologii i okhrany nedr pri Sovete Ministrov Turkmenskoy SSR. GPJ'F'CF,Vy V.V.,, inzh.; TOCIIILKJN, V.N., inzli. Blouing-through of the steamPlpes of a 300 thousand kw. b-.Icc;k. Energetik. 13 no.2.20-9-'." F 165. (MIRA is..c) dAPEYEV, Ye. and TUMAMV, 1. 1. !trw.-- - ZMA - Influence of friut-bearing organs in the maternal plant. Trucl)r Inst., Fiziol. rast., 7,, No 39 1951, --GAPEYEVK,.-A. Don't duplicate other departments.- Fin. SSSR 37 no.11:50-51 N163. (MIRA. 17:2) 1. flachallnik finansovo-sbytovogo otdela Moskovskogo zavoda "Dinamo" im. Kirova. o @ r s 0 06 oo 0 a 0 0 0 w v -M- Ji I I I III It 11 IS IS it 16 it 14 IS a S. It St ISW a is v 31 p w .1 IS m 0 r , I I , I . a t L-1 A, a -I- A x -so Gold In the r4atern Tarbefetal V M C., M. Gqwrva. $I'm "If. fjow 09, Nks.. Hf",& /Amr@ MY. No IfJAi1IdVj.-it@ ft'llft-fit-1 IIV (I'lAtt? .1111 chalimpytite and pyrite mur tust nummotm Ali I% IsmO III afr tit quatta-like r-1- thAt t,j"r, tat thr conuct foltv A th. 9 VAli-Citr intrlz%pyrl, By @alhcvonx A 111C f"1111AII-1- of Ir Au is lramixxtnl I-? thr vklrfik@ dt-W%iti A11MIS tbr FI%,r 0 0 rmnvr-vS,. 90 lithalAnash. PAIA(lit dIld 91tipar-Rulik are of the jcmd,,t 8 so j intr1r.t. W. R. l(clin 10 00 too 00 el zoo Oat goo 00 1 1 zoo 00 j -,400 00 00 ::o 0 00 f I I -tIALW61C-L LITINAT641 CL-SSIPKATIC- *0 2:00 ' tql@l, It C.-I all ` " ' q r - j--1 I , 0 ,'I -I u @, a a a It u " tv tt it rq @ -I ,T, to A 1 14 0 0 0 0 0 0 0 0 0 9 0 0 0 0 0 0 0 6 0 18019 0 0 omoo 0 * 0 0 o 0 0 0 o 00 9 00 0 0 0 0 0 0 o 0 o 0 o o 0 0 0 o 09 so *so Go 0 # 0 0 4, 0 0 0 0 0 & 0 00 0 o see 0 09 ***** 0 *:T:Trrra=G* 4 .' A . . I I, 0:.;t , - ': , t it " I .. .. @ , o . z . ' . " I I I I Ask, @t 4 it of 4' go CampWaitess Imns Totrun. southern Tyan-Shan. %I . ki I" l 7 M flovis. inera ,lpss . XA. - W. tiaw minii.J.1 78, N,,. 2. till lit 191-11- Cimpim. Irc 'ol"Itor'l its I .11kc, .1.1 -111, 111 tit. iirs " _-ot .-rn r%.iti stLt,,. w- go t--gied ..... I ..... Oirm I I. ...... .'III . ttIvIlIK -4 1110111 k Its,' -110- It-A 'I keg iq.11% "it it I Its: ".41fig 'W .,IV .%I I iiiii.m.led toy lit, ..-vultrileg. of sic"11 ki'I'l, .4 J..'111% frindt'd .111A wfl'oth'l pilf.11tv p.111% 4. M-INA wip.11111-1 ;,It, Im I 'I' I... Is ..I. tit. 111.1. 4 ... I I., so 0 title Ill M like w-411161 I smpl..11114 Atib I.-It"Ifill. m., 1 1. 8, 4'. ach, I I-Aflot-vikiles its fil4livi.111A tty't.d., If ill litmitil.it 4jil, Imith 4.11114 (miction tiIII0 ..( pyw%mv. plictiovir"o isrimirls.ibic Ixvmw i,f their tatiu,tidiv Istich Ikv. 0 Koss eI'Vitc,it. rise- 1 .11. go by "'LIM111C Ind .-Itcli 'N'.11 'i'l inchi'i.m@ -.1 0 Art Ilephrillic. while tilt- Klioullil-IIII.. i.111111,1V @-llgw 0 0: Omfpwm4a 1w. gV.101,111% A14V qwvurml its 111VIINCII'le %clu'14111. 0111CII ciWfItCPAIVII lit !tit ITMIUC MlIctill V%iII1 lit INE11111tV Kt Ml- on the drAvage (Akv@. Sem-lithie till hol,m.1, JUltitC. And Italict i, 1, tittv V11.111KIII to) I. hirdwititle. XenWithl, D1 ChrrAir ow pvtilivnitr " ills 00 oliville and a mr A.. Atillub"t. m,I itr'kfiti, ...I o4i I w v a- 0 0 0,04000 oto 0-0- I, V, It to I, I ar* zoo Fee 4lioiil is ,I it ot@ to sit to *lot of IT n it '111 413 :.Olt Ker"allites from Toyun. I, M III&I"p.: .11101crul. f MA. - xre-lli 79,69-71(19.5111. -Tire alk r.k.k. ..I flit s. 4 Tyun@Shan utft previtus,ly wilt, xrorrAliv kno,tti I% "trachjrdoicritc,.*',411ht)iiKlI Illy V'WO". It-11. ,rnitcB. ClAnIptlMlitCl. Anil ffl4vfIVhIqtIiIC1 "efr 'IV, TINA Ntkro-"ic stiklic, Intl I ill in miAlv- Tr Im- It* Lm @antitc which Ate in K-1.1p.-Ilem fill 11W.%% I@Ijm hn Utin fork t)lv Civiril by IWv. .111d .1111 ismovil- It 1, fti t1FIYCIlArACIcft'tiv I(W tht- S. I'vml-StLlpl. thm Ille em7tites are not oliwirve.1 ;I, vein mills. r 9,ions in Awwn. with dimite- ; )illy Imitalt.. and the Alk atilittrokis tirentionvial.ivearr tlr@-04NI :@ therrium important I'm the ismlct@lmuhtilc t4 timpimit, lifictentiAtittris in IntemiciliAlv-diteouc rawk. III flit- IN, rive-grauttoid weir,. asid that III hy ., %oViimii, Of IlIC $441!-1111 ill alkal-. I-,I I, ..i.1 .NIX( 0. ill the Trill illlnl,wsl@ ..f I ft. a % fit, 'ffi"S "UrAtIrt i- field. fly the ,r%*.tll 4 Vt A.C , Ili0tile. Ti-Augile. AellifItc. In4r. -4ivlllr. allik. title, antl ACIV-WiA -Mawlkskm from Toyun. 5 Tyan-Sma. tiow usm@talj ll). W A4 ruck" %ilh 14migile. U1311 JAJOJCIA@ (52,@ AM III If"' I INT'. 49,@ iO OW JA-I- 'ivhery). aspi a -knw. cry'l. InAlm, by ibusuUntanakime. Chcin.aiuly.~-vjtcgivtti.4mit;tnii. tured with ar. numichiquit" awl irsimichiquite. Irtmil th, Nlt-rscnA vukwwe@, atul shikh1unitc. Tlk' Uljly@ 4ti 1101. cusclaNive enough to mliblib a nc- I yiw uf nwrachi. quites In the Toyun wcurrencc@. Init thcre are lblinet imlividLial friturt, in their chem. mad mincral,pgmil ttsupa. The chid doubts Arc Wecl ma the 1.*., t Oul tp- p4mudy mmte AlA was drid. t.vthtr V& ith SiO.. %i luch I- c"lently too high for W4 lmic i-wk. %i-. liito "tin".) go. cf. NIL'A-ir. 6I.J. 33, deft-ribAml @% Ifachyttoksite, the Mir in questhin is tit Ill. Isy A tl,,w them. Awdyaw as a tytp@-.d lainpinphyric N-kinkinor, thm-ly to- Lilrdtolewhirnile. It orrettroin the vallry44 river Afrauki. The nxk is ChAlacterucif by linsphilk.le 1.11VIISArtyall (111) 16) 30 lam. WWII). and lew co2roc-cryst. lchl"mr, in a dense, bukoft". emod mass. SuhtwifinAte are ofivigw. alit' ctw- stated and Ictilly (UM11 %ritti- liths. The grt%tl%4 IIIIAia ANS INNI I AIM 3 IIJU Ittle As At flIlr III i1n; hip"lictit. The (41.14ar I. rulti.istiv urvel A NS-Ca IfIlIxIi.11. 'I be pi,1411rur i. a typh-A allitite. Inclow Ifucliws rrIA16-n the ilivine (70'@ rrmkn tit Awspritti-tt. 1-111--fife. Afill misphll.ile i,l A IVIII...41 611knikov, Iliwile I@ .Ally tit .1ftioligIV ti*Vl%ltll %Ihlf.tolk' jolicii-tifo% NrIllithoic ".6, lAftil,"l; it 1, al-1,41tully laWlys rrl.l.tr4,f by MI.Ati.r. whih mAir ltritogro Ile pnni.wr. The Liet Out Cz-Na fcklsl%Lr%.trr entirely Al,,rut ocTm% with the OICIII. 1AC11.9% nt1c4L froun the Analyis; at di.wiguilhr, the I.kittkinilc fritto c-.w%ite. tmhrnitc. Atilt trAchviloirnte. J,hc tit othtr nwk twj@ h4rucIrrue,% the lArkinkinite as a fin-Unix-fulic oliffric"ILItilm lifixturt ol lu%tlts And ir-Achv,1,4eIitc-- W. hitel GAMLVA, G. H. Toy,mi 17;, 1 1 - -';@ 1 -.1 L - ,I L t@ @, . 4 n . C) I) . -asaits cC Tc.yun- Zap. 81 lc,. 3, 1,452 - I I'cnthl LL;t ct' Russian Acceblons, Library of Congress, DEcember 19,52. UnclasAficd. GMYJWA, G.M. WWWF Alkaline magmatic region of the Maritime Territory. Dokl.AN SSSR 94 no.3:535-536 J& 154. (ULRA 7;1) 1. Vsesoyusnyy nauchno-Issledovatel'skly geologicheskiy Institut, LeniaCmd. Predstayleno akademikou S.I,.Xironovym. (Maritime Territory-Aeology) (Geology-Maritime Territory) USM/1-lining Petrography Card 1/1 Autipwo 1. Gapepva, G'a M, Tith, i Discovery o?)MRratrites 7 in the territory of the USSR. Periodical Dokl. AN SSSRj 97) Ed. 11 155 1@6, July 1954 Albsteact Data are presented on the -petrology of the alkaline magmatic deposits of the seashore provinces. The presence of ankaritrites (rare magmatic formations) in the USSR, was established. Ten references. Institution All-Union Scientific-Research Geological Institute 'Presented by Academician, D. S, K.orzhinskiy, May 3, 1954 GAPEYEVA, G.R. " *ife-picrites in Medvezhlys nountain. Hat. VSRG3I no. 21:5- @- @#` @ @@5 7 0 (MIRA 11:7) (Sikhote-Alin' Range-Basalt) GAPEMAS G.M. Position of klaberlite in the genetic classification of rocks. Biul. VSEGEI no.ltM-340 158. (MM 14:51' (Kimberlite) G"'-I)eyeva, G. M., Verbitskaya, it. P. SOV12o-122-2-32142 TITLZ': r1ruptive Hyperbasite Breccia of the Southern Urals (Eruptivnaya giperbazitovaya brokchiya Yuzhnogo Vrala) FE"ITODICAL: Dot:l,-(Iy Akademii nauk SSSR, 1958, Vol 122, Ur 2, pp 281 - 283 (Tjssa) A3')T,',,'ACT- it, the fall of 1956, S.@.'Moskaleva, while studying the hyperbasite masses of Yuz'hnyy Krak, discovered. an eruptive hyperbasite breccia in the bed of the Sukhoy Uzyan River near the confluence of the Belaya Rivers. At that time, however, the scientific value of the discovery was not appreciated and the outcrop was not carefully atudiod to determine the nature of the breccia, i.e. whether it was actually an eruptive rock or merely cemented river gravels. in 1957 no information from borings was obtained, but the mine workings in the area, in apite of their insignificant depth., afforded useful observations. The principal breccia outcrop occurs ' in the bed of the Sukhoy Uzyan River near the mouth of the Myslyayevskiy Sprinc-, on the walls of the abruptly widened valley tht. hyperbasite rock of the Card 1/3 Southern Krak t1assif is exposed. The breccia is covered by Erupti.c HyperbasiteBreccia of the Southern Urals SOV/2o-122-2-32/42 alluvium and soil varying in thickness from 0 to 0.75 m- It forms a lens-like body of irre@@ular outline (17o x 70 m) everywhere in contact with a non-cemented riverbed- marble. The e:cposed breecia in the river bed is structurally irregular. It consists of firm, greyish yellow masses, primarily composed of weatherinG products, carbonates with lesser anmotuitr nf serpentine and nontronite, yet still rich in hyperbasite -fragments. Sorting of the fragments by the river is not pronounced though they are to some extent dif!:erentially rounded. Microscopically the breccia is composed predomin,antly of hyperbasite rock , but the difficult-to-ascertain mine::-al composition hinders determination of the genesis. However, the river bed gravels in contact with the breccia lack rocks of extrusive appearance. The possibility of an eruptive ultrabasic breccia on the western side of the Ural must be considered from the standpoint of the general geology. The wide dispersal of diamonds along the western flank of the Urals testifies to the nearness of their source. Diamonds are known to occur in Kimberlite, a type o. hyperbasite Card 2/.) breccia. The heterogeneous structure of the wastern and eastern Eruptive Hyperbaelte Breccia of the Southern'Urals SOY/2o-122-2-32/42 zones of the Urals (Rafe 1,2) indicates that theories including them both in one fold system are poorly founded. The western zone is not a folded geouynclinal structure but the edge of the craton, Thus the occurmce of an extrusive hyperbasite brecois. is possible from general geologic considerations. There are 2 references,, 2 of' which are Soviet. ASSOCIATION:Vaesoyuznyy nauchno,isaledovatellakiy geoloe-icheekiy institut (All-Union Scientific Geologic Reaearch Institute ) PRESENTED: April 14, 19580 by D,S.Korzhinakiyq Member, Academy of Sciences, USSR SUBMITTED: April li, 1958 Card le- 30) SOV/132-59-3-3/15 AUTHORS: Verbitskaya. N.P., and Gapeyeva, G.r,L. T I On the Potential Diamond OriCins in th:2 Diamond Fields of the 17est-Sloped Urals PERIODICAL: 3azvedka i okhrana nedr, 1959, Nr 3, pp 8-12, (USSTZ) ABSTIACT: The authors point out that several new diamond deposits have been discovered in the above-mentioned region during the last years "on the rivers Aiq Belaya, Yurezan', etc.), but proved to be too small to be exploitcd on an industrial scale. This critical state of affairs is partly due to the divided state of opinion of joviet scientists on the diamond deposits, -aith several schools of thought being in existence. Thus, N.K. Vysotskiy, A.A. Kukharenko, V.S. 'I'rofinov, S.V. '.!osk.`LI('va ana others maintain that there I V is a close connection betweon tho diamonds found in the west-sloDed Urals ard the ultra-b,,@sic rocks of the plati- num-bearin.- strata- of that mountain nart. This is best illustrated in the g-olorical scheme of the Central and Card 1/2 South Urals (see page 9). Another group of scientists SOV/132-59-3-3/15 On the Potential Diamond Ozi,--'Lns in the Diamond Fields cf the 71'est-Sloped Urals (G.V. Pisemskiyq ZT.111. Vvedenskaya, A.V. Khabakov, and V.A. Dargavich) laold that the diamond deposits mi,,7ht derive frim Pale-,zol-, r,@-:ks representitic: secondary dianzond-bear- inG c:)Iloctoxo. --he authors give prcference to the first- mentioned and furnish the following, proof: the lower :,.)cks o-,currin& in that area - Ordovician and Ashinsl-lva fcr:n:7,tior,3 - contairt such minerals as garnets of the pyT-_@pe 4czic3 and mi,,roscopic partic:.1es of diamonds. The lattez wE-r.! found on the Sidorova 1.1ountain, Visimskiy rayon aad a'-,,zzi,@ the Serebryanka river, near the Xedrov- ka Settlement, T"th V3-2,G7E and TsZTIGRI institutes carrying ort research wr_@rk ip those areas. In addition to this, the following 1;ientist !-mes are citi2d in this article: K.F. Sprines, P.T. Kr@,tc;j , Yu.D. Smirnov, Yu.L. Orlov, and Mi- n@ralogist M.T. OrIcTa. There am- 1 map and 3 Soviet re- ferenres. A330CIATION: Vj7"'GT I Card 2/2 3 (8). AUTHOR: Gapeyeva, G. M. SOV'/20-126-1-43/62 TITLE: Ussurite - a Peculiar Variety of Alkaline Basaltiform, Rook (Ussurit - osobaya raznovidnost'shchelochnykh bazal'toidnykh porod) PERIODICALt Doklady Akademii nauk SSSR, 1959, Vol 126, Nr 1, PP 157-159 (USSR) ABSTRACT: The author found the rock variety mentioned in the title in the province of Primor'ye (Pacific). She did not find sufficient analogies among the known basaltoid rooks. Since the mentioned rooks occur not only in the separately occurring alkaline basaltoids on the upper course of the Ussuri River, but also for example in Mongolia and the southern Tyarl'-Shan' it is worth while separating it as a special variety and to describe it more thoroughly. According to its chemism it is most similar o the trachydolerites. Ussurite can, however, not be identified with them because of peculiarities of its minera- logical composition and structure. These differences are described by the author. Table 1 gives the oxide content. The rock discussed here ia gradually transformed into varieties Card 1/2 which are similar to the common trachydolerites. These Ussurite -a Peculiar Variety of Alkaline Basaltiform SOV120-126-1-43162 Rock ASSOCIATION: PRESENTED: SUBMITTED: varieties are, however, somewhat more melanocratic and differ from the typical trachydolerites by textural and structural peculiarities. The combination of the chemism peculiarities, of the mineralogical composition and structure as they are described above are not known for any other alkaline basaltoid rock. The mentioned rock is called ussurite beoause of its occurrence at the Ussuri River. There are 1 figure, I table, and 6 Soviet references. Vsesoyuznyy nauchno-iseledovatel'skiy geolog:Loheskiy institut (All-Union Scientific Geological Research Institute) March 6j 19599 by D. S. Korzhinskiy, Academician November 5, 1958 Card 2/2 AFANASIYEV, G.D., otv.red.; USTIYEV, Ye.K.. doktor geol.-min..nauk, red.; GAPMEVA, G.M., doktor geol.-min.nauk, red.; KOPTRY-DVORUIKOV, _T_.Z_._,-ff-6kT-6rge ol. -min. nauk, red.; IJOURV, A.P., doktor geol.- min.n,auk. red.; FAVORSKAYA, M.A., doktor geol.-min.nauk, red.; CHEPIKOVA, I.M., red.izd-va; DOROXHINA, I.N., tekhn.red. [Petrographic provinces, igneous and metamorphic roc):sj Petro- graficheskie provintsii, izver2hannye i metamorfichettkie gornye porody. Moskva, Izd-vo Akad.nauk SSSR, 1960. 343 p.. (Doklady sovetakikh geologov. Proble.ma 13). (KIRA 13:9) 1. International Geological Congress. 21st, Copenhagen, 1960. 2. Chlen-korrespondent AN SSSR (for Afenaslyev). (Petrography) GAFITEVA, G.M. - - -------- Genesis of lamprophyres and their position in the genetic classifica- tIon of rocks. Zap. Voss. min. ob-va 89 no.5:542-554 160. (KIRA 13:10) (UmProphyree) Zrul)tivc '-roccia in Gl@ol. i --Oofi--. 10:14- 61 " 60. (MIIA 14'*2) 1. Vso-.o.,ruznTr Muclft'c-is 7:. c! i.,r -coic@,ichen-11dy instit tut , Loningro.d. iiri Valle-!) --PArolof;y) (a-,,c;,avo.o'z r, (Uss KHUDOBINA, Yelena Afanaslyevna; GAPMEVA, G.M. nauchnyy red.; REEHERT, L.A.., vedushchiy red.; WYAWYEVA, I.M., tokhn.red. [Problem of oil and gas potentials of Central Asia] Problema neftegazonoonosti Sredeni Azii. Leningrad, Goe.nauchno--tekbn. izd-vo neft. i gorno-.toplivnoi lit-ry. Leningr,otd-nie.. Vol./p [Igenous rocks in western Turkmenial Magmaticheskie porody zapodnoi Turkmenii. 1961. 118-p. (Leningrad. VsesoiuZD3,i geo- logicheskii institut. Tn*, vol.45). (MMA 34: 10) (Turkmenistan-Rocks, Igneous) GAFEIEVA 1 0. M, --------- L%bthodological importance of petrographic azialysis of rocks for the interpretation of their geological position. Infom.sbor.VSEGEI noo50.,3-19 161. OUU 15:8) (petrology) FAVORSKAYA, X.A.; RUB9 M.G.; KIGAY, V.A.; IZOKH, EpP.; GAPEYEVA, G.H.; PREOMMHENSKAYA, G.K.; USTIM, Ye.K., doktor otv.red.; ROZAHOV, Yu.A.., rpd.izd-va; ULOYANOVA, O.G., tekhn.red. [Magmatic activity and metallogenic features of the Silchote-AlLn' Range and the lake Muuaka region] Magmatizrn Sikhote-A3--Lnia i Prikkan- kaiskogo raiona i ego metallogenicheskie osobennosti., I'lookvap Izd-vo Alcad. nauk SSSR, 1961. 34 p. (Akademiia nauk SSSR. Institut, geologii rudZykh mestorozhdeniij petrogrmfiii, mineralogii i gedlimii. Trudyp no.45). MIRA 150) (Sikhote-Alin' Range-Rocks, Igneous) (Mianka Lake region-Rocksp Ijenous) GAFEYEVA, G.M. Kimberlitelike picrites in the Lesozavodsk region. Geol. i geofiz. no.4t53-63 163. (MIRA 16slo) 1. Vsesoyuznyy nauchno-issledovatellskiy geologicheskiy institut, Leningrad. DOMI.All, Nina Borisovna, @-V=MHVA@, Valentina Ivanovna; VEYNBERG, A.K.; ijubiIIIGHi&, E.Ya.; MDANOV, V.V.; ZOTOVA, I.F.; IUvEV, M.G., TRODIA, V.Ya.; KFOREEVA, B.Ya.; SHOLPO, L.Ye.; GIpEyEVA, G.M., red.; KAU-1,YKOVA, I.A., ved. red. (Physical nroperties of rocks and minerals in the U.S.S.R.) Fizicheskie svoistva gornykh porod i poleznykh iskopaeriykh SSSR. Moskva, Nedra, 1964. 325 P. (M.M 18.1) 1. Leningrad. Vsesoyuznyy goologichoskly institut. GAPEYEVA , G. M. Alkali basaltolds of the Kirov upland. Zap. Vses- min. Olb--va 93 no.3;304-317 164. (MIFV. 18--3) 14--57-7-14515 Translation from: Referativn y zhurnal, Geografiya, 1957, Nr 7, P 40 (USSR AUTHOR: Gapeyeva, M. M. TITLE: Traces of Ancient Glacial Activity in the Baykal-Vitim Highland (K voprosu o proyavlenii drevney leUnikovoy deyatellnosti na territorii Bayk&lo-Vitimeskogo nagorlya) PERIODIGAL: V sb: Materialy po chetvertich. geol. i geomorfol. SSSR, Moscow, Gosgeoltekhizdat, 1956, pp 129-145 ABSTRACT: This study discusses finds of allogene gravels and boulders on the Siberian Platform. Analysis of this information permits the following conclusions: 1) a substantial amount of coarse clastic material on the Baikal-Patomskoye Highland area was carried 150 km or 180 km from south to north, and from the Patomskoye Card 1/2 Highland area for 300 Ian to 350 km onto the Siberian Traces of Ancient Glacial Activity (Cont.. ) . ' 14-57-7-14515 Platform. 2) Surface gravels loca@ed to the west and northwest of the Highland area, and containing elastic material brought from the Patomskoye Highland, are identical in age and origin with gravels fr,;m the basin of the Vilyuy River. -The latter gravels are overlain by marine deposits with Dogger fauna, while surface gravels in the upper reaches of the Lower Tunguska River contain many pebbles, fragments ok'trap and tuffaceous rocks of Triassic age. Thus,,the time when gravel deposits were transported is established between the end of the Triassic and the beginning of the Dogger ages, and data obtained from pollen analyses determine it as Middle Jurassic. The conclusion is reached that allogene gravels and boulders of the Siberian Platform were deposited by a glacier. The Baikal- Patomskoye Highland area was the center of this glaciation. The age of this gla@iation has been established as Rhaetian-Liassic. The article includes a map showing the distribution and routes followed by the loosq deposits of Lower Jurassic glaciation in the Baikal- Vitim mountiin area, and a bibliography of 23 title$,. Card 2/2 D. A. Timofeyev MALYARL'VSKIT. Boris Ivenovich; KILLMR, Ye.Y., nauchn" red.; GAPMVA. T., red. (Electric equipsient of industrial enterprises; training manual] Blektrooborudovanie promprodprilatil; uohebnoe posobie. Leningrad. Severo-Zapadnyl zaocha7i politakhn.in-t. See.). Dlectrio equipment of bleat furnaos roomaj Slektrooborudovanis metallurgicheakikh 2avodov. No.l. [Electric equipment of blest furnace rooms] 1960. 88 p. (MIRA 13:11) (Blast furnaces--Electric equipment) ZILIBERNMI, Jzralll losifovich, kand. tekhn. nauk; KATSIIAN, Yuriy Abramovich; GkPEYEVA, T., red. ..... .. --- (Multiresonator drift-tube klystrons; design textbook for a course in "Superhigh-frequency techniques and apparatus") Mnogorezonatornye proletpye klistrony; posobie k proekti.ro- vaniiu po kursu nTekhnika i pribory sverkhvysokikh chastot." Leningrad, Severo-Zapadnyi zaochnyi politekhn. in-t 1964 ' 55 P. (MIRA 18:31 KOROLI, ClIga Yevgenlyevna, dotsent, kand.tekbn.nauk; q@ , @VA@,@. p red - [Theoretical mechanics; trafectories of artificial earth satellites; correspondence course] Teoreticheskaia mekhanika; traektorii iskusEAvennykh sputnikov Zemli; pisimennye lektsii. Lenirgradq Severo-zapadnyi zaochnyi politekhn.in-tg 1960. 28 p. (KM l4s6) (Artificial satellites) VASSERMAN, Nina Borisovna; KASHCHEYEV, V.M., kand. tekhn. nawk, nauchn. red.; _G@PEY EVA ,.Z,.,,red. (Theoretical mechanics; kinematics of a mas3 point. Written lectures] Teoreticheakaia makhanika; kinematfla tochki. Pialmannye lektaii. Leningrad,, Sever o-ZapadjV:L za- ochnyi politekhn. in-t, 1965. 51 P. (MIRA 1911) GAFKMAJ, V.M. Perforation of gastric ulcer following X-ray examination. Vrach. dolo no.6:134-135 Je'63. (MIR;@ 1.6:9) (fMIC UILER) (STOMAM-RO10GRANY) C_ L3 pt-4 ... JD ACCESSION HR: AP5007175 6/0296/65/000/003/0042/0043 AUVIOR: Kutnenko-A-1,; Bqr1n6va, L, I.; Moshkin. P. A. I VoAov, 1. S.., Hikolayeva, V. M.; Mikhaylov, A. LIK M eyfell, TITLE: A cutting compound for cold finishing of metals. Class 23, No. 167939 -SOURCE: Byulleten' izabreteniy i tovarnykh znakov,'no. 36 1965, 42-43 'TOPIC TAGS: coolant. cutting fluid ABSTRACT: An Author*s Certificate has been granted'for a coolant with the follow- @ing composition: dialkylphenylphosphates or phthalic, adipic-or se 'bacie asters or i higher esters of monocarboxylic acid with alcohols containing from 4 to 10 atoms of! icarbon per molecule; or esters of polyhydrie alcohols and.monocarboxylic acids @whlch conta*In from 5 to 10 carbon atome per.moloculei ASSOCIATION: Moskovskiy avtomoblilnyy-savod Imont. 1. Likhachava (Moscoii Auto- mobile. rac@_O@ Card 1/2 N L @2571-66 ACC NR: AP5023379 @A) SOURCE CODE: 31776V666*7664, /bd_3,G/bO_3 7-1 AIPTmTO'Ri Gapich, P. ORG: none TTTILE: From a shovel to complex excavating machinery SOTMC'E: Tekhnika i vooruzheniye, no. 4, 1965, 36-37 TOPTO TAGS: excavating machinery, engineering machinery, vehicle engineering A-'PSTPACrP: -.This is a review of trench digging equipment used since the Russo-Turkish I-Tar of 1877. The EP-121, ET-1411 EV-251, and BT- 352 trenchers were designed and adopted as military equipment- in the years Of 1940-1963. Fxtensive use of the high speed BTN trencher be.-an in 1956, The BW trencher has an efficiency of 0.5-0.7 km/h, and a carrying rate of up to 30 Ion/hr. The history of the development of rsillitary technology shows that manual labor.will be replaced by machines in the near future. Ori-. art. hast I figure SUB CODE: 15,13/ STMM T)Arnr-,: none L Cqro_. 11@1 L 4 A L LTL@@. EWP(k)l EW(q)/M Ps.. AM Pf W/ `AC ESSICK VR: AP3001434 S101V63VjP0()O1C6510d 1�/100 @J 0 MFHOM: Ohl Ve I.; i Ga4 L. Replacing seoless b7 elastically wold6d stainless sted ones I slsouki:': 1!etallurg, no. 5., !T13 -21 19 V TOPIC ;tAGS: pipe,* searless pipe,.welded.-pipe, stainless steel pi _pa ',ABSTRACT: The advantng6s 'and shortcomings of cold-rolled 8.stainless steel pipes made @of":-ibl'ded blank are compared to those of hot-rolled sbamless pipes. The advantages .!.of: the blank: i's -115% J)Lthe coat of,the welded. 3 fformer type are; -10 - 41ower; 2) a pip cmi: be made in one operation;.3) a@greater accuracy is.attain'ed in pipe dirensions- 74Y the Ut-rolling defects on the*inside.surface of the.pipe"are absent. @bwevar, I ltlie:'j3i6duction of.such piped meets with the f ollowing' 'di f rlcultie@. i Th@,argon are, ,.we2d%"ng pro uces a porous zone inside-the pipe along the 'seem.- A brittl.e metal iis formed on the outer surface of the seam, producing'-certain defects formed .60 @0-rolling nnd in @the lorering of the corrobion-resistani;:e along the jivnetion ;area. I 1he inside -burr was too high and formed laps along the seam margins during .1,coid rolling. The authors conclude that these defects can be eliminated if the Arittle idetal layer is scraped from'tbe pipe avrfaco, nnd.if:tbe steel rollers in Car@ ,@ 1, M- ON --- M E @ NiA ". . @ . 1. ..i : @ -@ M-M- MAIM, RUMORS ZM:KOVSKIYY B.D., kand. tekhn. nauk; ZILI-FIERS11'THE', L.I., kand. tekhn. navk,; MIZF'.T?I.,, V.I., inzh.; PETRUNIN, Ye.f,., in-,h.; TIAT"YU,.K, G.7., inzh.; Prinimali uchastiye: HATULMOV, L.I.; NECHIPOREJU, DUPLIY, G.D.; GAPICH., V.I.; FATEYEVA,.A.F ; DYNIKO, N.M.; LUGOVENKO, I.P.; POSTIL, I.S.; BEZRODITMI, !.Ya. Investigating the possibility of manufacturing welded tube blanks for cold forming. Proizv. trub no.11:67-72 163. JMIRA 17:11)