SCIENTIFIC ABSTRACT BUSHIN, P. M. - BUSHINSKIY, G.I.

Document Type: 
Document Number (FOIA) /ESDN (CREST): 
CIA-RDP86-00513R000307720001-1
Release Decision: 
RIF
Original Classification: 
S
Document Page Count: 
100
Document Creation Date: 
November 2, 2016
Document Release Date: 
June 12, 2000
Sequence Number: 
1
Case Number: 
Publication Date: 
December 31, 1967
Content Type: 
SCIENCEAB
File: 
AttachmentSize
PDF icon CIA-RDP86-00513R000307720001-1.pdf1.93 MB
Body: 
,_-, BUSHINPaval Mikhaylovich _ [Irrigation of viwYards] Polivy vinogradnikov. Moskva, Goes izd-vo sellkhos. lit-ry, 1960. 87 p, (MIRA 34:10) (Viticulture) BUSHIN, V., inzh.; YEFRMOV. A., inzh., DMITRIYMKO, A., inzh. Precast tile floors. Stroitel' no-5:10 Vq 160. (MIRA 13:9) (Tiles) (floors) BUSHIN, V. N. "High-Speed Method for the Determination of the Moisture in Moisture-Containing Materials." Cand Tech Sci, Rhar1kov Polytechnic Inst, Khar1kov, 1954. (KL, No 2, Jan 55) Survey of Scientific and Technical Dissertations Defended at USSR Higher Educational Institutions (13) SO: Sum. No. 598, 29 Jul 55 YESYUTIN, Leonid Sergeyevich; _BMIN.,Va_,,__Fetsenzent; ZOTOV, '..A., retsenzent-, YEDVEDEV, P.I., retsenzent; EYZERVAII, V.L., retsenzent; REGELISON, L,14.r kand, tekhn. nauk., dots., red,; DOZORTSEVA, Ch.I,, red, [Elements of antenna and wave-guide systems] Elementy antenno-vo.inovodnykh ustroistv~ Moskva, Izd-vo Mosk. univ., 1964z 102 p. (MIRA 17:11) V1300 (16113~ 11A 11!13J 5,.2,L10 " 111,6 ,,,B J04-5 AUTHORS: Natanson, E. M., KQzachek, TITLE: Electrolytic Method of Prodacing Intermetallic Compound 11mBi_ PERIODICAL: Doklady Akademii nauk SSSR, 8h673 S/020/60/135/001/026/030 B016/BO67 N. N., and Bushin, V. V. the Highly Disperse _V1 1960, Vol. 135, No. 1, pp-137-139 TEXT: Intermetallic compounds of many metals are effective semiconductors, and have valuable magnetic properties, especially in the highly disperse state. The ferromagnetic properties of manganese-bismuth alloys have long been known (Ref. 1). They are caused by the formation of the intermetallic MnBi compound (Ref. 2). The manganese-bismuth alloys which contain a large amount of MnBi have a high coercive force and other valuable proper- ties which increase with increasing dispersity of the alloys (Ref. 3). In the present paper, the authors give the results of investigations made by applying the electrolytic method in a two-layer bath (Ref. 6). The lower layer of the bath consisted of a hydrochloric solution of manganese- and bismuth chloride. The solution contained ammonium chloride (25 9/1) and urea (30 g11). The upper layer consisted of a 0.2-0.7% solution of oleic Card 1/3 84673 Electrolytic Method of Producing the Highly S/020/60/135/001/026/030 Disperse Intermetallic Compound MnBi B016/BO67 acid in xylene. Fig. 1 shows the MnBi content in the cathode deposit as a function of the atomic ratio of the components in the electrolyte. Fig. 2 shows the dependence of this content on the current density. With the same current density, the ratio manganese : bismuth in the highly dis- perse cathode alloy deposit of these metals is smaller than in the cor- responding electrolytes. The disperse cathode manganese-bismuth deposit was subjected to magnetic separation. In this connection, a small amount of ferromagnetic fraction was obtained. The presence of glycerin in the electrolytic bath raised the yield in this fraction (see Table 1), especial- ly when the atomic ratio manganese : bismuth in the electrolyte was 85 : 15. This ratio was then 1 : 1 in the cathode deposit. Table 2 shows the results of the X-ray analysis. They indicate that the magnetic frac- tion of the disperse cathode MnBi deposit consists of metallic Bi. of the y-modification of manganese,and of the intermetallic MnBi compound. There are I figure, 2 tables, and 7 references: 4 Soviet, 2 German, and 1 French. ASSOCIATIONt Institut obshchey i neorganicheskoy khimii Akademii nauk USSR (Institute of General and Inorganic Chemistry of the Card 2/3 Academy of Sciences, UkrSSR) 8h673 Electrolytic Method of Producing the Highly S/020/60/135/001/026/030 Disperse Intermetallic Compound MnBi B016/BO67 PRESENTED: July 18, 1960, by A. N. Frumkin, Academician SUBMITTED: June 9, 1960 Card 3/3 .. 'BUSHIN, V.i.YEMMV, A. SuW,astione by finishers of the Cberepovets Trust for the Construction of Metallurgical Plants . Stroital I no.11: 18-20 N '59. (MIR4 13:3) 1. GlavMry inzhanar stroitelinogo upravleniya Spetastray trenta. Cherepovotemetallurgetroy (for Bushin). 2. Glavnvy inzhener upravlantya Montanb2hilatroy (for Yefremov). (Building--Tools and implements) v 4 BUSKIN, V., Inob.; TIMMY, A., inzh. Precast concrete porches with mosaiclike surfaces. Zhil.stroi. no.12:16 159. (MIRA 1)-.4) (Porches) Ij - BUSHIN, V.; Y]CMMOV, A.;STOUMOV, V.. insh. Using assembly-11ne methods in building large-panel houses. Stroitell no.12:7,10-11 D 159- (MIRA 13:3) 1. GlavzW inxhener upravleniya Spetsetroy (for Bugbin). 2. GlavzWy insbaner upravlaniya Montazhzhilatroy (for Yefremov). 3. Treat Cherepovetematallurgetroy, Cherepovate, Vologodakaya, oblast' (for Stounov). (Ansembly-line methods) (Leningrad--Apartment houses) BUSM, V-V-; UrREMOV, A-P-; STOUMOV, V.K.; YOKOLAYEV, G.I., red. CLarge-panel housing construction; practices of the "Cherepo- vetametallurgatrol" Trust] Krupnopanellnoe domostroonie; iz opyta raboty tresta "Cherepovetsmetallurgetroi." Vologda, Vologodskoe knizhnoe izd-vo, 1959. 39 P. (MIRA 13:12) (Apartment houses) (Precast concrete construction) "I 3/-137/62/000/001/DC4/237 A060/A101 AUTHORS: Natanson,.E. M.., Bushin, V. V., Shevtsova, A. F. TQTIY&. Thermal-reduction method,for obtaining intermetallio compounds on manganese base PERIODICAL- Referatimayy zhurnal, Metallurgiya, no. 1, 1962, 41, abstract IG314 .'(4'Poroshk. metallurgiya", 1961, no6 3, 29-34, English summary). TEXT.; A study was made of the conditions~for,reduoing Bi oxide by. metallic Mn at various ratios.of the oomponents.in the charge.. ,The maximum thermal-affect was obtained.at.the ratio B12O3 1 Mn --l : 5. At the same~ratio of.th,&,oompo- nents - one also observed -the maximum output of the magnetic fraction (MnBi):, :37.5% The characteristics of the MnBi compound obtained-by the.manganese thermal - . .; reduction method are investigated. Hc,turned out,to be equal-to.700 oersteds. There are 9 references. R. Andriyovskiy [Abstracterts note:- Complete translation].. Oard 1/1 NATANSON, E.M.; BDSHIN,-X!,V-; KOZACHEK, N.N. Cotditions for the formation of colloid p4l-ticles of intermetallic bompounds [with sumary in Bnglish]. Koll. zhur. 23 no-4:1+42-"? Jl-Ag 161. (I-ILRA 14: 8) 1. Institut obshchey i neorganichoskoy khimii Ali USSR, LabormUri7a kolloidnykh metallov, Kiyev. (Mang,anese-Bismuth alloys) (Colloids) 356r")7 S/020/62/143/001/022/030 B106/B138 AUTKORS: Natanson, E. M., Bushin, V. V., and Shevtsova, A. F. TITLE: A manganothermal method for producing the intermetallic compound manganese-bismuth PERIODICAL: Akademiya nauk SSSR. Doklady, v. 143, no. 1, 1962, 126 - 129 TEXT; The method involves the thermal reduction of bismuth oxide with highly disperse metallic manganese. Mixtures of pulverized bismuth oxide and manganese powder in various molar proportions (Bi 20 3:Mni from 2:1 to 1:8) were heated after careful mixing and sifting (200 mesh) in inert atmosphere until the reaction Bi 20 3 + 5Mn - 2MnBi + MnO + 134 kcal (1) took place. Typically metallothermal processes l1ke these are designated by the authors manganothermal method. The reaction was carried out in poorly meltable vessels 40 - 50 cm *~_high and 2 - 2.5 cm diameter. The apertures of these vessels were locked by thick-walled rubber tubes with oblique incisions which served as safety valves for the escape of gases during the reaction and isolated the reaction products from atmospheric oxygen. All experiments were carried out in an electric furnace at an Card 1/3 S/02 62/143/001/022/030 A manganothermal method for... Bio%ip initial temperature of 6000C and under identical conditions. The error in measureiaent was t150C. It is not possible in the example to calculate the rate of the reduction of bismuth oxide with metallic manganese, because the formation reaction of MnBi coincides with this reaction. The specific heat effects calculated for the reaction Bi 203 + 3AMn = 2Bi + 3MnO do not agree with the values obtained experimentally. This is due to the fact that 4 kcal/g mole of heat are liberated in the forma- tion of MnBi. The reaction products were subtly pulverized, siftedg and brought into a rotating magnetic field of a permanent magnet to determine the MnBi yield. The magnetic particles (MnBi) were separated from the nonmagnetic ones and weighed. It was not possible to separate chemically the manganese oxides from the magnetic fraction since the powder lost its magnetic properties when the reaction products were treated with organic acids. Obviously, manganese is also separated from the intermetallic compound when MnO is dissolved in organic acids. The optimum conditions ~or-the formation of YnBi are observed in mixtures with a molar ratio of Bi203;Mn - 1:5 because the yield of the magnetic fraction is a maximum in thesecases. Following Eq. (1), the MnBi yield should be 71,5~6 of the reaction products. The yield in practice is considerably lower, (37-5~) Card 2/3 A manganothermal method for... S/020/62/143/001/022/030 B106/B138 since other products (manganese oxides, pure bismuth, eutectic Bi-,MnBi) are formed during this reaction. The MnBi powders obtained by the manganothermal method showed the folbwing properties: microhardness - 148 kgf/Mm 2at a load of 50g (determined in a ITMT -3 (PMT-3) ) device. Thermal coefficient of electric resistance = 4.56-10-3. Constants of crystal lattice a - 4.26 2, c = 6.15 R. Coercive force - 700 oe. There are 2 figures, 2 tables, and 9 references: 7 Soviet and 2 non-Soviet. The reference to the English-language publication reads as follows: A. Goldmann, G. J. Post, J. Appl. Phys., 30, No. 4, 204 (1959). ASSOCIATION: Institut obshchey i neorganicheskoy khimii Akademii nauk USSR (Institute of General and Inorganic Chemistry of the Academy of Sciences UkrSSR) PRESENTED: August 3, 1961, by I. V. Tananayevp Academician SUBMITTEDs July 8, 1961 Card 3/3 AUTHORS: S/020/62/143/004/020/027 B101/B138 Bushin, V. V., Dumanskiy, I. A., and Dumanskiy, A. V., Corresponding-Member AS USSR TITLE: Electrical conductivity of a polyamide melt PERIODICAL: Akademiya nauk SSSR. Doklady, v. 143, no. 4, 1962, 894-895 TEXT: Results are given of the investigation of electrical conductivity of 0 capron polyamide at 230-290 C. The specific conductivity a was measured as a function of temperature (Fig. 1) and of holding time at constant tempera-. ture. The fusion was carried out in vacuum for 50 min, to eliminate moisture. Measurements were made in argon atmosphere. It was found that (1) gamma irradiation of solid capron has little effect on 'a-, (2) -clis not- linearlY d4ip6xfcT4nton holding time at a given temperature, it falls with soaking time. This is attributed to the evaporation of residual moisture and low-molecular compounds; (3) on heating, the *crof capron varies from dielectric (solid sample) to values characteristic of semiconductors. There are 2 figures. Card 11JL S/020/62/143/004/020/027 Electrical conductivity of a... B100138 ASSOCIATION: Institut obshohey i neorganicheekoy khimii Akademii nauk USSR (Institute of General and Inorganic Chemistry of the Academy of Sciences UkrSSR) SUBMITTED: November 30, 1961 Fig. 1. Specific conductivity, OF, of fused capron versus I/T. 41) non- irradiated sample activation energy 6E - 0-40 ev; (2) irradiqted with 302.5 krad y; M irradiated with 1.21 Mrad Card 2/3 5 107 8/183/63/000 0 V0031004 B1 01 /B'l 136 AUTHORS: -13ushin, V. V. , Dumanakiy, I. A. TITLE: Electrical conductivity of molten polycaprolactam -25 PERIODICAL. Khimicheakiy.e,volokna, no. 1, 1963, 23 TEXT: The conductivity of polyoaprolactam (caprone) was measured between 230 and 2900C in argon atmosphere. Results: (1) The conductivity of polyeaprolactam changes during heatingi probably due to evaporation of residual water and low-molecular degradation products. The'higher the temperature, the faster the conductivity approaches values characteristic of semiconductor polymers. (2) The temperature dependence of the conductivity is also similar to that of semiconductor polymers. (3) Gamma' irradiation of solid polyoaprolactam with 302-5 krad to 1.21 Mrad had little effect on the bondu6tivity of the melt. The activation energies of irradiated and of non-irradiated polycaprolactam were 0-35 - 0-32 ev and 0.40 ev. The small difference-'is due either to the small radiation dose or to the fact that high temperature affects the electrical properties of polycaprolactam more intensely than gammA radiation. There are 2 figures. Card 1/2 S/183/63/000/001/003/004 Electrical conductivity of molten ... B101/B186 ASSOCIATION: Instit ut obshchey i neorganicheakoy khimii AN USSR (Institute of General and Inorganic Chemistry AS.Uk.r8$R)z SUBMITTED: February 26, 1962 Card-2/2 VDOVENKO, I.D.; Corrosion resistance of indium-tin alloys in sulfuric acid. Ukr. khim; zhur. 29 no.11:1222-1223 163. (MIRA 16:12) 1. Institut obahchey i neorganicheskoy khimii All UkrSSR. BUSHIN, V.V., inzh,* Poliobing machine. Mekh. stroi. 20 no.10:21-22 0 163. (MW 16:10) ACC, NRt U C" 1257 J. V.; Duall-Lin, V. V.; Smotankina, id'. Pol:~rarization of siloxanos on a notal surface under tho influonco of a glow 3~'j: O`S: U:'-rain5ldy k*nimichaskiy z1hurnal, V. 32, no. 11 , 1966, 125'-11-2'~" TOPIC TAIU-3).- sl-o%ano, glow discharge, orpnosilicon compound, polynorization ~~e na-oor 6aals -w-ith the formation of nolyrrer films in an atlnos-z~hora of and on t h, e surfaco a a-, ,L- 4 r~,Z- -4'1 T*-cj -~,-er was ~3rod=eu Un6o' e i.-I co of a glow -L a '-av~-- a ~rrquenc- of 100, CDs at a vol~a~a of CCO-?'- !"'. --o ck - :,:ess of th E, '301--rm"Or. fiajr was found to inczoaso linoarly -w-Ith thu noir.-.orization t---o. 71 ~ho initial or-anosillicon cxrpounds anC poly-mor films Cotained and .rato analysis of the -polymor films show that the sti-actliro of the polymer is in- du-oan6ont of t.ie chain length in the iniuial organosilicon compounds. Orig. art. has",- figuras a.-,d I tc-'ble. 07/ SUEM, DATE: O-ju--.66/ CPLi REF- 005 Card J UDC' ?8.84 BUSHINA, A., karid,. biolog. nauk Wood pests of fruit trees. Zashch. rast. ot vred. i bol. 10 no.1g3l.-35 165. (MIRA 18z3) 1. Azerbaydzhanskiy Institut zaullichity rasteniy. Country : USSR Category: Forestry. Forest Cultures. Abs Jour: Mh-riol-,No 11, 1958, No 48789 Author : Dushina, Inst : Acad. Sci. Uzboh SSE Title Dynamics of t1le Growth of Hichory Dariii(, the Initial Period of Duvelopi-miA. OriG Pub: Dolcl. AN UzSSSR, 1957, No 7, 55-59 Abstract: This article cites cormparative data from studies on the dynattics of the growth of sccd1inC;s of Carya peemi, C. aquatica, C. cordiformis, C. ovata, C. alba and C. laciniosa in the 1jotanical Garden of the Acadow of Sciences of Uzbeh SSR. It is noted that durin[; t1ne first year of the stons Card 1/3 Country : USSR CateGary: Forestry. Fcrcst Cultures. ,I,bs Jour: R?-hDdo1-,N(, 11. 10587 No 48789 of hickory pla-Its covered by the study Groir very rapidly and that their grovth is corrActed in 7-10 days. In subsequent years, the growth of the seed- lin'~-s is drawn out cver a longer interval, With the exception of the pecan, the growth i.---crauent of the 2-year old scedlinGs does not attain a Great size. The C;rowth of the pecan seedlinrs ends later than in other sDecies - at the end of Sc-,)tu~.Icr - plaiiis its origin in localities wit'll, a which e3q long (6-8 mont-hs) vegetation period. In the case th of the pecan transplanted at : e --Ge of 3 years, the growth Incremient increases greatly in its 5th year in eomar--son with the specimens which wem not transplanted. In general, all scedlinGs Euid Card 2/3 country : USSR Category: Forestry. Forest Cultures. Abs Jour: RZhDiol-, No 11, 1958, No 48789 transplants of all Alickory varieties proditce a snall growth increment during the first 3-4 years. This increment --increases in subsequent years. With the exception of the pecan, the Growth of the hichory seedlinas ,~nd tr--.ispl---its proceeds very slowly during the f~-:rst 4-5 years. -- L.V. NL;s;.,,Clc)v K Cr~rd 3/3 ,r- of Bj7F:~rTj'jl A.I., Cand Bio Sci --(difs) 11 Biology of initial :7,z- certnin -,pecies of f:enus Cnryn Nutut,' and bioloCy of and fertility of tlll>~" tx carya pf-c".'n T!-s""kent, 197" u u e nu 6 lp, pp Sci UZS5R. BOtjL!nic,-l cnrdcn~. 200 co-~;ies VL,20-5B, 95) -33- BU HINEULI, A. [Buschinelli A.] P.-l- " . ~ - Y Experiments on vegetative hybridization in birds. Selskostop nauka (2] no. 2: 261-264 163. 1. Faculdade de Filosofia, Ciencias a Letras de Rio Claro, S. P. Brazil. BUSH I N OV , M. A. Improving SPLU and DK veneer cutting machines. Der.prom.4 nn-7: 25 J1'55- (MIRA 8:10) 1. Spichechnaya fabrika "Mayakl (Veneers and veneering) BUSHINSK&YA, A.11, "Hanual for the medical personnel In children's homes;" a collect- Ion. Podiatriia no.2:86-87 Mr-Ap '55. OILRA 8:8) (Or-pbane and orphanages) (Children--Care and hygiene) BUSHINSKAYA, A. V., GULTIN, 1. V,., y~jtjj,%p4t)Vj~, V. p. mi(I KUPPLIL, V. K. "Electrolytic Production of Lead by Electrolytes of Fused Salts" N Gentsvetnet -rePOrt submitted at a confereme on nm metboft of lesd prodwtion from comentmtes., Gintsvetmet (State Inst. Non-perroug Met&Uurgy)., Mosem 22_25 june 1956. (for ent:Lre conf. see card for IJM., V. F.) BUSHINISKIM'" L V .-- )-~ ~, 0 -- New type HIM machine for measuring stiff leather. Ko-.I-,.-obuv. prom. 7 no.6:24-25 Je 165. (YJRA 18-8) BUSHINSKIY, G.I., doktor geol.-mineral. nauk Symposium on bauxites, oxides and hydro-oxides of -aluminum. Vest. AN SSSR 34 no.5:127-129 MT 164. (MIRA 17:6) 6 0 0 W vw_,~~ IS W, - Im-K T"IPO to M v 111 31 11 11 31 a O 1- L N 0 it m IS w it to It 't 10 It 12 1 It n 1 . - ki" - 03 ' 1--i-i 00 A No s of the westem fe"Wes 01 the pboqh~dtt . a]. ssw e 9. N,).'-'. If, LB~#GAif. Ms- regiou. t_ 0& , 1jits slumed that till! 1,411,1 1.11-1111.)MV ee -mla ... tile wr%tcttl . . f - WA,Wl it ~X)j..C*CLh.Cmj.', ,11,1 tot k photolulaost mdm cha,. DIA11C 09 of a A 00 00 00 66 1.00 q 0 0 ;-Of ON t:o 0 00 00 17- a 04 01 of a AID n 0 0 0 0 6 : : : : IS 10 a 14 0 p ; " 1, It a 00 0 00 : : : : : oi: 0 a 0 o 90 0 a 0 0 : . : : e 0 of of at I list to v"1luljuul61?""mj 24 is 26 MIJ SAD ld V An&, .1 4jol &II16i Ait r . 9 0 a A" 11 1 1 L __, il-.---D-~,D-(). ~, E- --- ------- - ------------ .1 i- & 0 Deterinial"s Wit And anhydrilp, 6, M01111411. ik.S(11135). -Thc ptesetur "I gypmIsti A1141 snlmltit~ ill their 12milix. twil 1W delveled Ill. optival 111call.. The of 'ZI oI ppstitu 6 IMOS it) I.M(r) and of atiliOntr 1.613.14. while the dival,le irfractim, knwamu"t with ai~ Herck curupens2tsm) I, 0.01.A.07 Ir gylmiam and OM:17 for tbc anhydritc. A. A. It-litlinck zo 0 W-, Coo a alas roe xo* t's 0 too Allm-!LLA SETALLItillr~tCAL LITCRAIVRE CLASSIFICAYMN We 0 Z -&W ci;4 ------ Sk 0 T u a0 so N a K ft rt it or W n t 000 0 je0 00 0 goo*** 0(a 0 to o 9 30 11 u U 4 It 10 11 it )INDMAJOR)l H v a to j: Al It ju It IV 0-4v 4T--4 J. A x r a 1. AA N V. It It _7 0 0 Ggopb of flualits to oodlots" depootift. G. 1. h 1 a . 1 tit l(i. mat Itimbffilkil. Pull, atad, it i. 11, R. S~ S., ( g*f,.v4r. t4d. 1036, 77.*, VI; Allf'"ah't Ah.1mill 7.4 A I-NA14,11, 14 Or dilmlir slut woNkit. fit lu voith d,4,mW%h' -1 O IL ll. - lmd'i to 111c . if , J N It J. in 01ii,11 4 00 ' A. F ppid. ffoln wit 'A fttt:v W . f A 111:1011.1ft" at t cvi.jrlt,~ li'll Its Mr. 11-T 1% 111 04 -00 L A ANIALLURrKAL L1194411141 C%A%tWKAll" tie 0 flolls d6( 1 4 l u a AV IQ " Al U ft if IS It' l KLO 11 1 %a 0 0 0 0 0 0 0 0 0 0 0 0 0 0 * a 0 0 0 0 0 0 0 04 0 0 0 0 0 0 0 f 0 0 0 0 is __J1_ LIL 14.1 it AA H CC W A A. A_ 11-111-17 1-IN a 1 00 06 ir &4d some WI 491 dw seasoll of -00 " 10 r 7B 1216 vy8ft its. . L UWASUL DAW. 602 Joe. Sod. g'W '14''- No, 2, IWSO -00 (is Fmwh 1111-0)(19M.-The phamphositro occupy an am WWW" the rim" vyAlks, Kam and SYN44 at off) tatitfade IW* N. Imllitude M' R. Tlw phovItsuc im. terisil omm as conurtiorts and nodules in a 4-in. bed (it alautoo:itic nods. The order of formation is- (1) cWtic o * . ! " Muttrill WW Mg. rcmabo. (2) aranular atsucactite. (3) amorphous and MlcrocrYst. Phosphate. (4) cty-st. phos. phate with radial structure, (5) Pyrite and pooibly ff 00 a avikes. Secondary products frarn weathering am S". s=, vivianite sod strcrigite. It Is believed that the rog of .3 wnurpbous phosphate was pptd. from ses water. Analy. set of phosphate rock and ests. of tonnage am given. got R. If. Owkwith get, 06 see 0 0 Igoe A S a - IA NVIALLONCAL LMNAINN CLUSIPICAYMN lk T saaw .11 041 as( OJ4411 awt 400-1 at 7 4 saw" 0 U 5 AV 0 ui; is ;1,4"' 1 ad 0 a 0 1 IN a I A 4 0 9 * 0 0 0 0 *Is * 010 0 a 0 0 0 a 0 0 0 0 0 00000 00 0 00 0 0 0 0 00 0 * 0 & 01* go o 0 4 0 e 0 0 0 a 1:00 w-'w w- - - - - 9 14 A 7 :1 1 1 I 7 7 7 A it 41 f G 9 3 f. Q J.- 1 -6 It P . 1 ' as 0 at I l 0 1 at allietali'I11% 1-vilmitit'l I,- If;. so gril-in If liar Fg,,Io% K," 00 00 90 -00 L- A il. :': 00 00 0 4 of 00 4r ... .... I ..... go 60 & 0 00 -00 00 00 so .00 & ~i g g , , 00 3 - '06 00 1 . so 400 v 0 till It'lVal (IMIfItAllch so 00 'it a vk ~ 0 an Is -A I I ~.I` .1 a- 0 0 0 0 0 0 0 0 0 0 0 0 0 0 9 0 WO 0 0 a a 0 a 0 0 a 0 0 0 0 0 0 0 0 00 0 0 0 0 im 4 010 0 4 0 0 0 0 0 0 0 0 0 0 im to 0 a 0 0 0 0 0 0 0 0 0 0 0 0 _41-6 0 0 0 0 0 0 0 0 * 0 0 0 0 0 0 * 0 a 0 0 0 0 0 0 0 * Is 0 0 0 0 0 0 0 0 0 * o a I u CY X it u u is III v Is X~ D IF r 19 X L A 0 PQ R S I IN u T1 a * a . j Z *, MTO IS o1! , 00 so, 00 68- qw[ 1~ 1 1 00 so-, - 1.. 1, 1- ... ." - ---t . IV., I.- .1,1 m mu'l.,111 III!" II.-Ilk"111"I p- 0111I., ~ 1,111111111111 1 9 q1114111114d 41111-111-414V do 11110 Aqawjlkljll,l L T-m, 011 .1 "'.41 1 11 10 Im IV I I i. w .1 R A, of F1 I, ft I, a is 0 0 0 Ime 0 0 A-9 ----a 000000000000 is it a 71a Dion jor x I it 4 " Is I Is IV it -1 M X ~; 1 9191, 00 A fit A" .1'4! 661,111 002 00 The phosphocits lade# of r Cri-taivous- of- the Euro - Pean Upr A. Traxi. Sqi. 00 "A of U. S, S. R. G. Ood t1list?i 140, 87-03; Khim. Rrfetal. Zhijr. 1940, No. 1, 39-The individual phosphorites of the Upper Crelaccotts hurium :*0 are described. The conditions fur the formation of phits. Mr 0 of a pharitso of all hotizons an. (1) The phosphorites wt-rc dr- 0013 ~1, ~jgrd in sca rescrVoirs with a normal (or nearly normal I 0043 WX content and not contaminated with 110S. (1-1) 71c 0 0 laeposition of phosphorites took place in the reservoirs with 00 060 a slow accumulation of the sediments. (3) The m&%. itc- cumu 00" Jatlov of phosphates took place during the tranlor- zoo mation of the windy facks into the lime facirs. (4) The 002 plicsphorltes were deposited at depths from 50 to 3W In, In the study of pbospharites It Is necessary to cort5ldcr fit~t 09 the smaller sea deposits formed from lbefflow am-umulation 0 0 of the ppts. (the shallow-water fades). This can take place not only on platfonni, but also in gcosynclinal re- sioni. W. It. flenn 1::: 11109 !Z109 1-00 A S IA. I. a MAIIALLIARCK41. LITE14TURE CLASWICATION ire 0 CL s4no" %.lava 411 C"I 09t U U IV go it. I FW 0 N 1 ir so 0 'T a 3 V dAQ 0 It It it It It a, It It KOW A, 1 1.1 An I 0 11 Of 0 0 0 0 0 0 a 0 0 *10 0 of a 0 * * 0 0 of a 0 & a 0 0 0 * 0! 00:00 00 00 00 00 0 of 0a 09 01 0 a- 0- a- 0 a 0 0 0 0 0 0 a 0 0 Of Of 0 W - W ~ -- w- ~ # 41 11 u It W it Is it of flavalmAllm -11-9- v It -0 I W I --? m -AMX -AWL -A. "--j A A 0 j k I v varplailt, ..11f. iocl t41 o0. 09C 0 al Anuank- G. 1. -00 : 0 ced. Sci. U-BA-9- IM is of We rocks uml ;Z~t 0 : en 3B, UW-~ba mountams uld the Of the orded and =00 a of the zindAwin IKOW we roc L S. T. discummed. coo roe )Ilse is* 0 1 5 L A A LLLIPICKAL LITINATLOR CLAIWOCATION It- I 00 U90 ' L !, WOO Islas') wit *qv do! millslGht bliall it, 00 0 u Is As 10 0 tg a 0 a W a IN a o9 It a 1 11 1 IA KO (I I KA 0 0 * 0 0 0 0 w w tlid$,l i s 11111I)IJ4111611 0 It a R*3111 all U&I MAD by mam &1 IL 1 1 1 1 Y 4141 616CO A -2 -- It-4-" j A- A. a -A J - A . ." 4 I " -tqa? AkV'_lV_q�PL1F6 ___ . r-l-k". -, P&OPINT.11, .09. *G.x B. a-dkolum of Ph-0101101MIML G1. fluschinsk, Arad. Sri. U"?SS 19 -Pl d 1 06 c .. . fen . 411,47. 127 11 1 hnsphOrit" M twsed clasSifiCatitin ,I F . 1 ) are n Mcnet'UrnciPle. Is PrvFxwd. MiLrine '"O chemi' di' ift"e 06 a tinentai Y PP and organornous (1) Con. l c divided into an ogen.u, M Matic, metall0mlitic. and hydrothernw Orgatlogrnous~metaso_ i t W n o residual, redeposl orked (1) are divided ted. and metamor hi,, , divi i 1 s o , p ( ). Sorne of these hA. ns are so bdkided. 1':x&mP"" of O"h 4 - t " 'r 7, are tqi% 'ticA Of each tvW rn anti the are "irnpa" C 1j 11 . . . . coo sew COO 001 go 0 00 4p COO I j : go tjoe A%* LA .11ALLURrICAL UUMAT01 CLAWFICATION 12- w3av %alcaj -A. 1- oat )I cat ctm %.- u 0 AT 03 TV tv IT it 11, a, It It it 11 .1 1.7.K.Aft Li a Od 0 4 a I w 14 5 ill a 3 1 v d.00 0 0 0 0 0 0 a 0 a 0 0-6 4 a a 0 6 0 0 a 0 0 0 0 0 ei~ The conditi5nn In the famatIon of alderito, vivianites, aid- 11111y, I-.% thr rtli bop 0 Wh1tv Rusbift, 2)ONO.-TIm sails In the upper reachc3 are arid. Dr&in- age H:O haNing pli 4.G and higher le.3ebes glacU dep-mts cong. Ca, Fe, Mn, and P. In the natural flow the saint. come In contact with spring 1110 of the lowland bogq whrre p1l vnlim we In the range 7-8. Vivianhe rind siderite ltmviform apil 7.2-7.4nnd chalk tit p11 T.".O. Brown .Iron ore deposits rciult frorn oxicltiinu of %lderitc. Sever-&I beds of rbodmhrosite were found at the base of it vivianite -hrd-- Murray Stnk-us ~ V) - Vf1N Mordowts in jurazatc, Crtlaceous. and Palaeozoic marine sadmilate. C., 1. It to% ~1~11 %kol; Poklody Akad. Nauk NA - . - cuprtru (Zjftjki S.M. 73, 12714(1 1 . C. Mineral. Obxkthrjttj 69, A7(1140)) ifescrilKA analt-olp. it, ,awittoum (of the Ka.&m horizons a% a nrw hor-mation. ana tat" (V.A. 40~ 411=51) mordenito: and %iotilAr mitteralt of I fit- zvolite poup (e.g. laumontile) in marine %etlinirrus of Ill.- we-fertl tIite of the Ura!%. 11-111nule cry%lalt (ouly I if, III st, (A thew in nvraI% occur pAtticulatly in (fir lower Tutout.m *of the Bry2n* chalks, together with hydrontic-a and kaolm- lie. little quartz. chalmlony. g6uronitc. cit. Mordmitt- shows prismatic (cormi., with to 1.487-, the birefringoirr i, not perceptible. A chern. analy%is it given. The witle distribulion of mordenite in srflimrnl~ in all parts of ife Ru%%i:m Platform it particularly rrIIl.&rUA)Ir. Morlit-lo1q. lout Wim Ix-i mioakc,, for (CI&I.r. "t, --fl. ~ilfl ormI I- very comoncls ill the cements. but .11 high Illiplifica- tions thr ch~tnicttTistieni(irtirnitelirisnisarr m%ily identifitil The abq. amIq. ofmortlenite may vary from a frw % to 2(1' inat. Mortlenite wai never observfti in fro,th-walim m-11- mt-nt,; it it a typical dret)-ra marine prooinct. ill a late %late of thr diagelortit. A prarfiral ur of the mordenite. joerhtp, at a Itate-exchange material, I% not yet found Itecau4c of the extremely fine crystal size of the mineral. W. Fitorl BUSHINSKIY, G.I. ~: - (Apatite, phosphorite, vivianite: calcium phosphatea, their mineralog7, geology, origin, and methods of studying theml Apatit, foaforit, vivi- anit; foafaty kalltaiia, ikh mineraloglia, geologila, proiakhozhdania i sposoby izucheniia. Moskva, Akad. nauk, 1952. (MLRA 7:2) (Calcium phosphates) Busli'll"SYM G. 1. B=n=IY, G.I., doktor geologo-mineralogichookikh nauk. ". [origin, of mineralej Proinkhozhdonle polesnykh lskopaemykh. Mosk7a, GoB. izd-vo takhniko-teoratichaskoi'lit-rv, 1953. 61 p. (Nauchno-populiexnaia bibliotaka, no.63) (MM 7:5) (Mineraloa) 3159 BUSHINSKIY, G. I. Pmiskhozhdenie poleziyvkqriga. laggosizdag. 1954. 67 a. s. ill. I Kart. 20 sm (Nauch.-popul. 6-Ka. 7.000 ekz. 95k.-Na Latysh. yaz.-(54-56766) 553.04 BIUSHI':~KIY3 , T. 165 Litologiva !.Ielrvvlh 011o7h-niy Dnepro--sko~,Oorietskoy Upp-diny. "., tzd-vo Akad. "IBuk. 't-83SH, 1954 '~O~) 5- 3 ill- I Kert. 26 Sm. (Akad. :7puk- SSSR. Trudy In-ta Geol. N~wuk. V~,,,?- 1;6. Geo3. Seriya (no. 67)). 1.011 ~',kz. 11 r. 51) F.--~ibliogr: 3. 295--,)5-(54-14!l!zb) 551.76'(47)+(r)l,",.I) 30: Knizhnsya, L,~topis, Vol. 1, 1955 S/:~ 6?. Z~ Scientific Organization - Conferences Card 1/1 Pub. 116 - 18/19 Authors 1 Bushinskiy. G. I. Title I Conference on the geology of mineral fertilizers (agricultural ores) FeriocUeal Izv. AN SSSR. Ser. geol. 5, 176 178, Sep Oct 1954 -Abstract An account is given of a conference attended by 228 persons and hold from the 25th to the 29th of May 1954 in Moscow under the auspices of the Department of Geological and Geographic Sciences of the Acadearj of Sciences of the USSR, for the purpose of collecting all.available information relative to the country's resources in mineral fertili%er (agricultural ores), End finding ways of increasing them for the benefit of agriculture. Nineteen reports were read and discussed. Institution: Submitted: June 26 1954 -014 USSR/A C tu! - Minerals Card 1/1 Pub. 14 - 4/26 Authors : Bushinskiy, G. I., Dr. of Geol. Mineral. So. Title : A!7ricultural ores Periodical Vest. AN SSSR 12, 30-Al Doe 1954 Abstract Geological data on various agricultural ores, used in the manufactule 01 synthetic fertilizers, are-presented. Institution :8vbmitied UMIGOology Petrography Card Autbors I Bushinskly, Go and Frank-Kamenotskiy., V. A. Title I Hydraulic activity and roentganometric characteristic of an opalescent substance of tripolite and diatomite earths Perloddca3. i Dokl. AV SSSR, 96, Ed. 4, 817 - 820, June 1954 Abstract 60 The hydraulic activity of tripolite and diatomite earths was determined by adding calcium oxide, The diatomites have a lower hydraulic activity, In spite of their high opal content. The chemical composition of the Investigated trip- olite and diatomite earths is given in table. Nino refor- enees. Tables. Institution : ... Presented by: Academician N. M. Strakhov, March 19, 1954 N.M., akademik, glavny redaktoi; SIPOZOMM, D.G., otvetstvannyy redaktor; XOGOT, G.I., redaktor; IRMYVA, N.A., tekhnicheskiy redLktor. Litholegy of Orstaoeous deposits ofthe Dnieper-Donets Lowland. Trudy Inst.geol.nauk no. 156!3-307 154. (MIAL 8:2) (Dnieper Lowland--"ology,-Stratigraphic)(Donsto Bas In- Geology. Stratigraphic) BU Meeting on the origin of bsnixites. Izv.AN SSSR. Ser.geol.20 no.4:174-175 Jl-Ag'55. (MLRA 8: 10) (Bauxite) A 1~11V'SHT ~j ns/Mnerals Conferences Card 1/1 Pub. 12-4 -23/32 Authors s Bushinskiy, G. I., Dr. of Geol. Mineral. So. Title i Development of a theory on the origin of bauxites Periodi'cel i vest.. gj ss SR 25/6, 101-102, June 1955 Abstract Conference was hold atthb Geological-Geographical Sciences Institution of the Academy of Sciences., USSR where the development of a theory regarding the genesis of bauxite in ores was announced and discussed, Bauxite is an i-raportant raw material in.the manufacture of Al) and electrocorandum$ it is used as a metallurgical flux, and in the mant0tacture of fast hardening cement, high-quality refractories and absorbents. Institution Submitted *too* eda DOLGOPOLOV, N.N.; RUNNY, P.L.. redaktor; MA= _ ,~.L, r ktor; GIMMLI,FARB. B.M., redaktor; IVANOV, A.A'.. ra6'kU'i~,I'SMKHoV' N.M., akademik, otvatstvannyy radaktor; 1FISENKO, I.A., redaktor; ASTROV, A.V., redaktor izdatelistva; AU2AN, N.P., takhnichaskiy redaktor [Problems in the geology of agronomic minerals) Vbprosy geologii agronomichookikh rud. Moskva, 1956. 239 p.0 (KIRA 9:11) 1. Akademiya nauk SSSR.Otdelenive geologo-geograficheskikh nauk (Geology, Xcohomic) (FartAlizers and manures) BUSHINSKIY, G.I. A.D.Arkhangellokiilo work In litholopj. lEv.AN S=.8ar.geol.21 no.8:61-69 Ag 156. (MLRA 9:11) 1. Geologicheskiy institut Akademii nauk SMV Moskva. (Arkhangellskii, Andrei Dmitrievich, 1879-1940) Oil BUSHINSKIY, G.I. 'e"', Diagenesis in relation to the genesis of refractor7 clays, sodimentary rion ores, and bauxites. Biul. MOIP. Otd.geol. 31 no-15:125-126 S-0 156. (MLRA 10:3) (Bauxite) VVIAi"I 1131 X 1- dif" t-u ;2:~P= &ad 4is. As a hutcaiw. ofthe CDI emient tht cakid. and Jetd. d5. iholW 2 r0ld dj~&~ 7Xitb jnCrCP.SrMF C04, the Wtirularlv lovy e3cptl. da. indL-ate stmctural drJects iD whLIc F LA nea.:~ Vn -4 C C, t, Y" '-ZE-LENOV, Konstantivi Konstantinovich; KTA~Oi, N.M., glavnyy red.; ~USHINSKIY, otv. red.; ILI IRA, N.S., red'. Jid-va; POLYAKOVA, T.VP--,-1-,6TC red. [Lithology of lower Cambrian deposits in the northern slope of the Aldan massif] Idtologlia nizhnakembriiskikh otlozhenii severnoeo sklona Aldanskogo massiva. Moskva. Izd-vo Akad. nauk SSSR, 1957. 121 p. (Akademiia nauk SSSR. Geologicheakii institut. Trudy No.8). (Aldan Highland--Rocks, 6edimentary) (MMA 11:1) 1-1 1 j-" -s K; Y, Y-, STRAKHOV, N.H., akedemik, otvetstvennyy red.; BUSHIH$UY.__Q ,,, doktor geol.-min.nauk, red.; PUSTOVAIA)V, L.V., red.; MABAKOV, A.Y., kand. geol.-min.nauk, red.; KHVOROVA, I.V., doktor geol.-min.nauk: BABDITSEV, II.I., red. izd-ve; KOIDSKOVA, H.I., red.izd-ve; INTIN, H.L., red.izd-va; KRYNOCHKIHA, X.V., tekhn.red. (Methods for studying sedimentary rocks] Metody izucheniia osadoch- nykh porod. MoBkvs, Gos. nauchno-tekhn.izd-vo lit-ry po geol. i okhrane nedr. Vol.2. 1957. 563 P. (MIRA 11:3) 1. Akademiya nauk SSSR, Geologicheakiy institut. 2. Cblen- korrespondent AN SSSR (for Fustovalov) (Rocks, Sedimentary) STRAKHOV. N.H., akademik, otvetstvannyy red.; 1~~IISK~IYI_Lt" doktor gool-mineral.nauk, red,;PUSTOYALOV, L.V.; KHABAKOV, A.V., kand. geol.-mineral.nauk, red.; KUOROVA, I.Y., doktor geol.-mineral. nauk, red.; ENTIN, M.L., red,izd-va; KRYIIOCHKIIIA, K.V., tekhn.red. [Methods of studying sedimentary rocks] Metody lEucheniia oBadoch- nykh porod. Moskva, GoB.nsimhno-tekhn.izd-vo lit-r7 po geol. t okhrane nedr. Vol.l. 1957. 610 p. (MMA 11:2) 1. Akademiya nauk SSSR. Geologicheskiy institut. 2. Chlen-korrespon- dent Akademii nauk SSSR (for Pustovalov) (Rocks. Sedimentary) AUTHORt Bushinskiy, G.I. 11-9-12114 TITLE: Some Explanations to Critical Notes of A.K. Gladkovskiy (Nekotoryye razlyasneniya k kriticheakim zamechaniyam A.K. Gladkovskogo) PIRIODICALt Izvestiya Akademii N~uk SSSR, Seriya Goologicheskaya, 1957, # 9, P 95-96 (USSR) AISTRAM The author answers some critioal notes of Gladkovskiy in con- nection with Bushin kiy's paper "Lithological Works of A.D. Arkhangellskiy" (Re;.' 2). Some of the Gladkovskiyls remarks the author recognizes as correct, but disagrees with others. He paints out weak points in Gladkovakiy's argumentation and re- capitulates his own viewpoint as foll1owat modern factual data as to genesis of bauxites have shown some inaccuracies of both theories developed by Arkhangeltakiy and Malyavklnl but the first theory, devised by Arkhangel'Bkiy, proves to be more useful even up to the present time. There are 4 Slavic references. AVAILABLEt Library of Cont~reas Card 1/1 KRVOROVA, Irina Vasillyevna; STRAKILOV, N.M., akadAmik, glavnyy red.; BUSHINSKIY1- G.1.,Joktor geol.-min.nauk, otv. red.; CHKPIKOVA, -f.-M. re~.iz_d_-__va; IJOVICHKOVA, N.D., tekhn.red. [Atlas of carbonate rocks occuring In the middle and upper Carboniferous of the Russian Platform] Atlas karbonatnykh porod arednego I verkhmego karbona Ru9skoi platformy. Moskva, Izd-vo Akad.nauk SSSR, 1958. 169 p. (MIRk 12:1) (Russian Platform--Carbonates (Mineralogy)) SEIVETSOV, Mikhail Sergeyevich; BUSHINSKIY, G.I., red.; SMNOVA, N.Y., red.izd-va; [Petrography of Badimentary rocks] Petrografiia osadochnykh porod. Izd.3., parer. Koskva, Goa.nauchno-tekhn.izd-vo lit-ry po geol. i okhrane nedr, 1958, 415 p. (MIRA 12:3) 1. Moakovskly goologorezvedochnyy i-natitut im. Sergo Ordzhonikidze (for Shvetsov). (Rocks, Sedimentary) .3(55 15(6) PHASE I BOOK EXPIDITATION SOV/1254 Akademiya nauk SSSR. Otdeleniye geologo-geograficheskikh naulc Boksity, ikh mineralogiya i genezis (Mineralogy and Origin of BmLydtes) Moscow, izd-vo AN sssR, 1958. 488 p. 2,209 copies printed. Compiler: Dolgopolov, 17.N,; Chief.Ed.: Strakhov, N.M.,, Academician; Resp. Ed.: Bushinskiy, G,I.; Ed. of Publishing House: Nosov, G.I.; Tech. Ed.: Polenova, T.P. PURPOSE: The book is intended for scientists working in geolou and associated fields, and managers of industrial and engineering concerns* COVERAGE: This collection of articles by various authors on the mineralogy and geochemistry of bauxites appeared as a result of a 1955 conference on the origin of bauxite (Chairman, Academician N.M. Stakhov). The c:)nfer=ce dis- cussed the genetic theories propounded by various scientists, underlining the weakness of L.S. Berg's biochemical theory and the hydrothermal theories developed by some French scientists.. The majority of Soviet geologists appear to-be in accord with the sedimentary origin theory. The book discusses problems on the origin of bEwxite and describes some deposits found in the USSR. Each article is accompanied by Soviet and other references, photographs, diagrarn , tables and maps. Card 1/14 Mineralogy and Origin of Bauxites SOV/1254 TAKE OF CONEMNS: Foreword PART I. MINERATM OF BAUXITW Mineralogy of Sedimentary Bauxites (S.I. Beneslavskiy) 7 1. History of mineralogical investigations of bauxites 7 2. Alumina-contedning minerals 8 3. Silica in bauxites 21 4. Iron-containing minerals 23 5. Calcium in bauxites 26 6. Magnesium in bauxites 28 7. Titanium.minerals 30 8. Sulphur minerals 33 9. Phosphate minerals 35 10. Sodium and potassium in bauxites 36 11. Trace elements in bauxites 37 12. "Lode facies" in bauxites 42 13. Some problems of mineral formation in bauxites 44 14. Genetic classification of sedimentary bauxite minerals 48 Card 2/14 Mineralogy and Origin of Bauxites SOV/1254 Bibliography 49 The Origin of Alumina-bearing Minerals in Bauxite (K.F. T6rentlyeva) 52 Bibliography 69 Mineral Composition, Origin and Metamorphism of Lmver Cretaceous Bauxites of the Eastern Slope of the Urals and the Targay Plains (A.K. Sharova and A.K. Gladkovskiy) 70 Bibliography PART II. GENERAL PROBIM ON THE ORIGIN OF BAUXITES 71 A.D. Arkhangellskiy's Theory on the Origin of Bauxites in the Light of Modern Science (G.I. Bushinskiy) 83 Bibliography 91 IlRegularities in the Distribution of Bauxite Deposits and Conditions Under Which They Were Formed"(Ya,& Goretskiy) L--- 93 C ard 3h4 Mineralogy and Origin of Bauxites SOV/1254 I. Regularities in the distribution of bauxite deposits 93 1. World bauxite-bearing a;reas and their zoning 94 2. General patterns in the~distribution of bauxite deposits in the principal structural eleiaents of the earth's crust 99 II. Formation conditions of bauxite deposits Bibliography lo8 118 The Geochemistry of Aluminum, Titanium, Iron, and Silica Under the Effect Sulfate Weatheringlo(In Connection with Bauxite Origin)" (/(M.N. Yakovleva) 120 Introduction 1. Status of the problem I!. Methodology of investigation 121 124 III. The geochemistry of aluminum, titanium, iron and silica under sulfate weathering of base rocks in areas of pyritic deposits 125 Card 4/14 Mineralogy and Origin of Bauxites SOV/1254 1. Weatherita ci-ast 135 2. Ground waters in the sulfate weathering zone of base rocks 138 3. Surface waters 138 IV. Geochemistry of aluminum, titanium, iron, and silica in sulfate- boggy weathering conditions 142 1. Alum-peat bog (weathered crust) 142 2. Ground and surface waters 150 V. Review of observations 154 Conclusion 157 Bibliography i6o I'Conditions of Bmncite Formation // (F 01. Pasova) 162 Bibliography 162 Genetic Types of Bauxites (G.I. Bushifiskiy) 176 1. Genetic classification of bm!xitea 176 Card 5/14 Mineralogy and Origin of Bauxites SOV/l2r-,4 II. Solution, transfer and precipitation of bauxite components on the earth's surface 177 III. Laterites and laterite-bauxites 185 1. Laterites and laterite-bauxites of India 185 2. Laterites and laterite-bauxites outside of India 192 3. Conclusions concerning laterites and laterite-bauxites 202 4. General characteristics of laterites and laterite-bauxites 206 .TV. Sedimentary bauxites 209 1. Arkansas bauxites 209 2. Jamaica and Haiti bauxites 213 3. Ural Devonian bauxites 220 Limestones, underlying bauxites, and the configuration of their roofs 222 Karst breccia and conglomea~gte 223 Red and gray bauxites 227 Some diagenetic and later alterations in bauxites 236 Brief history of the development of concepts concerning the origin of Devonian bauxites of the Urals 240 Patt&rn of the origin of the Devonian bauxites of the Urals 253 Card 6114 Mineralogy ana Origin of Bauxites SOV/1254 V. Indications in exploring bauxites 256 Bibliography 259 PART III. ORIGIN OF BAUXITE DEPOSITS Geology and Origin of Bokson Bauxites in Eastern Sayan,(N.S. Illina) 267 1. Geological cross section 267 2. Age of bauxite beds 270 3. Position of the deposits in the structure of Eastern Sayan 271 4. Tectonics of thq deposits 272 5. Appearance and composition of bauxites 274 6. Morphology of bauxite beds 275 7. Manifestations of bauxite in the vicinity of the deposits 278 8. Origin of bauxites 279 Lithology, formation conditions, and patterns in the distributioij of Bokson bauxites." (P.V. Orlova),/ 282 1. Litholog~cal features of Upper Proterozoic and Cambrian deposits 282 2. Type of ores, their structure, and chemical and mineral compositions 287 3. Indications in the distribution of high grade ore 291 Card 7/14 Mineralogy and Origin of Bauxites sov/1254 4. Conditions of bauxite formation 295 Bibliography 305 Origin of Devonian Bauxites of the Salair Ridge (M.P. NE%gorskiy) 306 1. Underlying limestones 3o6 2. Origin of the pre-ore relief in limestones 308 3. Morphology and composition of the ore horizon 309 4. Trace elements in bauxites 311 5. Facies changes in the ore horizon 311 6. Signs of terrigenous weathering of the Devonian 313 7. Overlying limestones 313 8. Origin of Devonian bauxites 315 Bibliography 318 Anciez;t. WeathereaLaterite Crust of the North-Onega, Bauxite Deposits (K.N. 'Trubina) 319 1. Ancient relief 319 Card 8/14 Mineralogy and Origin of Bauxites SOV/1254 2. Geological structure 321 3. Weathered crust of Proterozoic rocks 324 4. Weathered laterite crust ofUpper Devonian beds 328 5. Weathering stages in basic extrusive rocks 330 Bauxite Deposits of the Podmoskovnyy Basin" (K.N. Trubin.a) 335 Bibliography 34q Carpathian Bauxites and Their Origin'~ (A.A. Denisevich) 34-7 South Ukrainian Bauxites and Their Origin" (Yu. B. Bass) 351 lower Cretaceous Bauxites of the Eastern Slope of-tht! Urals and T 355 Lheir Origin " (N.A. Kaxtbavin) Bibliography 360 Regarding the Origin of Lower Cretaceous Bauxite Deposits in the Urals" (B.P. Krotov)j, 361 Card 9/14 Mineralogy and Origin of Bauxites SOV/1254 1. Variegated clays 363 2. Bauxite clays 363 3. Clayey bauxites 30`3 4. "Bean- shaped" or "pisolithic" bauxite 369 5. Origin of the Sokolov bauxite deposits 373 Bibliography 377 "Geology of the Sout~vestern Section of the Turgay Downwarp and Its Possibilities in Bauxite Miningli(Ye.P. Boytsova..~ B.M. Mikhaylova, N.K, Ovechkin) 378 1. Stratigraphic outline 378 1. Upper Proterozoic ana Carboniferous 378 2. Mesozoic weathered crust 379 3. Cretaceous deposits 381 4. Tertiary deposits 387 5. Quaternary deposits 3M II. Formation conditions and general features of bauxites 388 Card 10/34 Mineralogy and Origin of Bauxites SOV/1254- III. Recommendations for future exploratory work 390 Conclusions 392 Bibliography 392 v (A.N. Volkov~ 393 Kazakhstan Bauxites and Their Origin I. Stratigraphic position and characteristics of bauxite facies 393 1. Mugodzhary deposits 395 2. Upper-Tobol.deposits 396 3. Kushmurun deposits 397 4. Amangelldy deposits 39B 5. Akmolinsk deposits group 400 Il. Origin of Kazakhstan bauxites 402 1. Source of alumina 402 2. Character of alumina solutions and conditions of their migration 404 3. Composition of solutions 405 4. Precipitation conditions 407 Card .11/14 Mineralogy and Origin of Bauxites SOV/1254 5. Diagenetic processes 410 6. Epigenetic processes 412 7. Possibilities of another, non-chemical origin of Kazakhstan bauxites 413 Bibliography 414 Gibbsite Deposits in the Amangelldy Bauxite Mining District of Central Kazakhstan (B.A.. Tyurin) 416 1. Basic lineaments in the geological structure of the Amangelldy bauxite mining district 417 2. Brief description of bauxite and refractory clay deposits 422 3, Origin of bauxites .428 Conclusions 429 Bedding Conditions of Cenozoic Terrigenous Bauxites of the Western Slope of the Kazakhstan Uplands (N.A. Lisits)na) 431 1. Existing concepts of bedding conditions in baimite-bearingirocks 431 Card 12/14 Mineralogy and Origin of Bauxites SOV/1254 2. Position of bauxite-bearing rock in the structure of the Paleozoic basement' ' 432 3. Bedding conditions of bauxite-bearing rock and the morphology bauxite accunulating basins 439 Bibliography 439 Stratigraphic Position and Age of Bauxites in the Head Waters of the Ashi-Tar.ty-Turgay River in Kazakhstan (V.N. Rasimova) 440 Bibliography h-50 Variegated Sediments of the Salair Ridge (M.P. Nag~rskiy) 451 Bibliography 453 RegdrclAng the Stratigraphic Position and OrigiA of the Yenisey Ridge Bauxites (K.V. Bogolepov) 454 Card 13/14 ;4ineralogy abd Origin of Bauxites Bibliography SOV/1254 454 Data on the Bauxite-Bearing Possibilitibs of Yenisey Region .(Yu,A., Lavrushin and 'Ye.N. Shchukina) 462 Bibliography 1462 Mesozoic Bauxites of Central Asia (L.T. Konnov) -478 Resolution of the Conference on the Origin of Bauxites 483 AVAILABLE: Library of Congress Card 14/14 W./Mas 3-13-59 I BUSHINSKIY. G.J. Formation and distribution of bauxite deposits. Zakonom, razma polesn. iskop. 1:426-461. '58. . (MIRA 1213) l.Geologicheekl.v institut AN SSSR, (1huxits) STRAKHOV, Nikolay Mikhaylovich; ZAWNZON. Emma Solomonovna; GJAGOLNVA, Mariya Andreyevna; BUSHINSKIY. G.I., otv.red.; NOSOV, G.I., red.izd-va: RYLINA, [Studies in the geochemistry of upper Phleozoic sediments in humid zones; facies and geochemical researeh) Ocherki geokhimli verkhne- paleozoiskikh otlozhenil gumiduogo tipa; opyt fatsiallno-geokhilni- cheskogo issledovaniia. Moskva, Izd-vo Akad.nauk SSSR, 1959. 21',7 (Akademiia nauk SSSR. Geologicheskii Institut Trudy, no.23). (MIRA 12:11) (Sediments (Geology)) BUSHINSKIY, G.I. Critical review t-f the Soviet literature on bauxites published in 1955-1957. Biul.MOIP.Otd.geolo' 34 no.4:117-132 Jl-Ag 159. (HIRA 13:8) (Bibliography--Bauxite) LISITSYRA, Nadezhda Alskeandrovana; SRATSKIY, N.S, glavny7 red., akademik; BUSHINSKIY. Q.1., otv.rod.; ROMANOVA, L.A., red.izd.-va-, SA31TOV, A.. tekhn.red.; BRUSLAVSKAYA, L.Sh., tekhn.red. [Old weathered surface in the western Kazakh Hills) Drevniaia kora vyvetrivaniia zapadnoi chauti Kazakhokogo nagorlia. Moskva, Gos.nauchno-tekhnizd-vo lit-ry pa gornomu delu, 1960. 97 p. (Akademiia nauk SSSR. Geologichaskii institut. Trudy, no.11). (MIRA 13:6) (Kazakh Hills--Weathering) VRA OV, Nikolay Mikhaylovich;-XMSajRSKIY, G.I., otv.red.; NOSOV, G.I., red.izd-va; POLENOVA, T.P., tekhn.re-al. --- [Principles of the theory of lithogeneBis] Osnovy teorii lito- g6neZa. KOBkva, Izd-vo Akad.nauk SSSR. Vol.l. [Types of litho- genesis and their occurrences on the earth surface] Tipy lito- genaza i ikh razmeshchenie na poverkhnosti zemli. 1960. 209 p. (Petrology) (MIRA 13:9) p STRA OT, NikolBy Mikhaylovich; BUSMSKIT, G.I.. otv.red. [Bases of the theory of lithogenesis] Oanovy toorii litogeneza. Moskva, Izd-vo Akad.nauk SSSR. Tol.2. [Composition and di6tribu- tion of humid sediments] 2akonomrnosti sostava i razmeBhcheniia gumidnykh otlozhenii. 1960. 573 P. WRA 14:1) (Petrogenosis) BUSHINSKIY, G.I.; BOGOLYUBOVA, L.I. Concretions of phosphatized bauxites from the lower JuraBsic coal seam near Karpinsk in the Northern Urals. Izv.AN SSSR.Ser. geol. 25 no.1:49-55 Ja 16o. (MIRA 13:8) 1. Geologicheskiy institut -LI SSSR, 14oskva. (Karpinsk regioa--Bauxite) "'~BUSHMSKIY, G. I. "Geology of the Arkansas bauxite region" H.Gordon, J.I.Trac7, and M.W.31lia. Raviewed by G.I.Bushinakii. Izv. AN SSSR. Ser. geol. 25 no.4:llZ.rll5 Ap 160. (MIRA 13: 11) (Arkansas-Bauxite) (Gordou, M.) (Trach, ,T.I.) (Ellis, H.W.) - BUSHINSKIY, G.I. Stylolites. Izv. AN SSSR. Ser.geol. 26 no-8:39-;7 Ag '61. (PURA 14:,9) 1. Geologicheskiy institut AN SSSR, Moskva. (stylolites) BLSHINSKIY, G.I., doktor Ceo.1.-mineral.nauk_(Moskva) Recent paleoclimatic maps of geological epochs. Priroda 50 no.8: 54-58 Ag 161. - (MMI. 14: 7) (Paleoclimatology-Maps) STRAKHOVI Niko2ay Mikhaylovich.. akademik, Lavreat Leninskoy prenii; otv. red.; NOSOV, G.I., red. izd-va; TSTROV, A.V.., red. izd-va; NOVICHKOTIA, N.D... telrhn. red.; SHEVCH M 0$ G.N.y tekhn. red. [Fundamentals of the theory of lithogenesiel Osnovy teorii lito- geneza. lzd.2. Moskva, Izd-vo Akad. nauk SSSR. Vol.l. (Types of lithogenesis and their distribution on the earth's surface] Tipy litogeneza i ikh razmeshchenie na, poverkbnosti zemli. 1962. 211 p. Vol.2. (Characteristics of the composition and distribution of aqueous sediments] Zakonomernosti sostava i razmeshcheniia gumid- nykh otlozhenii. 1962. 573 p. (MIRA -15-5) (Rocks, Sedimentary) STRAKHOV, Nikolay Mikhaylovich; BUSHINSKIY.-G-L-, otv. red.; NOSOV, G.I., red.izd-va; SHEVCHENKO, G.N., tekhn. red.; SIMKINA, G.S., tekhn.red. (Fundamentals of the theory of lithogenesis]Osnovy teorii litogene- za. Moskva, Izd-vo Akad. nauk SSSR. Vol.3.[Characteristies of the composition and distribution of and sediments]Zakonomermosti so- stava i razmeshcheniia aridnykh otlozhenii. 1962. 549 P. (MIRA 16:2) (Arid regions) (Rocks, Sedimentary) ITLEt The Conference on applied karstology PERIODICALi Izvestlya Akademii nauk SSSR, Serlya ge~logicheskaya, no. 1, 1963, 124 - 126 (OutbOrOf - OvOtUtokly, D. A., an& ChJkJJy, A. 0.) TEXT: The Conference was hold in Moscow on Apr?l 23 - 25, 1962, and was attended by 35 representatives from 16 scientiflcal and Industrial organizations. The Conference was opened by H. A. Ovozdetskiy who reported on the activities of the aeographical section of the Moscow Society of Natural scientists. The follow- Ing reports were deliveredi A. 0. Lykoshin on the investigation of karats for hydro-engineering construction by geological engineers; V. S. Polevoy on the use of geophysical methods to study karstz in areas of hydrological engineering struo- tures; 1. A. Savarenskiy on problems considering karats in Industrial and urban construction !9 -theDzerzhinak region; N. A. Ovozdetskiy on "Karat in the region of Caucasian Mineral Water Sourcee"I 1. 1. Ginzburg on mineral resources connected with karat prooesseal Q. L Waumki-T& bauxite and phosphorite karat deposital Ye. T. Bobrov on "Karat bauxites of the Yeniaey ridgi and the adjacent region of the Siberian platform"; N. A. 'Asitsyna on "Karat bauxites in the Kazakh folding: and the Turgay depreasion7r; B N. Ivanov and It. N. Dublu askiy on "The importanc of the Crimea karat in national economy"; ~'__-6::C-h_1'R_1ahev on "The Importance of the Central Ural karat In national economy"I 1. K. Kudryashov on the influence.of karat on agriculture in some Bashkirian reglofis; The reports delivered were dis- cussed 1,;.* D. S. Sokolova, V. A. V&rsanof'yeva, N. A. Kraail'nikova, S. A. Slad- a kopevtseva, V. S. Polevoy and others. The Conference approved the methods of .karat investigation, Including geophysical means, electrical i3eismio and ultra- sonic prospecting. It was deoided.to investigate in detail the development and expansions of karat; to study the origination of karat bauxites, to control the purity of mineral water sources and to continue research in the agricultural re- Sion* of Bashkiria. BUSHINSKIY, G.I. - Role of karat in the formation and distribution of bauxite deposits. Biul. MOIP Oltd. geol. 37 no.6:143-1-44 N-D 162. (MM 16:8) I BUSHINISKI'll Titanium in the sed3ment-ation Jdt.~ pol.iskop. no.2:197- 217 '63. (MIFU 17'10) ~ . Geojt)gir-.'. e,~ijdy in!; t i 4 it, AN Mos-~vu. .1 L-1 - BUSHINSKIY) G.J. 11-1 -1- --1--'.. - , Some problems of bauxite geology. Trudy GIN no.103:5-24 164. (MIRA 17.-11) LISITSYNA. N.A.; PASTUKHOVA, M.V.; BUSIIINSKIY) G.I., otv.red.; YEROFEYEVA) I.M., red.izd-va; ULYANOVA,-'O-.*G'.'-, tekhn.red. (structural types of Mesozoic and Cenozoic bauxites in Kazakhstan and Western Siberia.] Strukturnye tipy mozo-kainozoiskikh boksi- tov Kazakhatana i Zapadnoi Sibiri. Moskva, 1963. 107 p. illus. [Akademiia nauk SSSR. Geoloricheskii institut. Trudy, no-95). MIRA 17:2) -- OREROV., R.P.; GRINSHPAN, L.B.; BUSHINSKIY, G.I.; KUPEPEAN, M.Ye. Composition and structure of naturally occurring calcium phosphates. Zhur. prikl. khim. 37 no. 4:716-721 Ap 164. (MIRA 17:5)