SCIENTIFIC ABSTRACT SINYAGINA, M.I. - SINYAK, K.M.

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• Collection: Scientific Abstracts
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• Document Release Date: August 24, 2000
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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

The international Association of Geodesy (Cont.) 497
Larin,, B. A. Thermal Properties of Invar Measuring Vires 12
Modern triangulation techniques require the highest degree of
accuracy in measuring base lines. In the USSR, the commonly
accepted 24 m. long invar or super-invar wires show little change
in thermal coefficients with time, or thermal after-effects on
the length of the wire. Invar wires can now be manufactured with
temperature coefficients of equal value but of opposite sign.
Entint I.I. Basis Systematic Errors in Precision Leveling 16
The systematic errors in precision leveling are vertical dis-
placements of the markers and of the tripod, and changes in the
angle between the line of sight and the bubble axis due to the
effect of temperatures. Other errors caused by non-vertical
position of the rods, etc. are noted, and means for correcting
them are recommended. In precision leveling the computed systematic
error is + 0.05 mm per kilometer.
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The International-Association of Ceodesy (Cont.) 497
Sinyagina, M. I. Preliminary Findings in the Study of Vertical
Dl-s-pl-ac-effie-ftt of the Earth's Crust Through Repeat Leveling
There is a considerable number of repeat leveling traverses in the
European part of the USSR, run to obtain a vertical control grid
of the entire USSR. The western part of European USSR, circumscribed
by the Baltic, Black and Azov seaslis more thoroughly covered by
observations -.nd as such was selected for the study of uplifts. The
necessary material was selected, systematized and properly computed.
To this study of 20,000 km of traverses, were added other geodetic
data including oceanographic and geo-morphological material; 82% of
all the traverses proved to be reliable. The recent rate of uplift
is -5 to j 10 m per annum, determined to an accuracy of 2 mm per an
card 5/ 12

The International Association of Geodesy (Cont.). 497
Pellinen, L. P. The Effect of Refraction on Angular MeasurementS
The main source of systematic errors in triangulation work is laterial
(horizontal) refraction. In observation during one niaht or day,
the errors vary between -t-0.5 - 0.7. Under unfavorable conditions
therp may appear other ei-rors of the same order. The greatest of
these is caused by refraction while measuring traverses in cities,
when the line of sight passes close to and parallel to the wall of
a large building. The accepted technique of triangulation in USSR
and the adopted methods of adjustments minimize the effects of
refraction.
Belyayev, N.A. A Photoelectric Device for Field Astronomical
Measurements 26
The described photoelectric system designed to record ~he
passage time of stars is attached to the AU 2/10 astronomical
vertical instrument (engineer's transit) and does not increase
substantially the weight or bulk of a field party's equipment; it is
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The International Association of Geodesy (Cont.) 497
easy to control and permits making lqpgitudinal Pad latitudInal-
determinations at f irst order stations without introducing human
errors into the observationse kccuracy achieved 19 &C"LU&
than usual and observations can be reuuced in number.
Yiolodenskiy, M. S. New Methods in Studying the Earth's Figure 28
In relation to the Earth's gravitational field the figure of a
geoid is not of single definition. To make it so, densities all
over outside the geoid must be determined. The author worked out
another way of investigating the Earth's figure, which excludes
the necessity of knowing the density of masses outside the geoid.
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The International Association of Geodesy (Cont.) 497
Molodenskiy, M. S. Solution of the Stokes Problem With a
Relative Error on the Order of the Square of the Earth's
Oblateness 33
By applying Stokes' formula to an ellipsoid surface such accurate
results are obtained, that the relative error is reduced to the
order of the square of the oblateness.
Lyustikh, Ye. N. Abyssal Structure of the Earth's Crust
in Indonesia Based r%n*Gravity Data 34
Descri.bing thL geotectonles -)f Indonesia, and the seismicity and
volc~Enism of the are-., _-.4, author discusses thf origin 3f the
regiok., its structural setting and the existing geo-synclines and
uplifts. He connects the belts of active and extinct volcanoes
with two lines of the Inner Sunda and the Northern part of the Inner
Celebes uplifts. The focal depths of earthquakes are greater than
50 km. Distribution of gravity anomalies and their quantitative
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The International Association of Geodesy (Cont.) 497
interpretation does not fit into the Vening Meinesz picture, nor
do the hypotheses of buckling,-nntraction, convection or horizontal
displacements account for the real distribution of gravity anomalies.
Kruchinenko, V.G., Platonov, Yu.P., Sukhov, V. B.
Electromechanical Device for Computing the Mean Moments of
the Passage of Stars During Observations 39
A photoelectric amplifier makes it possible to measure the duration
of two parts of a contact (rectangular output signal) into which it
is divided by a pulse :from a clock. Computing the moment of a star's
passage is accomplished by a formula given in the text. Observations
could also be conducted of high magnitude stars producing deformed
edges of the contacts. Means of increasing the efficiency of the
device were also indicated.
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The International Association of Geodesy (Cont.) 497
Nemiro, A.A. and Pavlov, N.N. Systematic Z-1-1.jcY- errors of the
FK3 Type and Their Influence on the Determination of Time
The comparison of fundamental and new absolute catalogues with FK3
permits finding in the latter considerable systematic errors of the
type ~,c,7i. Tables give comparative values for FV3 with Nikolayev
(N30), CC and Pulkovo (Puocl) with respect to4~~d-~,c . The observed
errors have a tangible effect on the correction of time. It is
pointed out that Washington determinations of time corrections are
distinguished by their high accuracy.
Pavlov, N.N. Recent Results of Photoelectric Observations of
the Pulkovo Time Service
Recent (1955-56) observations of the right ascension of stars made
with a new 100 mm Zeiss transit instrument show much greater
accuracy than those made with previous photoelectrical instruments.
The probable observation error for onr star, reduced to the
equator, and the probable error of hourly corrections for ten stars
49
54
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The International Association of Geodesy (Cont.) 497
-was much smaller than in the past. It is proposed to organize
at Pulkovo, during the ICY, observations by two transit instruments
covering more than 500 stars.
Fedorov, Ye. P. Computing the Coordinates of the Pole 60
The systematic errors in the coordinates of the Pole published
by the Central Bureau of the International Latitude Service (ILS) are
caused by an insufficient number (3-6) of observations. The
regular latitude observations are now conducted at 13 stations and
will bu increased probably to more than 20 during the ICY. With a
sufficiently large number of stations participating in this program,
the inherently weak loop method of calculations is still the most
acceptable as some difference in the systems of Jeclinations at
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The International Association of Geodesy (Cont.) 497
various stations will not Agnificantly affect the results.
Mean latitudes are deterraiii.d by A. Orlov's method.
AVAILABLE: Library of Congress
Card 12/12 MM/Jmr
8-21-58

SUDAKOV. 8.G.; ALEKSAIMMV, T.F.; BAGROV, M.A.; BUIANOV, A.I.; KAMENSKAYA,
M.V.; KLJZIHIN. B.S.; LITVIHOV. B.A.; 4MAGIU-, M.I.,- TIM&RIV. A.A.;
XYTIN. I.I.; pri uchastii Sinyaginoy,V.I.: BUIANOV. A.I.. red.:
ROKAHOVA, V.V.. teldin.red.
[Instructions for first. second, third and fourth class leveling]
Instruktaiis po niveltroyaniiu 1, 11, 111 1 IV klassov. lzd. 2-oe,
ispr. i dop. Moskva, Izd-vo geodez. lit-r7, 1957. io6
% ('N'ift 11:4)
1. Russia (1923- U.S.S.Ra) Glaynoye upravleniye gecd~zii i
kartograf ii,
(Leveling)

- ~ A -:1. ~1~ At I .~~i 1 7~ " - - -- -
- - - ,- , 4 T.j -- !, -~i .--- I-,,-'I " 1,I '-~ .- . ,- - A. , "-," .I ,
I
"The Achievements of Soviet Science in the Geodesy."
paper presented at the XIth General AsBembly of the Int'l. Union of Geodesy and
Geophysics, Tornoto, Canada, 3-14 Sept. 1957 (Izv. Ak Nauk SSSR - Ser Geog. 1958,
No. 2, PP 3-8 [USSR]).

in. L.Y III, I.I . ,
"The Study of Present Movements of the Earth Crust in the European Part of
the USSR."
paper presented at the XIth General Assembly of the Int'l Union of Geodesy and
Geophysics, Toronto, Canada, 3-14 Sept. 1957 (Izv. Ak Nauk SSSR - Ser. Geog. 1958,
No. 2, PP 3-8 [USSRI).

SUDAKOY, S.G.; ALEKSMaROY, T.F., BAGROV, M.A.; BULANOV, A.I.; KAWNSKATA,
M.V.; KUZIKIN, B.S.; LITTINOT, B.A.; ~INYAGINA_, 9.1 - TIKOFEM,
A.A.; MIN, I.I.. Prinimala uchastiye SIRTAGINA, V.I.. ROKANOVA.
V.V., tekhn.red.
[instructions for first-. second-. third-. and fourth-order leveling]
Instraktaiia po nivelirovaniiu 1, N, III i IT klassov. Izd.3, Ispr.
i dop. Koskva, Izd-vo geod.T-ry. 1959. 111 P. (KIU 13:3)
1. Russia (1923- U.S.S.R.) Glavnoys upravieniye geodesii L karto-
grafii.
(Leveling--Handbooks, mamials, etc.)

3W SOV/6-59-8-4/27
AUTHORS: Sinyagina, X. I~,q_qandidate of Technical Sciencesq Orlenko9L. P.
TITLEs Present-day Vertical Movements of the Coast of the Caspian Sea
(sovremenny-ye vertikallnyye dvizheniya poberezhlya
Kaspiyokogo morya)
PERIODICAL: Geodeziya i kartografiyaq 1959, Nr 8, pp 22-;28 (USSR)
ABSTRACTs The results of the geologia -geomorphological investigations
showed that the assumed velocities of the vertioal movements
of the earth crust at the coast of the Caspian Sea differ
widely from the velocities found in the investigations carried
out by A. A. Izotov (Ref 1). N. I. Poteyev and V. G. Rikhter
established a hypothesis on the short-time earth crust
vibrations in the area of the Caspian Sea to explain these
phenomena. The new line of leveling of the 1st order,
established in 1949, between Baku and Astrakhan', and the
systematization and evaluation of the results of observations
made in the course of many ye4rs rendered it possible to reviewq
and add to-,:the present concepts of ~~':~,~_present-day movements
of the coast of the Caspian Sea. The results of releveling as
Card 1/3 well as the observation of I levels of seas not directly

Present-day Vertical Movements of the Coast of the SOV16-59-8-4127
Caspian Sea
connected with the oceans make it possible only to determine
the vertical shifts of the earth crust in two neighboring
points in relation to one another. The present investigationg
therefore, consisted in 1) the determination of the "absolute"
velocity of one of the leveling points regarded as the base
point. When selecting this point provision was made that it
was connected with other bench marks by a relevel; 2) the
determination of the velocity on the basis of the data obtained
by level observations; 3) checking the velocity of the
present movements determined on the basis of the level
observations and the data of the relevel. - The basis for the
determination of the "absolute" value of the velocity was
Makhachkala. It was selected for a nil ber of reasons: level
observations since 1901, connected reliably by relevel with
neighboring points on the Black Sea, and least mobile on the
west coast of the Caspian Sea from the point of view of geology
and geomorphology. It is assumed that the velocities of vertical
movements of the Black-Sea coast in present times has an
"absolute" character on the basis of the data of oceanograph i-
cal observations obtained. V. G. Rikhter's supposition was not
Card 2/3 found true. The velocities obtained differ greatly from those

Present-day Vertical Movements of the Coast of the SOV/6-59-~8-4/27
Caspian Sea
obtained by A. A. Izotov. The reason for the error to be found
with Izotov seems to lie in a wrong sign. - Diagram 3 shows
that a change of sign is to be found in the vibrations of the
earth crust in the Makhachkala-Khurdalan section only. In the
evaluation of the level observations it was found that the
zero point of the levels at Baku sinks irregularly with regard
to Makhachkala. The data shown in the table given at this point
show that Baladzhary, Baku, and Bailov Cape are sinking at a
faster rate than the rest of the Caspian-Sea coast. This was
found as early as the beginning of the 20th century. These
leveling 9perations of 1912 were repeated in 1929. The results
are contained in the papers by N. N. Boll shakov and G. F. Bregman.
They are shown in the present paper schematically in figure 4.
The lowering of the Surakhany, Sabunchi, and Romany oil fields
is most prominent. - In order to determine the intensity of the
present shift, a third leveling operation of the fixed points
established in 1910-12 will have to be carried out. There are
4 figures, 1 table, and 3 Soviet references.
Card 3/3

71
7 R 3 Candidate of sov/6-59-9-17/19
~
4
~
e s , ?i n I ',- o , Y e . -1 .
ie n c
73c
T--'-!.LE:, Conference on the Problem "Present Tectonic Movements in
the Territory of the USSR"
PERIODICAL: Geodeziya i kartografiya, 1959, Nr 9, PP 71-74 (USSR)
ABSTRACT: A conference on the problem "Present Tectonic Movements in
the Territory of the USSR" took place at the Institut geo-
grafii AN SSSR (Institute of Geography of the AS USSR) in
Moscow early in Pebruary 1959. At this conference, the results
of the work carried out-in 1958 were discussed. This work
was carried out by the Teentrallnyy nauchno-issledovateliskiy
institut geodezii, aeros"yemki i kartografii (TsNIIGAiK)
(Central Scientific Research Institute of Geodesy, Aerial
Surveying, and Cartography), the Institut geografii (Institute
of Geography), Moskovskiy institut inzhenerov geodezii, aero-
fotosllyemki i kartografii (MIIGAiK)(Moscow Institute of Geo-
detic, Aerial Survey, and Cartographic Engineers), and the
oceanographic institutes. In the conference were taking part:
more than 70 repre sentatives of the institutes of the AS USSR,
Card 1/6 of the Sibirskoy6 otdeleniye AN SSSR (Siberian Branch of the

Conference on the Problem "Present Tectonic SOV/6-59-9-17/19
Movements in the Territory of the USSR"
AS USSR), the Academies of Sciences of the Ukraine, Turk-
meniya, Esthonia, of the Bashkirskiy filial AN SSSn (Bash-
kiriya Branch ofthe AS USSR), of the MIIGAiK, the TsNIIGAiK,
of the Moskovskiy geologorazvedochnyy institut (Moscow Geo-
logical Prospecting Institute), of the Odesskiy gidrometeoro-
logicheskiy institut (Odessa Hydrometeorological Institute),
the Sverdlovskiy politekhnicheskiy institut (Sverdlovsk Poly-
technic Institute , the Nauchno-issledovatellskiy institut
geologii Arktiki 4cientific Research Institute of Arctic
Geology), the'vseso'yuznyy gidrogeologicheskiy trest (All-Union
Hydrogeological Trust), the Kiyevskiy universitet (Kiyev Uhi-
versity), the Permskiy universitet (Perm' University), and
the Sredneaziatskiy universitet (Soviet Central AsiaNUniversity).
The conference was opened by Academician I. P. Gerasimov,
Chairman of the Coordination Committee. He mentioned the high
scientific importance of the first monograph on the present
vertical motions of the earth's crust, as well as the important
circumstance of the participation of Poland and Rumania in
this research work. He also mentioned the participation of
Card 216 Yu. A. Meshcheryakov and M. I. Sinyagina Atthe International

Conference c- Problem "Present Tr~-.,onic SOV/6-59-9-17/19
Mov -~,
-.ents in ~h.~ Territory of the US,-~7V'
Oon
. -ress ~f "eodesy a-n-. Ceophysics in Canada, 1957.
S. 3. Shullts (Laboratoriya aerometodov AN SSSR (Laboratory
of Aeromethods of the AS USSR)) and N. I. Nikolayev (Moskov-
ski-y geologorazvedochnyy institut (Moscow Geological Prospect-
ing Institute)) delivered a report on the legend and model of
the map of modern tectonics (on a scale of 1 : 2,500,000),
which is being compiled for the whole territory of the USSR,
and on the additional map "Present Tectonics and Seismology".
M. I. Sinyagina reported on-the results of work in the I.TIIGAiK
in 1-958- One of the methods of checking the rate of present
tectonic -notions in the west of the European part of the USSR
was the calculation carried out by F. V. Antohova, Candidate
.Lor Diploma at the MIIGAiK, concerning the polygon misclosure
in the leveling net of 1st and 2nd order, G. A. Zhelning col-
laborator of the Institut fiziki i astronorii. AN ESSR (Institute
of Physics and Astronomy of the AS Esthon-im,'SSR) reported on
the second leveling in the state leveling net for the purpose
of ascertaining the present vertical motions of the earth's
crust in the area of Esthonia.- A. K. Pevnev (MIIGAiK) repmted
Card 3/6 on the results of the second leveling in the area of the

Conference on the Problem "Present Tectonic SOV/6-59-9-17/19
Movements in the Territory of the USSR"
Baskunchakskiy salt dome (town of Bogdo).- A. P. Bachmanov
(Odesskiy gidrometeorologicheskiy institut) spoke on the
systemaiization, evaluation, and analysis of leveling data
of different years in the area of Odessa.- S. K. Gorelov and
L. Ye. Setunskaya (Institut geografii AN SSSR) reported on
the results of application of geological-geomorphological
methods.-A. P. Rozhdestvenskiy and Yu. K. Zhurenko (Bashkirskiy
filial AN SSSR) piesented the results of investigations of
present tectonic motions in the territory of Bashkiriya.-
N. V. Dumitrashko, S. L. Kushchev, and D. A. Liliyenberg
(Institut geografii AN- SSSR) reported on'the studies of tectonic
motions in the Caucasus.- Preliminary results of the geological-
geomorphological analysis of data of the second leveling were
put forward in brief by the collaborators of the Institut
geografii AN SSSRv A, G. Doskach (Kurgan-Irgiz line), Ye. A.
FinIko (Semipalatinsk - Alma-Ata line), and V. A. Fillkin
(Barnaul-Semipalatinsk line).- V. V. Lomakin (Geologicheskiy
institut AN SSSR) reported on the wave-like character of the
motion of the earth's crust in the area of Lake Baikal.-
Card 4/6 N. P.-Ladokhin (Geologicheskiy institut Sibirskogo otdeleniya

"'OrIference c). t1ne Problem "Present Tect:)nic SOV/6-59-9-17/19
:.1cveqient3 in the Territory of "he U3S__-'1,"
AN SSSR (Geological Institute of the Siberian Branch of the
A3 USSR)) described the method of studying the present tectonic
movements in the Proval Grulf of Lake Baikal.- Ye. N. Pokrass
reported on the investigations of present tectonic movements
in the Lower Caucasus (Predkavkazlye) and in West Siberia by
means of geomorphological methods.- A. T. Donabedov (Kompleks-
nay-- yuzhrLO-geologicheskaya ekspeditsiya (Multiple-purpose
South-geological Expedition)) explained the connection between
the rate of present vertical motions and the gravitational
anomalies.- G. A. Kon1kov (Novocherkasskiy politekhnicheskiy
institut (Ilovocherkassk Polytechnic Institute)) pointed - by
the example of Donbass - to the possibility of a connection
between the coal- and gas discharge, on one hand, and the
present tectonic movements and stresses, on the other hand.
11. 1. Nikolayev (MGRI) spoke "On the Nature of Present Tec-
tonic Movements and on the liethod of Studying Them in the
Technical Activity of Man".- Yu. A. Meshcheryakov (Institut
--eografii AN SSSR) described the present state of knowledge
concerning secular motions.- A. V. Zhivago (Institut geografii
Card 5/6 AN SSSR) pointed to the necessity of considering the eustatic

Conference on the Problem "Present Tectonic SOV/6-59-9-17/19
Movements in the Territory.of the USSR"
variations.- A. I. Durnev (MIIGAiK) spoke in favor of an
extended investigation of this problem.- A. A. Izotov spolke
on the critical judgment of data of the second leveling,
V. Yu. Skullskiy (Sverdlovskiy universitet) analyzed the map
of present tectonic movements in the Ural.- Yu. A. Skvortsov
(Sredneaziatskiy universitet) pointed to the great possibiLities
of applying aeromethods to the analysis of present movements.-
The Conference decided to publish the monograph "Present Tec-
tonic Movements in the Territory of the USSR". The next con-
ferelace is planned for 1961.
Card 616

SNYAGINA M.I89 kand.tekhnonauk
StiAy of recent vertical movements of the earth's crust in the
U.S.S.R. Geod. I ke6rt. zio*7:12-17 Jl 160. (MIRA 13:9)
(Leveling) (Earth movewnts)

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S/035/62/000/007/071/083
The state of knowledge on... A001/~101
The data available make it nevertheless possible to notice certain regularities
in manifestations of recent movements. Evidently, recent movements of the Earth's
crust proceed everywhere; there are no stable regions of the crust. Prevailing
intensity of recent movements is within a few mm, in individual regions were
established movement speedsof the order of some cm and dm per year., The recent
movements represent apparently oscillation movements; however, the problem on the
period of these oscillations is still unclear. It can be presumed that duration of
the period is beyond the limits of several centuries, thus the term "secular mo-
vements" can be considered as synonym of recent tectonic movements. A relation
between recent movements and structural elements of the Earth's crust indicates
the tectonic nature of movements: They are caused by,abyssal (endogenous) processes.
In the present epoch, the glaciolsostatic factor affects weakly the character of
movements; however, during the Hoiocene (last 12,'000 - 15,000 years) this factor
played a large role. The taski of further studies of recent movements. conducted
by the International Geodetic and Geophysical Union, are as follows: 1) Compiling
summary maps of recent movements; 2) analysis of theoretical problems on regula-
rities in manifestations of recent movements and their relation to endogenous
processes; 3) studying the possibility of practical utilization of movements data
Card 2/3

3/00-5 16 21000/00221100-1 /001
DO 5 4
A U T P 43 R.,. R'y 13 r
TI-LE- Some lbasi,, probIRms of the study of p~o-~sen~--Iay veri,i -7a-,
mr, v ermen t,7 -: frhz: Eartlits crust.
PE' 7 OD 1 C 4L: leod.~-ziya i xartografiya, no. 2, 196-2 1.1 .a. 6
S XT Tn~ s,~ggpsts that a oommon appraa:h should bp mad--~ tc~ the
Pro:, em ~,.f sfui~ying prp3enf verfi;:tal movemen-L~; of the Earthlq ~-ruslt and
~i~,a;- ih~s I-ouli be ac:hieved f the mean su,-vfa---& were ac-
surfa.::-.!? and. t~e same method olt' adju-sting velo-ity
',,y rer,,7~A-tod leve-iling were usod.. Observatloria sy--tematinal-
ri-?d ia-in,~ tbe 'iasqt 80. 90 years showe-j tttat the deformatiark ~,t
e F r7 hj~5 k:,UV is M,:~S v ly naused ty te~,. tonic wh I-h cart cause
r sudden movempfits in seismi~,all'y a-tive regicyno or
~;-,C-W Mu"'Vemeris of an os-illatovy c-harmicter. I n t tie f ia s t c ~- sz
s-urvpy is r-ommended. The stuly of movements 3f the

Sloor~ 're,2/0()C)100~'1OC)_, /00--
S DO'z, 1,/D!
ra ruqcr-~ -omp, as several c,
d thawing
undergroun,i watter, Ireezirg an,
oj T-, --sra."luare t_--ffectsl the 40irlt W.-)rk of
1.9 ne~_,essary.. L, mp A -a c, ri o I'
L
M03r)-; thes"! molr?ment,~ it) Var-L.:,; -a is bas~3 on zn~
L ,E
n_- t ile vel :,e and di r,~, tion of i s ve" o t t,)r ower a per,.-J Of
rrr,5 Y eEtrs are ..ons tan kt howeve r, tht2 - oampar i5 oil of i h- z~ o~ map
ff,~ -T
U e ra u e C, f d I rent referen ~-u r faces E,,; t ed -r4
I r, e 0. ~.eie worlds oceans is .&K~n as 11-be
Ivlk f~,r eustatIc changes ifL thiS leVC-I. 0 f h
hd,e ,,~.oser difft-,rpnt referea-e zurfa_-s. Tbi_~ probjj~,-m
:L-. the M,)Okovskly
Gz,~-d P sy , A,~ r i a! Pho t ,g rapkiy
",71o wr, 111 z e, o f E ng I rtp - i - S ~t I -
r 13, r,,;' (rk_r~ ;AiK)- Tf-_~ re5QTts of ousiorvaticvn o' Lh-z i%-f
Z , ) . I - - 1. L i
3 P ~j i-, t, tie T r an s a.-- t 41 o ns ti.= In t e r na t -1 ~2 :.-al Oo. ano
5 1 a t r -t r, a I y z e 1They showel tinat the .-i~
F s - z,)v ts -),ar i -1 oill y by 0. 0 3 mm /Y,~S r, ') v,~ r

SIOC,~ '/6-2 /' 1000/002/001 /001
DO 541 /Dl I
m a na r) T C- L) I ~-Mi
r Tm) tbe me-an. level _' f the ;'To.rl ri 1 S c -,P' .-Orls
r 0,!.j I- tj 4- t 5 fa f a c' -.1 -y beinR
U )rs whj~-r influence thp .-a" --j'at~d 8r I
oc tjj~ whol.2 ~aoi_ d . Thi_'z; means that ._`nang~-S :n tb,~
ri T. 2 r IP r t a oristant rellle,,-tiag the .30- 6ia! M07&me~-C' -Jt

"I r r j e r, niz
f U ~_: r, Tner-,,or-~, the nean Ie-vel of ztr-t-.ht_-o cf
an be tal, &. n -as a referen-e zijrfa_e fcar, ~cmp:.lJr~g
on ne n
- tit of pi,esent-daj the zst~K'-:
-Ile v-1o
a c) 1 !
,
,
V
-~nuqixig th;- re' e - e r, o u ra
~i a ~~nifcrjri metl~orl of
Tii J i~ I s7- r anj f-om-
ci n; ng the abso.cite value of veloiiity of thet%(- facliements
-
1! a I ~i t:- ~3 in dilfferent, T)a-rts of th- Eartri, and wou'ic -L al5c) per-,
rr, i ~~ j,_t 1. e i r,.~, r i n t he tly compa, tat i-on by repeal td
,.n - a m ial -,~-feren, ;-1 s,,rt'a-;e. The study of tab'L~s of re7,aT?-.r,?
iqet4 i3y repeated 'Ieve"ling :-,~d ~Fea-'Ieve-l _~af
J'? t. e
s, no . 12 3 L' " T raris a,~ 11 ions of the Ts 11' 11 ("A *, K " an.:; i r! at, a r t i,"'

o!cr a -el obsenvatiuns .-.armn be diistor tej It -v
onfirm~3 that 9 e, -
- ilrrors and ~-.ar. b,~- used for rompilling Th-
variarion~~ i~n thr- -level of 'ht- aor_P-ils c-?aczz
ia-1 ~Z tudy and ar.ar'~ysis of tl,~ s of z-~a - 1,: I'sE I -
.a I

'Or,,o /,,)CI, /OC)
DO D-
Ti-0- r? i* re i,e n.--- c- r Cal -? i S di r,~- t 1 t -,.n-
I c,, 1 -3 d E t i r I c t .11 :1 Ir e 10 . i t ~ y '. , -, 4 ~ _,-, - OZI~. J 1 t- f r 9 t a
c; ~z wot7~-Szfs. In TISSIR, ~h~ U
IDU L a
MO y -~,.I r7
r, iz a c- -d be t t~n t h,~ P;~ 6 o c a - I ot I - n s
a f I e i by n. 'ar. rn.~hods and for &i,:j 1 a,- iu~ rt"r :--j*Lg v~~T
o. 1, - I I-, V,I-i
T~,, ~-: a u t n o o n s n,~ S u v -1 e m e l I:
Li L '--,--.n t "n u 3 61 LI 6 e .1 1 r -1 C 7 r I

SUDAKOV, S.G.; ALEKSANDROV, T.F.j BAGROV, M.A.; BULANOV, A.I.;
KAMENSKAYA, M.V.; KUZIMIN, B.S.; LITVINOV, B.A.; SINYAGINA,
M.-J,- TIMOFEYEV, A.A.; ENTIN, I.I. Prinimal uchaNCT.99--m-mmo
'9TWARGINA, V.I.; KOMARIKOVA, L.M., red.izd-va; HOMANOVA,
V.V.,, tekhn. red.
(Instructions for lst, 2dp 3d, and 4th-el4ps leveling] In-
struktsila po niveliroyaniiu I, 11, 111, 1 IV klaasov. 4 izd.
dop. i Aspr.- Moskva, Gosgeoltekhizdat, 1963. 110 P.
(miRA 16:6)
1. Russia (1923- U.S.S.R.) Glavnoys upravlenlye goodezii i
kartografli.
(Leveling)

L 22398-66 LEW T1 ( 10q
ACC NR, AT6011137 SOURCE CODE: UR/3197/65/000/002/0032/0037
AUTHOR: MI.I.
ORG: Moscow Institute.of ~Geodetic, Aerial Surveying and Cartographic Engineers
(Moskovs1dy institut inzhenerov geodezii, aerofotos "yemki i kartografii)
TITLE: Principles of designing a Map of the rate of contemporary movements
in a large area
SOURCE: AN EstSSR. Institut fizild i astronomii. , Sovremennyye dvizheniya
zemnoy kory. Recent crustal movements, no. 2, 1965, 32-37
TOPIC TAGS: geophysical conference, geodetic conference, leveling, map
compilation, tectonic map
ABSTRACT: The author discusses problems involved in compiling a map covering
a large area which shows the rates of movements of the earth's crust. The main
problem is defined as the analysis, sytematization, and adjustment of existing
repeated leveling lines run by various nations, based on different datums, of dif-
ferent quality, performed in different types of terrain with different procedures
and instruments, and the connection of these lines to lines still to be laid out.

L 22398-66
FACC NR. AT6011137 07
The need for uniform data processing is emphasized, and a formula is recom~!-
mended for use in determining weighted values, The desirability of carrying out
preliminary geological and geomorphological studies to be used as guides for
regional adjustments of leveling nets is emphasized. Orig. art. has- I fdrmulw.
[ER
SUB CODE: 08/ SUBM DATE: none
L Card 212 dOL

KARLINSKAYA, 14.I.;SINYAGINA,-M.N.
Telemachanization of city gas supply systems. Gaz. prom. no.6:15-20
Js 156. (WaA 9:12)
(Gas distribution) (Remote control)

PHASE I BOOK EXPWITATION 1137
Sinyagina., M.N. and Magnichkina., V.P.
Ispollzovaniye beBkontaktnykb i chastotnVkh elementav v kommanallnom khozyaygtve
(Use of Contactless and Frequenicy Devices in Nkmicipal Services) Moscow, Izd-
vo Min-va kownmallnogo khozyaystva Rsm, 1957. 120 P- 1.9500 copies printed.
Sponsoring Agency: Akademiya kommaniillnogo khozyVstva.
Ed. (Title page): Karlinskayaq M.I.; Ed... (Inside book): Bashkiror, L.G.; Tech.
Konyashins., A.D.
POMSE: This book is intended for scientists and engineers vorking in mnicipal
services.
COVEME: The authors describe contactless devices of remote control and sigua-
ling systems for controlling a small number of regulators, Tbey also describe
certain types of contactless and frequency devices ihich nV be used in auto-
matic control, remote control and signal" circuits of mmicipal system.
The book explains the basic theoreticatl prInciples of the application of reIA7
Card 1/4

Use of Contactless and (Cont.) 1137
circuits in automatic and telemechanical system with contactless eqailnent.
The authors describe the theoretical fundamentals of deelani ftequency
devices and nev types of frequency and contactless relays. They give ex-
amples of remote control systela using contactless and frequency devices.
Them are 20 references, of -which 13 are Soviet (including 1 translation),
and 7 English.
TABIE OF CORTEWS:
Introduction 3
PART 1. BASIC FROPERTISS AND CHAPACTERISTICS OF CONZACTrMS NAGNMC
SLEMENTS 8
Ch. 1. Survey of Existing Contactless Magnetic Elements 8
Ch. 2. Application of the Relay Circuit Theory to the Design Of Systems
With Contactless Magnetic Elements 13
Card 2/4

Use of Contactless and (Cont.) 1-137
Ch. 3. Properties, Characteristics and Basic Parameters of VAgnetic Elements of
Remote Control and Signalling Devices Used in Municipal Services for Con-
trolling a Snall, Number of Regulators 31
PART 2. BASIC FEATURES AND CHARACTHRIMICS OF HIMMONECHMCAL FRZQUZ=
DEVICES 56
Ch. 1. Survey of Existing Electromehanical Frequency Relays and Generators 56
Ch. 2. Theoretical Analysis of the Operation of a C(mitactless TUning-Fork Re-
lay and Tuning-Fork Generator 67
Ch. 3. Construction and Parameters of Tuning-Fork Relays and Generators
Developed by the Academy of Municipal Services 96
PART 3- KWMZS OF SYS7M WITH C072ACTLESS AND FREQUENCY UMCES FOR
CONTROLLING A SMALL NUMBER OF REGULATORS io6
Ch. 1. Systems of Remote Control Without Back-signalling for Controlling a
Card 3/4

Use of ContarAless and (Cont.) 1137
Small Number of Regulators
Ch. 2. Remote CoAtrol Systems With Back-signalling
Conclusions
Bibliography
AVAIIMLE: Library of Congress (TK2861.S5)
io6
111
120
122
Card 4/4 JP/mfd
1-23-59

ntac
SINYAGIN.ti,, .1. Cand Tech Sci (diss) "Utilization of wwzo
elements in ants d" the remote control of ptfolic
facilities." Mos, 1958. 13 pp (Acad of Economy im K. D. Pamfilov), 150
copies (KIL, 52-58, 103)
-92-

GAY111YEV, S.S., dots.; KLULLOVA,
II.R.,
st. prepod., red.
A.A., doto., glav. red.;
dots., red.; 3111YAGIIIA, N.P.,
[Vertebrates of Ullyanovsk Province] Pozvonochrye zhivotrqe
Ullianovskoi oblasti. Ullianovsk. Gos. pedagog. in-t, 1959.
74 P. (1-URA 16:10)
(Ullyanovsk Province-Vertebrates)

SINYAGINk. T.M.
Bottom fauna of Tashkepri Reservoir. Trudy Airg.gidrobiol.sta-
no-4:183-215 158. OMIRA 15:8)
(Tashkepri Reservoir-Benthos) '

S INYAG INA p T . M.
New apeuies of tendipedid IAa-vae of the subfamily Orthocladiinae
from some bodies of water of Turkmenistan. Trudy Murg.gidroblol.
sta. no-4:228-230 158. OMIU 15:8)
(Turkmenistan-Chironamidae)

SINYAGINA, V.A., kand. toklin. i-Lak.
~-: - ~... ...
Analysis of t~,~i rpault,8 of first-clans leveling in the Soviet Union.
Trudy TSNIMI.E." 15% (KIRA 11:3)
(I.-mling)

m
STRYA'alm 2 V. 1.
ANTIN, I.I.; GINTAGIWA. V.I.; YELISIM, S.V., kandidat tekhnichanicikh
nauk,
[fligh-accuracy surveyor's 1B level] Vysokotochnyi nivelir 1B.
Moskva, Isd-vo goodesicheskoi i Icartografichaskoi lit-ry, 1953.
118 P. (Kft 7:8)
(Surveying-Instruments)

SINYAGINA, V. 1.
"Principal Systematic Errors in Class I Leveling." Cand Tech. Sci, Moscow
Inst of 1~ngineers of Geodesy, Aerial Photography, and Cartography, Min Higher
Education USSR, Moscow, 1955. (KL, No 14, Apr 55)
SO: SUA. No. 704, 2 Nov 55 - Survey of Scientific and Technical Dissertations Defended
atUSSR Higher Educati-mal Institutions (16).

SUDAKOV.S.G.; ALIKSANDROV,T.F.; BAGROV.M.A.; BULANOV,A.I.; KA NSUYA.K.V.;
KUZIMIN,B.S.; LITVINOV,B.A4SI1fYAGDU,_N.I.; TIMOYBYBV,A.A.; BN?IN,I.I.;
SINTAGINA.V..I.
[Instructions for class I,II.III and IT leveling) Instruktsila po
nivelirovanliu I, II, III i IT klasmov. Moskvalzdvo geodozicheskot
lit-i7. 1955. 106 p. W" 9:3)
1. Russia (1923- 'U.S.S.R. )Glavuoye vipmvleaiye goodesit I 1mrtograf ii.
(Leveling)

ENTIN, Isay Illich; SINYAGIRA, Vera Ivimovaa; YELISEYEVA, S.V., kandidat
takhnichesk'ikh -~~l -r, VASIL'YEVA, V.I., redaktor;
KUZIMIN, G.M., tekhnicheskiy redaktor.
[High-precision level ORB21 Vreskotochnyi nivelir INBI. W.2-9e
Pod obshchsti red. S.Y.Tellsoreva. Moskva, izd-ve geodesichesket
lit-ry, 1956. 114 p. (MLRA 9:6)
(Level (Tool))

SINYAGINA, VI,, knndidat t6khnicheekikh nnuk.
"OL"; 11~,-
Accumulntion of systmatic errors in Int class leveling. Geod.1 kart.
no.4-.69-71 Je '56. (Leveling) (NLU 9310)

6 2 _7
"Geodetic Testing of the SVV-1 Light Range Finder.," by I. I.
Entin and V. I. Simyagina, Geodezia i Kartolgrafiya, No 4, Apr 57,
pp 9-17
The article gives a complete report on geodetic field tests carried
out by the Central Scientific Research Institute of Geodesy, Aerophotography
and Cartography (TsNIIGAiK) in 1W 6n the SVV-l light range finder. This
instrument is manufactured by the Scientific Research Experimental Workshop
(NM) of TsNIIGAiK according to drawings made by the Scientific Research
Institute of the Military Topographic Service (NII VTS).
In the field tests, data was compiled for the purpose of increasing the
accuracy of measurement control methodr with the SVV-1 instrument and of
establishing the possibility of using "polygonometry" in the constiuction
of a geodetic net with a light range finder.
The article includes a drawing of a previously constructed triangulation
net, on which the tests were based, and several tables which give comparative
wasurements and show the relative errors.
The authors atate that, vhereas the result* of the tests were encowmg
ing, further tests with the light range finder are necessary before a com-.
plete solution to the problem can be obtained.

It Is further stated that the SVV-1 itself needs to be further improved,,
for example by increasing the power of the illuminating lamp, and therebv
its operating distance, and by simplifying and reducing the weight of the
electric power supply system. "Together with the improvement of the light
range finder SVV.Ll, it is necessary to work persistently on the creation
of a light range finder with photoelectric indication, since this extremely
facilitates measurement and permits a reductinn in the size of the staff."
Four photographs appear in the article: Photo No 2'jO567 and Photo No
2TO568 give two.views of the range finder; Photo No 270569 shows a view of
the wave meter; and Photo No 270570 shows a large and one of two small
reflectors. (U)