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1	CHARACTERISTICS OF THE GEOPHYSICAL FIELDS IN THE TERRITORY OF THE USSR (Kharakteristika Geofizicheskikh Polei Territorii SSSR)
	Soloveva,N. M.
	In: DTIC AND NTIS (1970)
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2	ON BOUGUER ANOMALIES IN THE OCEAN (Ob Anomaliyakh Buge na Okeanakh)
	Grushinskii,N. P.; Sazhina,N. B.
	In: DTIC AND NTIS (1970)
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3	On the Errors of Determining the Earth's Potential from Measurements of Gravity on a Given Surface (Ob Oshibkakh Opredeleniya Potentsiala Zemli po Izmereniyam Sily Tyazhesti na Izvestnoi Poverkhnosti)
	Shkodrov,V. G.
	In: DTIC AND NTIS (1970)
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4	Report on Gravimetric Work Completed in the Soviet Union from 1966 to 1969 on Subjects of the International Gravity Commission.
	In: DTIC AND NTIS (1970)
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5	THE EARTH'S CRUST AND MANTLE
	Demenitskaya,R. M.
	In: DTIC AND NTIS (1970)
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6	On the Equation of Gravity (Pro Rivnyannya Syly Tyazhinnya)
	Chornyi,A. V.
	In: DTIC AND NTIS (1970)
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7	ON THE DETERMINATION OF THE VERTICAL GRADIENT OF THE TERRESTRIAL ACCELERATION OF THE GEOIDAL EARTH (Pro Viznachennya Verticalnogo Gradienta Zemnogo Priskorennya Geoidalnoi Zemli)
	Monin,I. F.
	In: DTIC AND NTIS (1969)
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8	ON THE NUMERICAL SOLUTION OF MOLODENSKII'S INTEGRAL EQUATION FOR LAYER DENSITY (K Voprosu o Chislennom Reshenii Integralnogo Uraveniya Molodenskogo dlya Plotnosti Sloya)
	Eremeev,V. F.
	In: DTIC AND NTIS (1969)
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9	GRAVIMETER IN A GONDOLA (Gravimetr v Gondole)
	Gubarenko,L. A.; Staklo,A. V.
	In: DTIC AND NTIS (1969)
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10	THE PROBLEM OF ALLOWING FOR THE EFFECT OF THE CENTRAL ZONE ON THE VALUE OF MOLODENSKII'S CORRECTION G SUB 1 (K Voprosu ob Uchete Vliyaniya Tsentralnoi Zony na Velichinu Popravok G1 Molodenskogo)
	Yurkina,M. I.; Kropotova,L. E.
	In: DTIC AND NTIS (1969)
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11	REFINEMENT OF MOLODENSKII'S INTEGRAL FORMULAS FOR RADIAL AND LENGTHWISE DISPLACEMENTS (Utochenie Integralnykh Formul Molodenskogo dlya Radialnogo i Prodolnogo Sdvigov)
	Eremeev,V. F.; Yurkina,M. I.
	In: DTIC AND NTIS (1969)
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12	ON THE PROBLEM OF PROCESSING THE RESULTS OF A GRAVIMETRIC SURVEY (K Voprosu ob Obrabotke Rezultatov Gravimetricheskoi s Emki)
	Aleksidze,M. A.
	In: DTIC AND NTIS (1969)
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13	THE INFLUENCE OF ATMOSPHERIC MASSES ON THE EARTH'S GRAVITATIONAL FIELD (Vluiyanie Atmosfernykh Mass na Gravitatsionnoe Pole Zemli).
	Dvulit,P. D.
	In: DTIC AND NTIS (1969)
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14	ON THE PROBLEM OF CALCULATING THE HIGHER DERIVATIVES OF THE GRAVITY POTENTIAL (K Voprosu Vychisleniya Vysshykh Proizvodnykh Potentsyala Sily Tyazhesti)
	Aleksidze,M. A.; Kartvelishvili ,K. M.
	In: DTIC AND NTIS (1969)
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15	ON THE COMPUTATION OF PLUMBLINE DEFLECTIONS AND QUASIGEOID HEIGHTS IN MOUNTAINS (O Vychislenii Uklonenii Otvesa i Vysot Kvazigeoida v Gorakh)
	Pellinen,L. P.
	In: DTIC AND NTIS (1969)
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16	BASIC FEATURES OF THE DEEP-SEATED STRUCTURE OF THE URALS (Osnovnye Cherty Glubinnogo Stroeniya Urala)
	Sobolev,I. D.
	In: DTIC AND NTIS (1969)
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17	ACCURACY OF COMPUTATION OF THE ANOMALOUS PART OF THE GRAVITATIONAL FIELD OUTSIDE THE EARTH (Tochnost Vychisleniya Anomalnoi Chasti Gravitatsionnogo Polya Vne Zemli)
	Molodenskii,M. S.
	In: DTIC AND NTIS (1969)
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18	ON THE DERIVATION OF THE BOUNDARY CONDITION IN THE EARTH FIGURE THEORY (O Vyvode Granichnogo Usloviya Teorii Figury Zemli)
	Eremeev,V. F.; Yurkina,M. I.
	In: DTIC AND NTIS (1969)
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19	ON THE METHOD OF HARMONIC ANALYSIS OF WEAK TIDES (O Metode Garmonicheskogo Analiza Slabykh Prilivov)
	Balenko,V. G.
	In: DTIC AND NTIS (1969)
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20	DETERMINATION OF THE COMPOSITION OF ROCKS OF THE PALEOZOIC BASEMENT ACCORDING TO CHARACTERISTIC PECULIARITIES OF THE ANOMALOUS MAGNETIC FIELD.
	Glazunova,A. V.
	In: DTIC AND NTIS (1968)
	Abstract: The translation discusses at length, and shows with graphs and charts, the comparison of results of the aeromagnetic survey with drilling data. It is indicated that aeromagnetic investigations are effective in determining the material composition of rocks of the Paleozoic basement in a geologically closed area. The conclusions drawn from this work are as indicated: (1) Determination of the basement rocks should be carried out on the basis of physical properties of rocks and peculiarities of the anomalous magnetic field above open areas, where known Paleozoic complexes of rocks are exposed on the surface. (2) While dividing the Paleozoic basement rocks in terms of material composition it is necessary to consider the depth of occurrence of magnetic rocks which cause T anomalies. (3) On a geologically closed area an analysis of the anomalous magnetic field from the point of view of determining the composition of the Paleozoic basement should be carried out in combination with the gravimetric data. (Author) ; Trans. of Akademiya Nauk Turkmenskoi SSR, Ashkhabad. Izvestiya. Seriya Fiziko-Tekhnicheskikh, Khimicheskikh i Geologicheskikh Nauk, n6 p65-74 1966, tr. by Walter L. Burton.
	Keyword: (*STRUCTURAL GEOLOGY; AERIAL PHOTOGRAPHS; DEPOSITS; Geochemistry and Mineralogy; Geology; Geomagnetism; GRAPHS(CHARTS); GRAVITY; INTENSITY; MAGNETIC ANOMALY DETECTION; MAGNETIC FIELDS; MAGNETIC PROPERTIES; MAPS; METAMORPHIC ROCK; PALEONTOLOGY; PHYSICAL PROPERTIES; ROCK; SEDIMENTARY ROCK; SEDIMENTATION; TRANSLATIONS; USSR)
	URL: http://www.dtic.mil/docs/citations/AD0668301 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0668301
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