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1
CHARACTERISTICS OF THE GEOPHYSICAL FIELDS IN THE TERRITORY OF THE USSR (Kharakteristika Geofizicheskikh Polei Territorii SSSR)
In: DTIC AND NTIS (1970)
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2
DETERMINATION OF THE COMPOSITION OF ROCKS OF THE PALEOZOIC BASEMENT ACCORDING TO CHARACTERISTIC PECULIARITIES OF THE ANOMALOUS MAGNETIC FIELD.
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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3
UTILIZATION OF THE COMPLETE VERTICAL GRADIENT OF GRAVITY IN DETERMINING THE DEPTH OF THE ORIGINS OF GRAVITY ANOMALIES.
In: DTIC AND NTIS (1968)
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4
UTILIZATION OF ELECTRONIC COMPUTERS IN THE INTERPRETATION OF AERO-MAGNETIC SURVEYS.
In: DTIC AND NTIS (1967)
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5
GRAVITATIONAL FIELD OF THE ATLANTIC OCEAN AND ITS CONNECTION WITH THE ABYSSAL STRUCTURE OF THE EARTH'S CRUST.
In: DTIC AND NTIS (1967)
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6
GEOLOGICAL FACTORS FORMING GRAVITY ANOMALIES AND ISOSTATIC DISTURBANCES.
In: DTIC AND NTIS (1967)
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7
GEOPHYSICAL SKETCH-MAP OF KAZAKHSTAN.
In: DTIC AND NTIS (1967)
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