RESULTS OF STUDY OF THE FORM OF THE GEOIDAL SURFACE IN ANTARCTICA (Rezultaty Issledovanii Formy Poverkhnosti Geoida v Antarktide)

Because of hydrological and geophysical investigations in Antarctica carried out by various countries, it is possible to present in the first approximation the structure of the sub-glacial relief and gravity field of considerable sections of the Antarctic continent and ocean. (Author) Trans. of Mors...

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Bibliographic Details
Main Author: Frolov,A. I.
Other Authors: AERONAUTICAL CHART AND INFORMATION CENTER ST LOUIS MO LINGUISTIC SECTION
Format: Text
Language:English
Published: 1969
Subjects:
Geology
Geochemistry and Mineralogy
(*STRUCTURAL GEOLOGY
ANTARCTIC REGIONS)
MAGNETIC ANOMALY DETECTION
ISOSTATIC CHANGE
EQUILIBRIUM(PHYSIOLOGY)
ICE
AERIAL PHOTOGRAPHY
GLACIERS
USSR
EARTH CRUST
ISOSTASY
TRANSLATIONS
Antarctic
Burton
The Antarctic
Antarc*
Antarctica
Online Access:http://www.dtic.mil/docs/citations/AD0689508
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0689508
Description
Summary:Because of hydrological and geophysical investigations in Antarctica carried out by various countries, it is possible to present in the first approximation the structure of the sub-glacial relief and gravity field of considerable sections of the Antarctic continent and ocean. (Author) Trans. of Morskie Gravimetricheskie Issledovaniya (USSR) v3 (covers 1960-65) p99-112 1967, by Walter L. Burton.

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