ISOSTASY OF ANTARCTICA.

Because of the complexity of isostatic anomaly computations, the conclusion on the isostatic state of Antarctica was originally drawn by averaged anomalies with a free-air reduction. However, B. A. Andreyev drew the conclusion that at the center of Antarctica one can expect to discover intensive neg...

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Bibliographic Details
Main Authors: Ushakov,S. A., Frolov,A. I.
Other Authors: AERONAUTICAL CHART AND INFORMATION CENTER ST LOUIS MO LINGUISTIC SECTION
Format: Text
Language:English
Published: 1967
Subjects:
Geology
Geochemistry and Mineralogy
(*ANTARCTIC REGIONS
*ISOSTATIC CHANGE)
TERRAIN
GRAVITY
NUMERICAL ANALYSIS
THEORY
POLYNOMIALS
TABLES(DATA)
USSR
Andreyev
Antarctic
Antarc*
Antarctica
Online Access:http://www.dtic.mil/docs/citations/AD0653952
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0653952
Description
Summary:Because of the complexity of isostatic anomaly computations, the conclusion on the isostatic state of Antarctica was originally drawn by averaged anomalies with a free-air reduction. However, B. A. Andreyev drew the conclusion that at the center of Antarctica one can expect to discover intensive negative isostatic anomalies of the order of 80 mgals. In this article the authors independently and by different methods attempted to find answers to the given conclusions. (Author) Izostaziya Antarktidy, trans. of Akademiya Nauk SSSR. Doklady, v160 n4 p819-22 1965.

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