منابع مشابه
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The theory of isostasy supposes that, in regions which have not been disturbed recently, each vertical column of the earth's crust with a certain minimum radius and extending to a depth of about IOO km has approximately the same mass. To find the deviation from this approximation in a given region, the density must be assumed as a function of depth. Such assumptions used at present for calculat...
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ژورنال
عنوان ژورنال: American Journal of Public Health
سال: 1927
ISSN: 0271-4353
DOI: 10.2105/ajph.17.7.734