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地质学
THEORETICAL REFLECTICTIONS ON THE GEOMORPHOLOGY OF CHINA FROM THE VIEWPOINT OF GLACIO-EUSTATISM.
<正> It is quite generally accepted that the growth of the Pleistocene ice-capsdemanded world-wide depression of mean sea-level; indeed,as Henri Bauligsays,"it expresses a physical necessity." There is striking evidence,moreover,for such a recent depression in the extension of river systems across the continental
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中国地质学会志
1936年01期
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