ON ABSOLUTE FALL OF SEA-LEVEL DURING QUATERNARY

被引:10
作者
HOLMES, JW
机构
[1] Commonwealth Scientific and Industrial Research Organisation, Division of Soils, Adelaide
关键词
D O I
10.1016/0031-0182(69)90016-9
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The discrepancy between the decline in sea-level since the beginning of the Quaternary Period, and the volume of water stored in the world's ice may be accounted for partly by a contemporaneous increase in water content of the land masses of earth. The assumption required is that precipitation upon the continents has increased and has caused a general rise in water tables of some hundreds of metres. © 1969.
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页码:237 / &
相关论文
共 3 条
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Fairbridge R.W., 1961, PHYS CHEM EARTH, V4, P99, DOI DOI 10.1016/0079-1946(61)90004-0
[2]  
Todd D.K., 1959, GROUNDWATER HYDROLOG, V1st ed.
[3]  
Zeuner F.E., 1959, PLEISTOCENE PERIOD