KEY TO SOURCES OF PLIOCENE AND PLEISTOCENE GLACIATION IS AT BOTTOM OF BARENTS SEA

被引:18
作者
KVASOV, DD
BLAZHCHISHIN, AI
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D O I
10.1038/273138a0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
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页码:138 / 140
页数:3
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共 24 条
[1]  
[Anonymous], CLIMATIC FLUCTUATION
[2]  
[Anonymous], 1974, J GLACIOL, DOI DOI 10.3189/S0022143000023327
[3]  
ASTAKHOV VI, 1976, DOKL AKAD NAUK SSSR+, V231, P1178
[4]  
Berggren W. A., 1972, INITIAL REPORTS DEEP, VXII, P953
[5]  
BLAZHCHISHIN AI, 1977, DOKL AKAD NAUK SSSR+, V236, P696
[6]  
GRICHUK V P, 1971, Pollen et Spores, V13, P101
[7]  
Herman Y., 1974, MARINE GEOLOGY OCEAN, P283, DOI DOI 10.1007/978-3-642-87411-6_13
[8]   WAS THERE A LATE-WURM ARCTIC ICE SHEET [J].
HUGHES, T ;
DENTON, GH ;
GROSSWALD, MG .
NATURE, 1977, 266 (5603) :596-602
[9]  
KVASOV DD, 1966, B MOSKOW SOC NATUR G, P99
[10]  
KVASOV DD, QUAT RES