EXCESS HE-3 AND HE-4 IN GALAPAGOS SUBMARINE HYDROTHERMAL WATERS

被引:178
作者
JENKINS, WJ
EDMOND, JM
CORLISS, JB
机构
[1] MIT,DEPT EARTH & PLANETARY PHYS,CAMBRIDGE,MA 02139
[2] OREGON STATE UNIV,DEPT OCEANOG,CORVALLIS,OR 97330
关键词
D O I
10.1038/272156a0
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 ;
摘要
SINCE the discovery of excess 3He in Pacific deep waters 1, it has been argued that the source of this anomaly is the mid-depth injection of primordial helium from seafloor spreading centres 1,2. This hypothesis is consistent with the spatial distribution of excess 3He in the deep waters3-5, its presence in the glassy (rapidly quenched) margins of extruded ocean basalts6,7, and the detection of a large 3He excess in a 'thermal plume' (thermal anomaly ∼0.1 °C, sampled using a deep-tow sled) over the Galapagos Spreading Centre8-10. In this report, we summarise 37 measurements of excess helium in hydrothermal waters sampled using the Alvin deep submersible at the Galapagos Spreading Centre during February and March of 1977. © 1978 Nature Publishing Group.
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页码:156 / 158
页数:3
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