Radioactivity and Earth Movements.

Radioactivity and Earth Movements.
复制标题

DOI:
10.1038/128496e0
复制
发表时间:
1931-09
期刊:
影响因子:
64.8
通讯作者:
A. Holmes
A. Holmes
中科院分区:
综合性期刊1区
文献类型:
--
作者:
A. Holmes

文献摘要

被引文献

相似文献

在我关于这个问题的格拉斯哥讲座的通知中(《自然》杂志,1931年9月5日,第419页)出现了这样一段话:“在其他有益的结论中,‘我们可以把太平洋的地壳看作和大陆的地壳一样’(第570页)。”由于我已经收到了几份证明这个所谓的“结论”的邀请,我想指出的是,我实际上写的是:“因此,我们可能认为太平洋地壳与大陆地壳相似,但辉长岩向下进入角闪岩,取代了硅质上层。”
IN a notice of my Glasgow lecture on this subject (NATURE, Sept. 5, 1931, p. 419) occurs the passage: “Amongst other instructive conclusions are that ‘we may regard the Pacific crust as being like that of the continents’ (p. 570)”. As I have already received several invitations to justify this alleged “conclusion” I wish to point out that what I actually wrote was: “we may therefore regard the Pacific crust as being like that of the continents, but with gabbro passing down into amphibolite in place of the sialic upper layer”.