洋脊裂谷与上涌流动

IMECH-IR > 力学所知识产出(1956-2008)

	洋脊裂谷与上涌流动
	李荫亭; 关德相; 薛恩
Source Publication	科学通报
	1979
Volume	24 Issue:18 Pages:850-852
ISSN	0023-074X
Abstract	<正> 洋脊中轴裂谷是板块的创生边界,多年来一直吸引着地球科学家的注意。但是,对于中轴裂谷的成因,至今没有得到圓满的解释。本文利用我们在文献[1]中所提出的上涌流动模式,算出了裂谷的深度和宽度、裂谷内底宽度等。这些结果均与观测数据符合,从而给出了洋脊中轴裂谷地形的动力学解释。
Keyword	流动模式洋脊动力学解释观测数据科学家文献地球粘性剪切大洋中脊
Language	中文
Document Type	期刊论文
Identifier	http://dspace.imech.ac.cn/handle/311007/38696
Collection	力学所知识产出(1956-2008)
Corresponding Author	李荫亭
Recommended Citation GB/T 7714	李荫亭,关德相,薛恩. 洋脊裂谷与上涌流动[J]. 科学通报,1979,24,18,:850-852.
APA	李荫亭,关德相,&薛恩.(1979).洋脊裂谷与上涌流动.科学通报,24(18),850-852.
MLA	李荫亭,et al."洋脊裂谷与上涌流动".科学通报 24.18(1979):850-852.

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