Geophysical Study of the Easternmost Walvis Ridge, South Atlantic: Morphology and Shallow Structure

J. GOSLIN; J. MASCLE; J. C. SIBUET; H. HOSKINS

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Geophysical Study of the Easternmost Walvis Ridge, South Atlantic: Morphology and Shallow Structure

机译：南大西洋最东部的沃尔维斯山脊的地球物理研究：形态学和浅层结构

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The landward termination of Walvis Ridge consists of two east-trending basement ridges of probable basaltic composition enclosing a relatively important sedimentary basin. East of long. 10° E., the southern ridge disappears under the sediments of the continental margin.

机译：沃尔维斯山脊的陆上终结点由两个可能具有玄武岩成分的东向基底脊组成，围成一个相对重要的沉积盆地。东长。 10° E。，南脊消失在大陆边缘的沉积物之下。

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《GSA Bulletin 》 |1974年第4期| 619-632| 共14页
作者
J. GOSLIN; J. MASCLE; J. C. SIBUET; H. HOSKINS;
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作者单位

Centre National pour l'Exploitation des Océans, Centre Océanologique de Bretagne, Boite Postale 337, 29.273 Brest Cedex, france;

Centre National pour l'Exploitation des Océans, Centre Océanologique de Bretagne, Boite Postale 337, 29.273 Brest Cedex, france;

Centre National pour l'Exploitation des Océans, Centre Océanologique de Bretagne, Boite Postale 337, 29.273 Brest Cedex, france;

Woods Hole Oceanographic Instituion, Woods Hole, Massachusetts 02543;

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7. Geophysical study of the easternmost Walvis Ridge, South Atlantic: Deep structure [O] . J. GOSLIN, J. C. SIBUET 1975

机译：南大西洋东部沃尔维斯岭的地球物理研究：深层结构

Geophysical Study of the Easternmost Walvis Ridge, South Atlantic: Morphology and Shallow Structure

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