THE PALEOMAGNETIC FIELD FROM EQUATORIAL DEEP-SEA SEDIMENTS - AXIAL SYMMETRY AND POLARITY ASYMMETRY

被引：27

作者：

SCHNEIDER, DA ^{[1
]}

KENT, DV ^{[1
]}

机构：

[1] COLUMBIA UNIV, DEPT GEOL SCI, NEW YORK, NY 10027 USA

来源：

SCIENCE | 1988年 / 242卷 / 4876期

关键词：

D O I：

10.1126/science.242.4876.252

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：

引用

页码：252 / 256

页数：5

共 26 条

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[5]

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[7] LOWER MANTLE HETEROGENEITY, DYNAMIC TOPOGRAPHY AND THE GEOID [J].

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CLAYTON, RW ;

RICHARDS, MA ;

COMER, RP ;

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LINDH, T .

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[9]

King R. F., 1955, GEOPHYSICAL SUPPLEME, V7, P115, DOI [10.1111/j.1365-246X.1955.tb06558.x, DOI 10.1111/J.1365-246X.1955.TB06558.X]

[10]

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