GEOID ANOMALIES ACROSS ASCENSION FRACTURE-ZONE AND THE COOLING OF THE LITHOSPHERE

被引：10

作者：

GIBERT, D ^{[1
]}

CAMERLYNCK, C ^{[1
]}

COURTILLOT, V ^{[1
]}

机构：

[1] INST PHYS GLOBE, F-75232 PARIS 05, FRANCE

来源：

GEOPHYSICAL RESEARCH LETTERS | 1987年 / 14卷 / 06期

关键词：

D O I：

10.1029/GL014i006p00603

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

引用

页码：603 / 606

页数：4

共 23 条

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[2]

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[3] THERMAL COOLING OF THE OCEANIC LITHOSPHERE - NEW CONSTRAINTS FROM GEOID HEIGHT DATA [J].

CAZENAVE, A .

EARTH AND PLANETARY SCIENCE LETTERS, 1984, 70 (02) :395-406

[4] THERMAL PARAMETERS OF THE OCEANIC LITHOSPHERE ESTIMATED FROM GEOID HEIGHT DATA [J].

CAZENAVE, A ;

LAGO, B ;

DOMINH, K .

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[5] THE EXISTENCE OF A THIN LOW-VISCOSITY LAYER BENEATH THE LITHOSPHERE [J].

CRAIG, CH ;

MCKENZIE, D .

EARTH AND PLANETARY SCIENCE LETTERS, 1986, 78 (04) :420-426

[6] GEOID ANOMALIES ACROSS FRACTURE-ZONES AND THE THICKNESS OF THE LITHOSPHERE [J].

CROUGH, ST .

EARTH AND PLANETARY SCIENCE LETTERS, 1979, 44 (02) :224-230

[7] AN ANALYSIS OF GEOID ANOMALIES ACROSS THE MENDOCINO FRACTURE-ZONE - IMPLICATIONS FOR THERMAL MODELS OF THE LITHOSPHERE [J].

DETRICK, RS .

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[8] GRAVITATIONAL EDGE EFFECT [J].

DORMAN, LM .

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[9]

DRISCOLL M, 1986, EOS T AGU, V67, P364

[10]

FREEDMAN AP, 1986, EOS T AGU, V67, P371

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