THERMAL-CONDUCTIVITY VARIATION IN A DEEP-SEA SEDIMENT CORE AND ITS RELATION TO H2O, CA AND SI CONTENT

被引：11

作者：

MATSUDA, JI ^{[1
]}

VONHERZEN, RP ^{[1
]}

机构：

[1] WOODS HOLE OCEANOG INST,WOODS HOLE,MA 02543

来源：

DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS | 1986年 / 33卷 / 02期

关键词：

D O I：

10.1016/0198-0149(86)90116-0

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

引用

页码：165 / &

共 16 条

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[3] THE FLOW OF HEAT THROUGH THE FLOOR OF THE ATLANTIC OCEAN [J].

BULLARD, EC ;

DAY, A .

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[4]

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[5]

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[6]

HAYS JD, 1969, GEOL SOC AM BULL, V80, P1481, DOI 10.1130/0016-7606(1969)80[1481:PSOTEP]2.0.CO

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[8]

HAYS JD, 1972, INIT REPTS DSDP, V9, P909

[9]

HORAI K, 1981, INITIAL REPORTS DEEP, V60, P807

[10]

Hyndman R.D, 1974, INITIAL REPORTS DEEP, V26, P451

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