OXYGEN ISOTOPIC COMPOSITION OF FRACTION LESS THAN 2 MICRONS (CLAY FRACTION) IN RECENT SEDIMENTS FROM WESTERN-EUROPE

被引：10

作者：

SALOMONS, W

HOFMAN, P

BOELENS, R

MOOK, WG

机构：

[1] UNIV GRONINGEN,LAB INORG CHEM,GRONINGEN,NETHERLANDS

[2] UNIV GRONINGEN,PHYS LAB,GRONINGEN,NETHERLANDS

来源：

MARINE GEOLOGY | 1975年 / 18卷 / 02期

关键词：

D O I：

10.1016/0025-3227(75)90036-5

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：M23 / M28

页数：6

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[2]

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[3]

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[4]

Goldberg E.D., 1973, N SEA SCI, P75

[5] HYDROGEN AND OXYGEN ISOTOPE SYSTEMATICS IN WEATHERING PROFILES [J].

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TAYLOR, HP .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1972, 36 (12) :1377-&

[6]

MEADE RH, 1969, J SEDIMENT PETROL, V39, P222

[7]

Mook W. G., 1973, International Journal of Mass Spectrometry and Ion Physics, V12, P273, DOI 10.1016/0020-7381(73)80044-0

[8]

POSTMA H, 1967, 83 AM ASS ADV SCI PU, P158

[9]

SALOMONS W, 1974, CHEMICAL ISOTOPIC CO

[10] OXYGEN AND HYDROGEN ISOTOPE GEOCHEMISTRY OF OCEAN SEDIMENTS AND SHALES [J].

SAVIN, SM ;

EPSTEIN, S .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1970, 34 (01) :43-&

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