ISOTOPE COMPOSITION OF STRONTIUM FROM INTERSTITIAL WATERS SQUEEZED FROM RECENT SEDIMENTS - ARGUMENT IN FAVOR OF ISOTOPIC HOMOGENIZATION OF CLAY-MINERALS

被引：15

作者：

CLAUER, N

HOFFERT, M

GRIMAUD, D

MILLOT, G

机构：

[1] UNIV LOUIS PASTEUR, INST GEOL,CNRS,CTR SEDIMENTOL & GEOCHIM SURFACE, 1 RUE BLESSIG, 67084 STRASBOURG, FRANCE

[2] UNIV PARIS 7, LAB GEOCHIM EAUX, 2 PL JUSSIEU, 75221 PARIS, FRANCE

来源：

关键词：

D O I：

10.1016/0016-7037(75)90162-3

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

页码：1579 / 1582

页数：4

共 13 条

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[2]

ARRHENIUS G, 1963, SEA, V3, P655

[3]

BONHOMME M, 1966, P INT CLAY C, V1, P121

[4]

BONHOMME MG, 1972, MEM BUR RECH GEOL MI, V77, P943

[5]

BONHOMME MG, 1966, 151 INT C CNRS NANC, P541

[6] TRACE ELEMENTS IN INTERSTITIAL WATERS OF MARINE SEDIMENTS [J].

BROOKS, RK ;

PRESLEY, BJ ;

KAPLAN, IR .

[7]

CLAUER N, 1973, GEOCHIM COSMOCHIM AC, V37, P2243

[8]

HOFMANN A, 1972, REP DIR GEOPHYS LAB, P563

[9]

LUCAS J, 1962, TRANSFORMATION CLAY

[10]

Millot G., 1964, GEOLOGIE DES ARGILES