DIFFRACTOMETRIC CLAY MINERAL ANALYSIS OF RECENT SEDIMENTS OF LAKE CONSTANCE (CENTRAL EUROPE)

被引：8

作者：

MULLER, G

QUAKERNA.J

机构：

[1] Lab. f. Sedimentforschung, Heidelberg, 6900

来源：

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY | 1969年 / 22卷 / 04期

关键词：

D O I：

10.1007/BF00400125

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：

Mica, smectite, and chlorite are the characteristic clay minerals in about 120 Recent sediment samples of Lake Constance as shown by semiquantitative clay mineral analysis. Interstratified clay minerals are practically absent, kandites were not found. The decrease of the smectite/mica ratio from West to East is apparently due to the dominance of the mica-chlorite assemblage of the Rhine river derived from the northern Alps in the eastern part of the lake. With increasing distance from the delta of the Rhine river, the Tertiary Molasse clay minerals (mainly mica and smectite) derived from rocks surrounding the lake become more abundant. © 1969 Springer-Verlag.

引用

页码：268 / &

共 22 条

[1]

BRINDLEY G. W., 1966, Clay Mineralogy, V6, P237, DOI 10.1180/claymin.1966.006.4.01

[2]

Forstner U, 1968, NEUES JB MINER ABH, V109, P33

[3]

FUCHTBAUER H, 1958, ECLOGAE GEOL HELV, V51, P928

[4]

Fuchtbauer H, 1964, ECLOGAE GEOL HELV, V57, P157, DOI DOI 10.5169/SEALS-163140

[5]

HARWARD ME, 1966, CLAYS CLAY MINERALS, V25, P209

[6]

HOFMANN F, 1959, ECLOGAE GEOL HELV, V52, P461

[7]

HOFMANN F, 1959, SCHWEIZ MINERAL PETR, V39, P115

[8]

HOFMANN F, 1961, ECLOGAE GEOL HELV, V54, P133

[9]

KITTRICK J. A., 1960, SOIL SCI SOC AMER PROC, V24, P17

[10]

Lemcke K., 1953, BEIH GEOL JAHRB, V11, P1

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