Hungarian investigations on the ''Zempleni'' illite

被引：22

作者：

Viczian, I

机构：

[1] Hungarian Geological Inst, Budapest

来源：

CLAYS AND CLAY MINERALS | 1997年 / 45卷 / 01期

关键词：

HRTEM; Hungary; illite/smectite; K/Ar analysis; locality; TEM; X-ray;

D O I：

10.1346/CCMN.1997.0450114

中图分类号：

O64 [物理化学（理论化学）、化学物理学];

学科分类号：

070304 ; 081704 ;

摘要：

The `Zempleni' illite is a hydrothermal clay from Hungary. Zempleni is a the name of the mountain range located in northeast Hungary and is built almost exclusively of tertiary volcanics. Zempleni mountains is used mostly in the geographic and touristic literature. In geology, it is synonymous to the term Tokaj mountains.

引用

页码：114 / 115

页数：2

共 15 条

[1]

AHN JH, 1990, AM MINERAL, V75, P267

[2]

DODONY I, 1985, THESIS HUNGARIAN ACA

[3]

MATYAS E, 1979, 10 KAOL S GEN KAOL G

[4]

MATYAS E, 1979, FOLDT KOZL, V109, P488

[5] INTERSTRATIFIED CLAYS AS FUNDAMENTAL PARTICLES [J].

NADEAU, PH ;

WILSON, MJ ;

MCHARDY, WJ ;

TAIT, JM .

SCIENCE, 1984, 225 (4665) :923-925

[6]

Nemecz E., 1970, FOLDTANI KOZLONY, V100, P11

[7]

Nemecz E, 1981, CLAY MINERALS

[8]

Pecskay Z., 1986, GEOL CARPATH, V37, P635

[9]

Pecskay Z., 1987, FOLDTANI KOZLONY, V117, P237

[10] X-RAY-DIFFRACTION STUDIES OF ILLITE SMECTITE FROM ROCKS, LESS-THAN-OR-EQUAL-TO-1 MU-M RANDOMLY ORIENTED POWDERS, AND LESS-THAN-OR-EQUAL-TO-1 MU-M ORIENTED POWDER AGGREGATES - THE ABSENCE OF LABORATORY-INDUCED ARTIFACTS [J].

REYNOLDS, RC .

CLAYS AND CLAY MINERALS, 1992, 40 (04) :387-396

← 1 2 →