STRUCTURE AND GROWTH-MECHANISM OF GLAUCONITE AS SEEN BY HIGH-RESOLUTION TRANSMISSION ELECTRON-MICROSCOPY

被引：53

作者：

AMOURIC, M

PARRON, C

机构：

[1] FAC SCI ST JEROME,GEOL DYNAM LAB,F-13397 MARSEILLE 13,FRANCE

[2] FAC SCI ST JEROME,CNRS,LAB 132,F-13397 MARSEILLE 13,FRANCE

来源：

CLAYS AND CLAY MINERALS | 1985年 / 33卷 / 06期

关键词：

D O I：

10.1346/CCMN.1985.0330601

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：

引用

页码：473 / 482

页数：10

共 41 条

[31]

PAULUS M, 1975, CLAYS CLAY MINERALS, V20, P193

[32] TRANSMISSION ELECTRON-MICROSCOPY OF FINE-GRAINED PHYLLOSILICATES IN ULTRA-THIN ROCK SECTIONS [J].

PHAKEY, PP ;

OERTEL, G ;

CURTIS, CD .

CLAYS AND CLAY MINERALS, 1972, 20 (04) :193-&

[33]

Porrenga D.H., 1976, MAR GEOL, V5, P495, DOI [10.1016/0025-3227(67)90056-4, DOI 10.1016/0025-3227(67)90056-4]

[34]

TCHOUBAR C, 1973, J MICROSC-PARIS, V18, P147

[35] MINERALOGY OF GLAUCONITE [J].

THOMPSON, GR ;

HOWER, J .

CLAYS AND CLAY MINERALS, 1975, 23 (04) :289-300

[36] FURTHER INFORMATION RELATED TO ORIGIN OF GLAUCONITE [J].

VELDE, B ;

ODIN, GS .

CLAYS AND CLAY MINERALS, 1975, 23 (05) :376-381

[37] CHEMICAL EVOLUTION OF GLAUCONITE PELLETS AS SEEN BY MICROPROBE DETERMINATIONS [J].

VELDE, B .

MINERALOGICAL MAGAZINE, 1976, 40 (315) :753-760

[38]

WARSHAW CM, 1957, THESIS PENNSYLVANIA

[39]

WERMUND EG, 1961, B AM ASS PETROL GEOL, V45, P1667

[40]

WISE WS, 1964, AM MINERAL, V49, P1031

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