SERPENTINE MINERALS - INTERGROWTHS AND NEW COMBINATION STRUCTURES

被引：87

作者：

VEBLEN, DR ^{[1
]}

BUSECK, PR ^{[1
]}

机构：

[1] ARIZONA STATE UNIV,DEPT CHEM,TEMPE,AZ 85281

来源：

SCIENCE | 1979年 / 206卷 / 4425期

关键词：

D O I：

10.1126/science.206.4425.1398

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

The serpentine minerals chrysotile, lizardite, and antigorite have been found intimately intergrown with each other and with talc, chlorite, and amphibole in incompletely reacted chain silicates. High-resolution transmission electron microscopy has revealed new variations in serpentine planar and roll structures, as well as regions of mixed-layer silicate consisting of serpentine and talc layers.

引用

页码：1398 / 1400

页数：3

共 24 条

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