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
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
收藏
页码:1398 / 1400
页数:3
相关论文
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