Abstract

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.

Original languageEnglish (US)
Pages (from-to)1398-1400
Number of pages3
JournalScience
Volume206
Issue number4425
StatePublished - 1979

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talc
mineral
inosilicate
lizardite
antigorite
asbestos
amphibole
mixed layer
chlorite
transmission electron microscopy
silicate

ASJC Scopus subject areas

  • General

Cite this

Serpentine minerals : Intergrowths and new combination structures. / Veblen, David R.; Buseck, P R.

In: Science, Vol. 206, No. 4425, 1979, p. 1398-1400.

Research output: Contribution to journalArticle

Veblen, DR & Buseck, PR 1979, 'Serpentine minerals: Intergrowths and new combination structures', Science, vol. 206, no. 4425, pp. 1398-1400.
Veblen, David R. ; Buseck, P R. / Serpentine minerals : Intergrowths and new combination structures. In: Science. 1979 ; Vol. 206, No. 4425. pp. 1398-1400.
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