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
Issue number4425
StatePublished - Jan 1 1979

ASJC Scopus subject areas

  • General

Fingerprint Dive into the research topics of 'Serpentine minerals: Intergrowths and new combination structures'. Together they form a unique fingerprint.

Cite this