Serpentine–Hisingerite Solid Solution in Altered Ferroan Peridotite and Olivine Gabbro

We present microanalyses of secondary phyllosilicates in altered ferroan metaperidotite, containing approximately equal amounts of end-members serpentine ((Mg,Fe2+)3Si2O5(OH)4) and hisingerite (□Fe3+2Si2O5(OH)4·nH2O). These analyses suggest that all intermediate compositions can exist sta...

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Bibliographic Details
Main Authors: Benjamin M. Tutolo, Bernard W. Evans, Scott M. Kuehner
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Minerals
Subjects:
Online Access:http://www.mdpi.com/2075-163X/9/1/47