![Minerals | Free Full-Text | Deformation Processes, Textural Evolution and Weakening in Retrograde Serpentinites Minerals | Free Full-Text | Deformation Processes, Textural Evolution and Weakening in Retrograde Serpentinites](https://www.mdpi.com/minerals/minerals-08-00241/article_deploy/html/images/minerals-08-00241-g006.png)
Minerals | Free Full-Text | Deformation Processes, Textural Evolution and Weakening in Retrograde Serpentinites
Characterization of Serpentines from Different Regions by Transmission Electron Microscopy, X-ray Diffraction, BET Specific Surf
![Antigorite crystallization during oceanic retrograde serpentinization of abyssal peridotites | SpringerLink Antigorite crystallization during oceanic retrograde serpentinization of abyssal peridotites | SpringerLink](https://media.springernature.com/lw685/springer-static/image/art%3A10.1007%2Fs00410-019-1595-1/MediaObjects/410_2019_1595_Fig3_HTML.png)
Antigorite crystallization during oceanic retrograde serpentinization of abyssal peridotites | SpringerLink
![File:Chrysotile asbestos veins in serpentinized komatiite (Upper Komatiitic Unit, Kidd-Munro Assemblage, Neoarchean, 2.711-2.717 Ga; southwest of the Potter Mine, east of Timmins, Ontario, Canada) 5 (47835838352).jpg - Wikimedia Commons File:Chrysotile asbestos veins in serpentinized komatiite (Upper Komatiitic Unit, Kidd-Munro Assemblage, Neoarchean, 2.711-2.717 Ga; southwest of the Potter Mine, east of Timmins, Ontario, Canada) 5 (47835838352).jpg - Wikimedia Commons](https://upload.wikimedia.org/wikipedia/commons/d/dc/Chrysotile_asbestos_veins_in_serpentinized_komatiite_%28Upper_Komatiitic_Unit%2C_Kidd-Munro_Assemblage%2C_Neoarchean%2C_2.711-2.717_Ga%3B_southwest_of_the_Potter_Mine%2C_east_of_Timmins%2C_Ontario%2C_Canada%29_5_%2847835838352%29.jpg)
File:Chrysotile asbestos veins in serpentinized komatiite (Upper Komatiitic Unit, Kidd-Munro Assemblage, Neoarchean, 2.711-2.717 Ga; southwest of the Potter Mine, east of Timmins, Ontario, Canada) 5 (47835838352).jpg - Wikimedia Commons
![Figure 2.3 from The Logatchev Hydrothermal Field ( MAR , 15 ° N ) : High-and Low-Temperature Alteration of Ultramafic Oceanic Crust – Geology | Semantic Scholar Figure 2.3 from The Logatchev Hydrothermal Field ( MAR , 15 ° N ) : High-and Low-Temperature Alteration of Ultramafic Oceanic Crust – Geology | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/2be59b69a0bed8c5d8c427c539f40a4bfa03d2cb/41-Figure2.3-1.png)
Figure 2.3 from The Logatchev Hydrothermal Field ( MAR , 15 ° N ) : High-and Low-Temperature Alteration of Ultramafic Oceanic Crust – Geology | Semantic Scholar
![Spatial variations in antigorite fabric across a serpentinite subduction channel: Insights from the Ohmachi Seamount, Izu-Bonin frontal arc - ScienceDirect Spatial variations in antigorite fabric across a serpentinite subduction channel: Insights from the Ohmachi Seamount, Izu-Bonin frontal arc - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0012821X10005601-gr3.jpg)