Chemistry:Sericitic alteration
From HandWiki
Short description: Process of mineral alteration
 | This article relies largely or entirely on a single source. (May 2026) |
Sericitic alteration or sericitization is a type of hydrothermal alteration characterized by the development of fine-grained white mica assemblages collectively referred to as sericite. In the Buchans–Roberts Arm Belt of Newfoundland, these assemblages include muscovitic illite, phengite, and paragonite associated with hydrothermal alteration zones.[1]
References
- ↑ Sparkes, G.W. (2022). Short wavelength infrared spectrometry studies of sericitic alteration zones, southern Buchans–Roberts Arm Belt, Newfoundland (Current Research). Newfoundland and Labrador Department of Industry, Energy and Technology. pp. 85–118. 22-1. https://www.gov.nl.ca/em/files/CurrentResearch_Sparkes_2022.pdf. Retrieved 2026-05-08.
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