Discrimination of Clinozoisite–Epidote Series by Raman Spectroscopy: An application to Bengal Fan Turbidites (IODP Expedition 354)
Epidote group minerals are one of the three most abundant kinds of heavy minerals in orogenic sediments, the other two being amphibole and garnet. They resist diagenesis better than amphibole and resist weathering in soils better than garnet. Their chemical composition and optical properties vary ma...
Main Authors: | Mara Limonta, Sergio Andò, Danilo Bersani, Eduardo Garzanti |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2022-12-01
|
Series: | Geosciences |
Subjects: | |
Online Access: | https://www.mdpi.com/2076-3263/12/12/442 |
Similar Items
-
A summary of the variations in relative abundance of the lanthanides and yttrium in allanites and epidotes
by: M. Fleischer
Published: (1985-12-01) -
Freiherr Sigmund Zois, Zoisit und Karinthin (Zum 250. Jahrestag seiner Geburt)
by: Ernest Faninger
Published: (1999-12-01) -
Zoisite-(Pb), a New Orthorhombic Epidote-Related Mineral from the Jakobsberg Mine, Värmland, Sweden, and Its Relationships with Hancockite
by: Natale Perchiazzi, et al.
Published: (2021-12-01) -
Continental Growth and Recycling in Convergent Orogens with Large Turbidite Fans on Oceanic Crust
by: Ben D. Goscombe, et al.
Published: (2013-07-01) -
Cause of Color Modification in Tanzanite after Heat Treatment
by: Teerarat Pluthametwisute, et al.
Published: (2020-08-01)