Cogenetic Origin of Magmatic Enclaves in Peralkaline Felsic Volcanic Rocks from the Sanshui Basin, South China
Centimeter-scale magmatic enclaves are abundant in peralkaline felsic volcanic rocks in the Sanshui Basin. Their lithology is mainly syenite and syenitic porphyry, and they mainly comprise alkali feldspar and amphibole, which is similar to the mineral assemblage of the host trachyte and comendite. T...
Main Authors: | Peijia Chen, Bo Qian, Zhiwei Zhou, Nianqiao Fang |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2023-04-01
|
Series: | Minerals |
Subjects: | |
Online Access: | https://www.mdpi.com/2075-163X/13/5/590 |
Similar Items
-
Peralkaline Felsic Magmatism of the Atlantic Islands
by: Adam J. Jeffery, et al.
Published: (2018-11-01) -
Geochemical Insights from Clinopyroxene Phenocrysts into the Magma Evolution of an Alkaline Magmatic System from the Sanshui Basin, South China
by: Peijia Chen, et al.
Published: (2021-11-01) -
Post-Mineralization, Cogenetic Magmatism at the Sungun Cu-Mo Porphyry Deposit (Northwest Iran): Protracted Melting and Extraction in an Arc System
by: Amin Allah Kamali, et al.
Published: (2018-12-01) -
Geology and Chemical Characterization of the Ultrapotassic Peralkaline Magmatism of the Manaíra-Princesa Isabel Dike Swarm, Borborema Provine
by: Maria Helena Bezerra Maia de Hollanda, et al.
Published: (2009-10-01) -
Magmatic Processes at Euganean Hills (Veneto Volcanic Province, Italy): Clinopyroxene Investigation to Unravel Magmatic Interactions
by: Sabrina Nazzareni, et al.
Published: (2022-02-01)