2019
DOI: 10.1007/s12040-019-1197-3
|View full text |Cite
|
Sign up to set email alerts
|

Evolution of fluid from the ultrahigh temperature lower crust to shallower levels: Constraints from silicate–oxide–sulphide–sulphate assemblages of mafic granulites of the Eastern Ghats Belt, India

Abstract: Mafic granulites from key localities of the Eastern Ghats Province preserve Fe-Ti oxides, Cu-Fe sulphides and traces of sulphate minerals along with silicate phases. Two different varieties of mafic granulite exhibit slightly contrasting mineral assemblages. While the massive type of mafic granulite contains minerals assemblage orthopyroxene + clinopyroxene + plagioclase + magnetite + ilmenite + pyrite + pyrrhotite, the migmatitic variety contains garnet as an additional phase. Both oxide and sulphide minerals… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...

Citation Types

0
0
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
5

Relationship

0
5

Authors

Journals

citations
Cited by 6 publications
references
References 139 publications
(184 reference statements)
0
0
0
Order By: Relevance