volume 25, issue 18, P3433-3436 1998
DOI: 10.1029/98gl00713
View full text
|
|
Share

Abstract: Abstract. The andesite lava currently erupting at the Soufriere Hills volcano, Montserrat, contains ubiquitous mafic inclusions which show evidence of having been molten when incorporated into the andesire. The andesire phenocrysts have a range of textures and zonation patterns which suggest that non-uniform reheating of the magma occurred shortly before the current eruption. Reheating resulted in remobilisation of the resident magma and may have induced eruption.

Search citation statements

Order By: Relevance

Paper Sections

0
0
0
0
0

Citation Types

4
102
0
1

Publication Types

Select...

Relationship

0
0

Authors

Journals