Standard
Harvard
Murphy, MD, Sparks, RSJ, Barclay, J, Carroll, MR, Lejeune, A-M, Brewer, TS
, MacDonald, R, Black, S & Young, S 1998, '
The role of magma mixing in triggering the current eruption at the Soufriere Hills Volcano, Montserrat, West Indies.',
Geophysical Research Letters, vol. 25, no. 18, pp. 3433-3436. <
http://www.agu.org/pubs/crossref/1998/98GL00713.shtml>
APA
Murphy, M. D., Sparks, R. S. J., Barclay, J., Carroll, M. R., Lejeune, A-M., Brewer, T. S.
, MacDonald, R., Black, S., & Young, S. (1998).
The role of magma mixing in triggering the current eruption at the Soufriere Hills Volcano, Montserrat, West Indies. Geophysical Research Letters,
25(18), 3433-3436.
http://www.agu.org/pubs/crossref/1998/98GL00713.shtmlVancouver
Author
Bibtex
@article{9fa2d715426b451a859c2d91e08abc58,
title = "The role of magma mixing in triggering the current eruption at the Soufriere Hills Volcano, Montserrat, West Indies.",
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 andesite. The andesite 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.",
author = "Murphy, {M. D.} and Sparks, {R. S. J.} and J. Barclay and Carroll, {M. R.} and A.-M. Lejeune and Brewer, {T. S.} and Raymond MacDonald and Stuart Black and S. Young",
year = "1998",
language = "English",
volume = "25",
pages = "3433--3436",
journal = "Geophysical Research Letters",
issn = "0094-8276",
publisher = "John Wiley & Sons, Ltd",
number = "18",
}
RIS
TY - JOUR
T1 - The role of magma mixing in triggering the current eruption at the Soufriere Hills Volcano, Montserrat, West Indies.
AU - Murphy, M. D.
AU - Sparks, R. S. J.
AU - Barclay, J.
AU - Carroll, M. R.
AU - Lejeune, A.-M.
AU - Brewer, T. S.
AU - MacDonald, Raymond
AU - Black, Stuart
AU - Young, S.
PY - 1998
Y1 - 1998
N2 - 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 andesite. The andesite 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.
AB - 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 andesite. The andesite 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.
M3 - Journal article
VL - 25
SP - 3433
EP - 3436
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 18
ER -
