Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma

Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Petford, Nick, Gallagher, Kerry
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2001
Subjects:
Earth systems and environmental sciences
granites models
partial melting
amphibolites
granite
magmas
models
periodicity
layered intrusions
continental-crust
Antarctic peninsula
subduction zone
heat-flow
generation
model
batholith
origin
geochemistry
system
Antarctic
Antarctic Peninsula
Antarc*
Online Access:https://eprints.kingston.ac.uk/id/eprint/686/
https://doi.org/10.1016/S0012-821X(01)00481-2
id ftunivkingston:oai:eprints.kingston.ac.uk:686
record_format openpolar
spelling ftunivkingston:oai:eprints.kingston.ac.uk:686 2023-05-15T13:34:31+02:00 Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma Petford, Nick Gallagher, Kerry 2001-12-15 https://eprints.kingston.ac.uk/id/eprint/686/ https://doi.org/10.1016/S0012-821X(01)00481-2 unknown Elsevier Petford, Nick and Gallagher, Kerry (2001) Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma. Earth and Planetary Science Letters, 193(3-4), pp. 483-499. ISSN (print) 0012-821X Earth systems and environmental sciences granites models partial melting amphibolites granite magmas models periodicity layered intrusions continental-crust Antarctic peninsula subduction zone heat-flow generation model batholith origin geochemistry system Article PeerReviewed 2001 ftunivkingston https://doi.org/10.1016/S0012-821X(01)00481-2 2022-02-22T09:01:30Z Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Kingston University London: Research Repository Antarctic Antarctic Peninsula Earth and Planetary Science Letters 193 3-4 483 499
institution Open Polar
collection Kingston University London: Research Repository
op_collection_id ftunivkingston
language unknown
topic Earth systems and environmental sciences
granites models
partial melting
amphibolites
granite
magmas
models
periodicity
layered intrusions
continental-crust
Antarctic peninsula
subduction zone
heat-flow
generation
model
batholith
origin
geochemistry
system
spellingShingle Earth systems and environmental sciences
granites models
partial melting
amphibolites
granite
magmas
models
periodicity
layered intrusions
continental-crust
Antarctic peninsula
subduction zone
heat-flow
generation
model
batholith
origin
geochemistry
system
Petford, Nick
Gallagher, Kerry
Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma
topic_facet Earth systems and environmental sciences
granites models
partial melting
amphibolites
granite
magmas
models
periodicity
layered intrusions
continental-crust
Antarctic peninsula
subduction zone
heat-flow
generation
model
batholith
origin
geochemistry
system
format Article in Journal/Newspaper
author Petford, Nick
Gallagher, Kerry
author_facet Petford, Nick
Gallagher, Kerry
author_sort Petford, Nick
title Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma
title_short Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma
title_full Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma
title_fullStr Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma
title_full_unstemmed Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma
title_sort partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma
publisher Elsevier
publishDate 2001
url https://eprints.kingston.ac.uk/id/eprint/686/
https://doi.org/10.1016/S0012-821X(01)00481-2
geographic Antarctic
Antarctic Peninsula
geographic_facet Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
genre_facet Antarc*
Antarctic
Antarctic Peninsula
op_relation Petford, Nick and Gallagher, Kerry (2001) Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma. Earth and Planetary Science Letters, 193(3-4), pp. 483-499. ISSN (print) 0012-821X
op_doi https://doi.org/10.1016/S0012-821X(01)00481-2
container_title Earth and Planetary Science Letters
container_volume 193
container_issue 3-4
container_start_page 483
op_container_end_page 499
_version_ 1766053840949346304

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