Magmatic processes in the Eastern Volcanic Zone of Iceland

Basaltic volcanism is an important consequence of mid-ocean ridge (MOR) spreading. On arrival in the crust and uppermost mantle, melts are processed in magma reservoirs prior to erup- tion, leading to geochemical signals of mantle melting being obscured by mixing, crystallisation and degassing proce...

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Main Author: Neave, David A.
Format: Thesis
Language:English
Published: 2014
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/3064/
http://eprints.esc.cam.ac.uk/3064/1/deave%20image1.png
http://eprints.esc.cam.ac.uk/3064/2/dneave_thesis.pdf
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spelling ftucambridgeesc:oai:eprints.esc.cam.ac.uk:3064 2023-05-15T16:48:16+02:00 Magmatic processes in the Eastern Volcanic Zone of Iceland Neave, David A. 2014-06 image text http://eprints.esc.cam.ac.uk/3064/ http://eprints.esc.cam.ac.uk/3064/1/deave%20image1.png http://eprints.esc.cam.ac.uk/3064/2/dneave_thesis.pdf en eng http://eprints.esc.cam.ac.uk/3064/1/deave%20image1.png http://eprints.esc.cam.ac.uk/3064/2/dneave_thesis.pdf Neave, David A. (2014) Magmatic processes in the Eastern Volcanic Zone of Iceland. PhD thesis, University of Cambridge. cc_by CC-BY 05 - Petrology - Igneous Metamorphic and Volcanic Studies Thesis NonPeerReviewed 2014 ftucambridgeesc 2020-08-27T18:09:33Z Basaltic volcanism is an important consequence of mid-ocean ridge (MOR) spreading. On arrival in the crust and uppermost mantle, melts are processed in magma reservoirs prior to erup- tion, leading to geochemical signals of mantle melting being obscured by mixing, crystallisation and degassing processes. In order to use the compositions of primitive crystals to interrogate both mantle melting and magma reservoir processes, it is thus important to understand not only how crystals relate to the melt in which they are erupted, but the relationships between indi- vidual compositional zones within crystals. Thesis Iceland University of Cambridge, Department of Earth Sciences: ESC Publications
institution Open Polar
collection University of Cambridge, Department of Earth Sciences: ESC Publications
op_collection_id ftucambridgeesc
language English
topic 05 - Petrology - Igneous
Metamorphic and Volcanic Studies
spellingShingle 05 - Petrology - Igneous
Metamorphic and Volcanic Studies
Neave, David A.
Magmatic processes in the Eastern Volcanic Zone of Iceland
topic_facet 05 - Petrology - Igneous
Metamorphic and Volcanic Studies
description Basaltic volcanism is an important consequence of mid-ocean ridge (MOR) spreading. On arrival in the crust and uppermost mantle, melts are processed in magma reservoirs prior to erup- tion, leading to geochemical signals of mantle melting being obscured by mixing, crystallisation and degassing processes. In order to use the compositions of primitive crystals to interrogate both mantle melting and magma reservoir processes, it is thus important to understand not only how crystals relate to the melt in which they are erupted, but the relationships between indi- vidual compositional zones within crystals.
format Thesis
author Neave, David A.
author_facet Neave, David A.
author_sort Neave, David A.
title Magmatic processes in the Eastern Volcanic Zone of Iceland
title_short Magmatic processes in the Eastern Volcanic Zone of Iceland
title_full Magmatic processes in the Eastern Volcanic Zone of Iceland
title_fullStr Magmatic processes in the Eastern Volcanic Zone of Iceland
title_full_unstemmed Magmatic processes in the Eastern Volcanic Zone of Iceland
title_sort magmatic processes in the eastern volcanic zone of iceland
publishDate 2014
url http://eprints.esc.cam.ac.uk/3064/
http://eprints.esc.cam.ac.uk/3064/1/deave%20image1.png
http://eprints.esc.cam.ac.uk/3064/2/dneave_thesis.pdf
genre Iceland
genre_facet Iceland
op_relation http://eprints.esc.cam.ac.uk/3064/1/deave%20image1.png
http://eprints.esc.cam.ac.uk/3064/2/dneave_thesis.pdf
Neave, David A. (2014) Magmatic processes in the Eastern Volcanic Zone of Iceland. PhD thesis, University of Cambridge.
op_rights cc_by
op_rightsnorm CC-BY
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