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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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 |
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University of Cambridge, Department of Earth Sciences: ESC Publications |
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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. |
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cc_by |
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CC-BY |
_version_ |
1766038377614802944 |