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Isotope disequilibrium studies and magmatic processes

Abstract:

Subsurface crystallisation and degassing significantly influence the evolution and eruption of magmas. Both processes are inevitable consequences of the residence of magma in shallow reservoirs, and both obscure the nature of the pristine liquids derived from the melting region. However, the signatures of crystallisation and degassing, and the very act of being stored, can be recognized under suitable conditions in the signature of the various decay-chain products of the isotopes 238U and 232...

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Journal:
Geoscientist
Volume:
4
Issue:
3
Pages:
18-20
Publication date:
1994-01-01
Source identifiers:
165101
Language:
English
Pubs id:
pubs:165101
UUID:
uuid:8a6ebc30-09f2-4c50-8140-a4d059257474
Local pid:
pubs:165101
Deposit date:
2013-02-20

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