Journal article icon

Journal article

Porosity-driven convection and asymmetry beneath mid-ocean ridges

Abstract:

Seismic tomography of the asthenosphere beneath mid-ocean ridges has produced images of wave speed and anisotropy that are asymmetric across the ridge axis. These features have been interpreted as resulting from an asymmetric distribution of upwelling and melting. Using computational models of coupled magma/mantle dynamics beneath mid-ocean ridges, I show that such asymmetry should be expected if buoyancy forces contribute to mantle upwelling beneath ridges. The sole source of buoyancy consid...

Expand abstract
Publication status:
Published

Actions


Access Document


Publisher copy:
10.1029/2010GC003282

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Journal:
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Volume:
11
Issue:
11
Pages:
n/a-n/a
Publication date:
2010-11-10
DOI:
EISSN:
1525-2027
ISSN:
1525-2027
Language:
English
Keywords:
Pubs id:
pubs:103787
UUID:
uuid:c5028ed1-fd85-4455-9684-7caf87817406
Local pid:
pubs:103787
Source identifiers:
103787
Deposit date:
2012-12-19

Terms of use


Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP