Source:http://linkedlifedata.com/resource/pubmed/id/12947196
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rdf:type | |
lifeskim:mentions | |
pubmed:issue |
5637
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pubmed:dateCreated |
2003-8-29
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pubmed:abstractText |
One of the principal means of understanding upper mantle dynamics involves inferring mantle flow directions from seismic anisotropy under the assumption that the seismic fast direction (olivine a axis) parallels the regional flow direction. We demonstrate that (i) the presence of melt weakens the alignment of a axes and (ii) when melt segregates and forms networks of weak shear zones, strain partitions between weak and strong zones, resulting in an alignment of a axes 90 degrees from the shear direction in three-dimensional deformation. This orientation of a axes provides a new means of interpreting mantle flow from seismic anisotropy in partially molten deforming regions of Earth.
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pubmed:commentsCorrections | |
pubmed:language |
eng
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pubmed:journal | |
pubmed:status |
PubMed-not-MEDLINE
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pubmed:month |
Aug
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pubmed:issn |
1095-9203
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pubmed:author | |
pubmed:issnType |
Electronic
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pubmed:day |
29
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pubmed:volume |
301
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pubmed:owner |
NLM
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pubmed:authorsComplete |
Y
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pubmed:pagination |
1227-30
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pubmed:dateRevised |
2007-3-19
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pubmed:year |
2003
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pubmed:articleTitle |
Melt segregation and strain partitioning: implications for seismic anisotropy and mantle flow.
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pubmed:affiliation |
Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. holtz007@umn.edu
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pubmed:publicationType |
Journal Article
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