Persistence of mantle lithospheric Re–Os signature during asthenospherization of the subcontinental...
Persistence of mantle lithospheric Re–Os signature during asthenospherization of the subcontinental lithospheric mantle: insights from in situ isotopic analysis of sulfides from the Ronda peridotite (Southern Spain)
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Publisher
Berlin/Heidelberg: Springer-Verlag
Journal title
Language
English
Formats
Publication information
Publisher
Berlin/Heidelberg: Springer-Verlag
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Scope and Contents
Contents
The western part of the Ronda peridotite massif (Southern Spain) consists mainly of highly foliated spinel-peridotite tectonites and undeformed granular peridotites that are separated by a recrystallization front. The spinel tectonites are interpreted as volumes of ancient subcontinental lithospheric mantle and the granular peridotites as a portion...
Alternative Titles
Full title
Persistence of mantle lithospheric Re–Os signature during asthenospherization of the subcontinental lithospheric mantle: insights from in situ isotopic analysis of sulfides from the Ronda peridotite (Southern Spain)
Authors, Artists and Contributors
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Record Identifier
TN_cdi_hal_primary_oai_HAL_hal_00564508v1
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_00564508v1
Other Identifiers
ISSN
0010-7999
E-ISSN
1432-0967
DOI
10.1007/s00410-009-0429-y
