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High P‐T Sound Velocities of Amphiboles: Implications for Low‐Velocity Anomalies in Metasomatized Up...

High P‐T Sound Velocities of Amphiboles: Implications for Low‐Velocity Anomalies in Metasomatized Up...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_004473c2ece7471db145394843b001b4

High P‐T Sound Velocities of Amphiboles: Implications for Low‐Velocity Anomalies in Metasomatized Upper Mantle

About this item

Full title

High P‐T Sound Velocities of Amphiboles: Implications for Low‐Velocity Anomalies in Metasomatized Upper Mantle

Publisher

Washington: John Wiley & Sons, Inc

Journal title

Geophysical research letters, 2024-03, Vol.51 (5), p.n/a

Language

English

Formats

Publication information

Publisher

Washington: John Wiley & Sons, Inc

More information

Scope and Contents

Contents

Metasomatized mantle xenoliths containing hydrous minerals, such as amphiboles, serpentine, and phlogopite, likely represent the potential mineralogical compositions of the metasomatized upper mantle, where low seismic velocities are commonly observed. This study presents the first experimentally determined single‐crystal elasticity model of an Fe‐...

Alternative Titles

Full title

High P‐T Sound Velocities of Amphiboles: Implications for Low‐Velocity Anomalies in Metasomatized Upper Mantle

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_004473c2ece7471db145394843b001b4

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_004473c2ece7471db145394843b001b4

Other Identifiers

ISSN

0094-8276

E-ISSN

1944-8007

DOI

10.1029/2023GL106583

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