The role and conditions of second-stage mantle melting in the generation of low-Ti tholeiites and boninites › Research Explorer

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The role and conditions of second-stage mantle melting in the generation of low-Ti tholeiites and boninites: the case of the Manihiki Plateau and the Troodos ophiolite

Research output: Contribution to journal › Article › peer-review

Ultrahigh Pressure Mineralogy Laboratory

DOI

https://doi.org/10.1007/s00410-017-1424-3
Final published version

Roman Golowin
Maxim Portnyagin
Kaj Hoernle
Alexander Sobolev
Dimitry Kuzmin
Reinhard Werner

Original language	English
Article number	104
Number of pages	18
Journal	Contributions to Mineralogy and Petrology
Volume	172
Issue number	11-12
DOIs	https://doi.org/10.1007/s00410-017-1424-3
Publication status	Published - 1 Dec 2017

Research areas

High-Ca boninite, Manihiki Plateau, Mantle plume, Refractory lherzolite, Second-stage melting, Troodos ophiolite, TRACE-ELEMENT COMPOSITION, SUBDUCTION INITIATION, MIDOCEAN RIDGES, DEPLETED MANTLE, EXPERIMENTAL CALIBRATION, VOLCANIC GLASS, MACQUARIE ISLAND, ONTONG JAVA PLATEAU, OCEANIC-CRUST, SOLOMON-ISLANDS

OECD FOS+WOS

ID: 12670537