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Lithosphere erosion and crustal growth in subduction zones: Insights from initiation of the nascent East Philippine Arc

Macpherson, C.G.

Lithosphere erosion and crustal growth in subduction zones: Insights from initiation of the nascent East Philippine Arc Thumbnail


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Abstract

The Philippine Trench marks a nascent plate margin where subduction initiation is propagating from north to south. Magma compositions in the East Philippine Arc record thinning of arc lithosphere as it is eroded from below. Lithosphere is thicker beneath the younger, southern part of the arc causing basaltic magma to stall and fractionate garnet at high pressure. In the mature, northern section basaltic magma differentiates at shallower levels, at pressures where garnet is not stable. Local variations in lithosphere thickness suggest that thinning is rapid and may be piecemeal. Fluctuations in arc lithosphere thickness throughout the history of this margin appear to control spatial and temporal variations in magma fluxes into the arc crust. Varying fractionation depths of hydrous basalt may help explain the andesitic composition of bulk continental crust.

Citation

Macpherson, C. (2008). Lithosphere erosion and crustal growth in subduction zones: Insights from initiation of the nascent East Philippine Arc. Geology, 36(4), 311-314. https://doi.org/10.1130/g24412a.1

Journal Article Type Article
Acceptance Date Dec 21, 2007
Publication Date Apr 1, 2008
Deposit Date Mar 19, 2015
Publicly Available Date Mar 19, 2015
Journal Geology
Print ISSN 0091-7613
Electronic ISSN 1943-2682
Publisher Geological Society of America
Peer Reviewed Peer Reviewed
Volume 36
Issue 4
Pages 311-314
DOI https://doi.org/10.1130/g24412a.1
Keywords Subduction initiation, Arc lithosphere erosion, Crust growth, Adakitic magmatism, High-Mg# andesite.

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