Emplacement, growth, and gravitational deformation of serpentinite seamounts on the Mariana forearc
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/170/2/615/2518901/170-2-615.pdf
Reference73 articles.
1. Bebout, G.E. & Scholl, D.V., eds, 1996. Subduction: Top to Bottom. American Geophysical Union, Washington, DC.
2. Distribution and origin of Igneous Rocks from the Landward Slopes of the Mariana Trench: implications for its structure and evolution;Bloomer;J. Geophys. Res.,1983
3. Gabbroic and ultramafic rocks from the Mariana Trench: An island arc ophiolite
4. Dynamic basis of volcanic spreading;Borgia;J. Geophys. Res.,1994
5. 3-D configuration of subducted lithosphere in the Western Pacific;Chiu;Geophys. J. Int.,1991
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