Emplacement, growth, and gravitational deformation of serpentinite seamounts on the Mariana forearc

Author:

Oakley A. J.,Taylor B.,Fryer P.,Moore G. F.,Goodliffe A. M.,Morgan J. K.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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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