Geodynamic modeling of late Archean subduction: Pressure-temperature constraints from greenstone belt diamond deposits

Author:

O'Neill C.,Wyman D. A.

Publisher

American Geophysical Union

Reference46 articles.

1. Dehydration, asthenospheric convection, and seismicity in sub-duction zones;Anderson;Journal of Geology,1980

2. The association of Zn-Chromite with diamondiferous lamprophyres and diamonds: unique compositions as a guide to the diamond potential of non-traditional diamond host rocks;Armstrong,2003

3. Slab breakoff: a model for Caledonian, Late Granite syn-collisional magmatism in the orthotectonic (metamorphic) zone of Scotland and Donegal, Ireland;Atherton;Lithos,2002

4. Evolution of the southern Abitibi greenstone belt based on U-Pb geochronology: autochthonous volcanic construction followed by plutonism, regional deformation and sedimentation;Ayer;Precambrian Research,2002

5. Origin of Diamondiferous Archean Lamprophyres in the Evolution of the Michipicoten and Abitibi Greenstone Belts;Ayer,2003

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