Distribution of recent volcanism and the morphology of seamounts and ridges in the GLIMPSE study area: Implications for the lithospheric cracking hypothesis for the origin of intraplate, non-hot spot volcanic chains

Author:

Forsyth Donald W.1,Harmon Nicholas1,Scheirer Daniel S.1,Duncan Robert A.2

Affiliation:

1. Department of Geological Sciences; Brown University; Providence Rhode Island USA

2. College of Oceanic and Atmospheric Sciences; Oregon State University; Corvallis Oregon USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference48 articles.

1. Convection beneath young oceanic lithosphere: Implications for thermal structure and gravity;Buck;J. Geophys. Res.,1986

2. Irradiation of samples for 40Ar/39Ar dating using the Geological Survey TRIGA reactor;Dalrymple;U. S. Geol. Surv. Prof. Pap.,1981

3. Current plate motions;DeMets;Geophys. J. Int.,1990

4. Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions;DeMets;Geophys. Res. Lett.,1994

5. Geochemical constraints on melting process in the GLIMPSE region;Donnelly;Eos Trans. AGU,2003

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