Variation of cooling rate with depth in lower crust formed at an oceanic spreading ridge: Plagioclase crystal size distributions in gabbros from the Oman ophiolite-Reference-Cited by-同舟云学术

Variation of cooling rate with depth in lower crust formed at an oceanic spreading ridge: Plagioclase crystal size distributions in gabbros from the Oman ophiolite

Published:2001-10 Issue:10 Volume:2 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Garrido Carlos J.¹,Kelemen Peter B.¹,Hirth Greg¹

Affiliation:

1. Woods Hole Oceanographic Institution; Department of Geology and Geophysics; Woods Hole Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference52 articles.

1. Theories of normal grain growth in pure single phase systems;Atkinson;Acta Metall.,1988

2. Magma chambers in the Oman Ophiolite: Fed from the top and the bottom?;Boudier;Earth Planet. Sci. Lett.,1996

3. Geochem. Soc.;Brandeis,1987

4. The kinetics of nucleation and crystal growth and scaling laws for magmatic crystallization;Brandeis;Contrib. Mineral. Petrol.,1987

5. Nucleation, crystal growth and the thermal regime of cooling magmas;Brandeis;J. Geophys. Res.,1984

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