Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness.
Publication
, Journal Article
Klein, EM; Langmuir, CH
December 1, 1987
Thermal modeling independently predicts the observed relationships among basalt chemistry, ridge depth, and crustal thickness resulting from temperature variations in the mantle. Beneath the shallowest and deepest ridge axes, temperature differences of approximately 250oC in the subsolidus mantle are required to account for the global systematics. -from Authors
Duke Scholars
Publication Date
December 1, 1987
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Klein, E. M., & Langmuir, C. H. (1987). Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness.
Klein, Emily M., and C. H. Langmuir. “Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness.,” December 1, 1987.
Klein EM, Langmuir CH. Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness. 1987 Dec 1;
Klein, Emily M., and C. H. Langmuir. Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness. Dec. 1987.
Klein EM, Langmuir CH. Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness. 1987 Dec 1;
Publication Date
December 1, 1987