Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness.

dc.contributor.author	Klein, Emily M
dc.contributor.author	Langmuir, CH
dc.date.accessioned	2014-01-17T15:53:35Z
dc.date.accessioned	2014-01-23T18:25:49Z
dc.date.accessioned	2014-01-23T18:28:04Z
dc.date.issued	1987-12-01
dc.description.abstract	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
dc.identifier.issn	0148-0227
dc.identifier.uri	https://hdl.handle.net/10161/8320
dc.relation.ispartof	Journal of Geophysical Research
dc.relation.replaces	http://hdl.handle.net/10161/8314
dc.relation.replaces	10161/8314
dc.relation.replaces	http://hdl.handle.net/10161/8319
dc.relation.replaces	10161/8319
dc.title	Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness.
dc.type	Journal article
pubs.begin-page	8089
pubs.end-page	8115
pubs.issue	B8
pubs.organisational-group	Duke
pubs.organisational-group	Earth and Ocean Sciences
pubs.organisational-group	Nicholas School of the Environment
pubs.publication-status	Published
pubs.volume	92

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