Reconciling the geophysical and geochemical mantles: Plume flows, heterogeneities, and disequilibrium
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Description
Geophysical evidence and numerical models of mantle stirring imply the source of mid-ocean ridge basalts (MORBs) comprises most of the mantle, excepting only the D″ region and the "superpile" anomalies deep under Africa and the Pacific. Geophysical evid
| Collections | ANU Research Publications |
|---|---|
| Date published: | 2009 |
| Type: | Journal article |
| URI: | http://hdl.handle.net/1885/29418 |
| Source: | Geochemistry, Geophysics, Geosystems. G3 |
| DOI: | 10.1029/2009GC002634 |
| Access Rights: | Open Access |
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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Davies_Reconciling_the_geophysical_2009.pdf | 511.23 kB | Adobe PDF | Request a copy |
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