Subduction recycling of continental sediments and the origin of geochemically enriched reservoirs in the deep mantle
Isotopic and trace element geochemical studies of ocean island basalts (OIBs) have for many years been used to infer the presence of long-lived (∼ 1-2 Ga old) compositional heterogeneities in the deep mantle related to recycling of crustal lithologies
| Verfasser: | |
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| Dokumenttyp: | Journal article |
| Verlag/Hrsg.: |
Elsevier
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| Schlagwörter: | Keywords: Continental (CO) / Continental crusts / Deep mantle / Ocean island basalt (OIB) / trace element composition / Agricultural chemicals / Basalt / Chemical analysis / Chemical elements / Earth sciences / Gallium / Isotopes / Landforms / Lithology / Microfluidics / Recyclin continental sediments / K-hollandite / lamproite / mantle transition zone / ocean island basalts (OIB) / subduction zones |
| Sprache: | unknown |
| Permalink: | https://search.fid-benelux.de/Record/base-27123300 |
| Datenquelle: | BASE; Originalkatalog |
| Powered By: | BASE |
| Link(s) : | http://hdl.handle.net/1885/35406 |
