| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8911781 | Lithos | 2018 | 99 Pages |
Abstract
Essentially, the ultramafic complexes in the SIP comprises deep-seated transient magma chambers that facilitated mixing and homogenisation of a rich diversity of fertile asthenospheric melts en route to the upper parts of the continental crust.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Rune B. Larsen, Thomas Grant, Bjørn E. Sørensen, Christian Tegner, Suzanne McEnroe, Zeudia Pastore, Christine Fichler, Even Nikolaisen, Kim R. Grannes, Nathan Church, Geertje W. ter Maat, Alexander Michels,