Melt- versus fluid-induced metasomatism in spinel to garnet wedge peridotites (Ulten zone, Eastern Italian alps): clues from trace element and Li abundances
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Scambelluri, Marco; Hermann, Joerg; Morten, Lauren; Rampone, E
Description
The peridotite bodies of the Ulten Zone (Upper Austroalpine, Italian Eastern Alps) are enclosed in Variscan migmatites and derive from a mantle wedge environment. They display the progressive transformation of porphyroclastic spinel peridotites (T =1,200
| Collections | ANU Research Publications |
|---|---|
| Date published: | 2006 |
| Type: | Journal article |
| URI: | http://hdl.handle.net/1885/18535 |
| Source: | Contributions to Mineralogy and Petrology |
| DOI: | 10.1007/s00410-006-0064-9 |
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| File | Description | Size | Format | Image |
|---|---|---|---|---|
| 01_Scambelluri_Melt-_versus_fluid-induced_2006.pdf | 932.91 kB | Adobe PDF | Request a copy |
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