Very high-pressure orogenic garnet peridotites
Mantle-derived garnet peridotites are a minor component in many very high-pressure metamorphic terranes that formed during continental subduction and collision. Some of these mantle rocks contain trace amounts of zircon and micrometer-sized inclusions. The constituent minerals exhibit pre- and posts...
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| Veröffentlicht in: | Proceedings of the National Academy of Sciences - PNAS 2007-05, Vol.104 (22), p.9116-9121 |
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| container_title | Proceedings of the National Academy of Sciences - PNAS |
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| creator | Liou, J.G Zhang, R.Y Ernst, W.G |
| description | Mantle-derived garnet peridotites are a minor component in many very high-pressure metamorphic terranes that formed during continental subduction and collision. Some of these mantle rocks contain trace amounts of zircon and micrometer-sized inclusions. The constituent minerals exhibit pre- and postsubduction microstructures, including polymorphic transformation and mineral exsolution. Experimental, mineralogical, petrochemical, and geochronological characterizations using novel techniques with high spatial, temporal, and energy resolutions are resulting in unexpected discoveries of new phases, providing better constraints on deep mantle processes. |
| doi_str_mv | 10.1073/pnas.0607300104 |
| format | Article |
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| identifier | ISSN: 0027-8424 |
| ispartof | Proceedings of the National Academy of Sciences - PNAS, 2007-05, Vol.104 (22), p.9116-9121 |
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| source | Jstor Complete Legacy; MEDLINE; PubMed Central; Alma/SFX Local Collection; Free Full-Text Journals in Chemistry |
| subjects | Earth Earth (Planet) Eclogite Garnets Geological Phenomena Geology Gneiss High-Pressure Geoscience Special Feature Igneous rocks Mantle Metamorphism Mineralogy Minerals Nanostructures - ultrastructure Peridotite Petrology Pressure Rocks Subduction |
| title | Very high-pressure orogenic garnet peridotites |
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