Evolution of the lower crust
Granulites, high-grade metamorphic rocks that are deficient in hydrous minerals, are significant constituents of the middle and lower continental crust, and are of great petrological interest. Granulites are discussed.
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| Veröffentlicht in: | Nature (London) 1988-05, Vol.333 (6169), p.119-120 |
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| container_issue | 6169 |
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| container_title | Nature (London) |
| container_volume | 333 |
| creator | Wickham, Stephen M |
| description | Granulites, high-grade metamorphic rocks that are deficient in hydrous minerals, are significant constituents of the middle and lower continental crust, and are of great petrological interest. Granulites are discussed. |
| doi_str_mv | 10.1038/333119a0 |
| format | Article |
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| identifier | ISSN: 0028-0836 |
| ispartof | Nature (London), 1988-05, Vol.333 (6169), p.119-120 |
| issn | 0028-0836 1476-4687 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_36319684 |
| source | Nature; Alma/SFX Local Collection |
| subjects | Continental crust Crystalline rocks Earth sciences Earth, ocean, space Exact sciences and technology Geology Igneous and metamorphic rocks petrology, volcanic processes, magmas Internal geophysics Metamorphic rocks Minerals Solid-earth geophysics, tectonophysics, gravimetry |
| title | Evolution of the lower crust |
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