| Abstract: | Most coarse detrital rutile is derived from high-grade metamorphic rocks. Contrary to a conventional assumption, independent rutile grains are particularly rare in igneous rocks except alkalic rocks. The use of rutile in the zircon-tourmaline-rutile index of mineralogic maturity is only partially valid, owing to its restricted provenance. -Author |
| Genre: | Article |
| ProdID: | 70012393 |
| Citation Author: | Force, E. R. |
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| Citation End Page: | 488 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Journal of Sedimentary Petrology |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | The provenance of rutile.; 1980; Article; Journal; Journal of Sedimentary Petrology; Force, E. R. |
| Citation Start Page: | 485 |
| Citation Volume: | 50 |
| Citation Year: | 1980 |
| Type: | citation/reference |
| Text: | The provenance of rutile.; 1980; Article; Journal; Journal of Sedimentary Petrology; Force, E. R. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1980 00:00 -0600 |
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