| Abstract: | XRF analyses of individual grains show that the I/S minerals become more illitic (near mica composition) with depth, but they always contain a portion of a smectite component, that is, silica-rich, low layer charge component. Both lath I/S and hexagonal illite minerals appear to grow by adding illite layers of the same composition (0.9 potassium atoms and a slight celadonite, phengite component) onto original crystallites. -from Authors |
| Genre: | Article |
| ProdID: | 70015143 |
| Citation Author: | Lanson, B.; Champion, D. |
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| Citation End Page: | 506 |
| Citation Issue: | 5 |
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| Citation Language: | English |
| Citation Larger Work Title: | American Journal of Science |
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| Citation Number Of Pages: | 34 |
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| Citation Search Results Text: | The I/S-to-illite reaction in the late stage diagenesis; 1991; Article; Journal; American Journal of Science; Lanson, B.; Champion, D. |
| Citation Start Page: | 473 |
| Citation Volume: | 291 |
| Citation Year: | 1991 |
| Type: | citation/reference |
| Text: | The I/S-to-illite reaction in the late stage diagenesis; 1991; Article; Journal; American Journal of Science; Lanson, B.; Champion, D. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1991 00:00 -0600 |
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