| Abstract: | Mixed-layer clays of randomly interstratified kerolite/stevensite occur as an abundant mineral in lake and/or spring deposits of probable Pliocene and Pleistocene age in the Amargosa Desert of S Nevada, USA. Kerolite is a trioctahedral mineral similar to talc, but with a basal spacing of approx 9.65 A (cf. talc at 9.38 A). The data suggest that talc, kerolite and stevensite may form a continuous structural series based on layer charge. (Following abstract) -D.F.B. |
| Genre: | Article |
| ProdID: | 70011847 |
| Citation Author: | Eberl, D. D.; Jones, B. F.; Khoury, H. N. |
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| Citation End Page: | 326 |
| Citation Issue: | 5 |
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| Citation Language: | English |
| Citation Larger Work Title: | Clays & Clay Minerals |
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| Citation Number Of Pages: | 6 |
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| Citation Search Results Text: | Mixed-layer kerolite/stevensite from the Amargosa Desert, Nevada.; 1982; Article; Journal; Clays & Clay Minerals; Eberl, D. D.; Jones, B. F.; Khoury, H. N. |
| Citation Start Page: | 321 |
| Citation Volume: | 30 |
| Citation Year: | 1982 |
| Type: | citation/reference |
| Text: | Mixed-layer kerolite/stevensite from the Amargosa Desert, Nevada.; 1982; Article; Journal; Clays & Clay Minerals; Eberl, D. D.; Jones, B. F.; Khoury, H. N. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Fri, 1 Jan 1982 00:00 -0600 |
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