| Abstract: | Zeolites and associated minerals occur in a tholeiitic basaltic pillow lava sequence. Although the zeolite assemblages are similar to those found in other major zeolite occurrences in basaltic pillow lavas, regional zoning of the zeolite assemblages is not apparent. The formation of the different assemblages is discussed.-D.F.B. |
| Genre: | Article |
| ProdID: | 70012327 |
| Citation Author: | Keith, T. E. C.; Staples, L. W. |
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| Citation End Page: | 144 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Clays & Clay Minerals |
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| Citation Number Of Pages: | 10 |
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| Citation Search Results Text: | Zeolites in Eocene basaltic pillow lavas of the Siletz River Volcanics, Central Coast Range, Oregon.; 1985; Article; Journal; Clays & Clay Minerals; Keith, T. E. C.; Staples, L. W. |
| Citation Start Page: | 135 |
| Citation Volume: | 33 |
| Citation Year: | 1985 |
| Type: | citation/reference |
| Text: | Zeolites in Eocene basaltic pillow lavas of the Siletz River Volcanics, Central Coast Range, Oregon.; 1985; Article; Journal; Clays & Clay Minerals; Keith, T. E. C.; Staples, L. W. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1985 00:00 -0600 |
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