| Abstract: | Harmotome, a Ba-rich zeolite, is reported in a lacustrine sandstone dominated by basaltic fragments now mainly altered to smectite and iron oxides. Harmotome forms 4-5% of the rock and occurs as an authigenic layer of stubby prismatic crystals typically 2-7 mu m long, lining voids in the sandstone.-D.F.B. |
| Genre: | Article |
| ProdID: | 70011387 |
| Citation Author: | Sheppard, R. A.; Gude, 3rd, A. J. |
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| Citation End Page: | 59 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Clays & Clay Minerals |
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| Citation Number Of Pages: | 3 |
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| Citation Search Results Text: | Harmotome in a basaltic, volcaniclastic sandstone from a lacustrine deposit near Kirkland Junction, Yavapai County, Arizona.; 1983; Article; Journal; Clays & Clay Minerals; Sheppard, R. A.; Gude, 3rd, A. J. |
| Citation Start Page: | 57 |
| Citation Volume: | 31 |
| Citation Year: | 1983 |
| Type: | citation/reference |
| Text: | Harmotome in a basaltic, volcaniclastic sandstone from a lacustrine deposit near Kirkland Junction, Yavapai County, Arizona.; 1983; Article; Journal; Clays & Clay Minerals; Sheppard, R. A.; Gude, 3rd, A. J. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1983 00:00 -0600 |
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