| Abstract: | Uses anisotropy of magnetic susceptibility (AMS) to define the flow fabric and possible source area of the Peach Springs Tuff, a widespread rhyolitic ash flow tuff in the Mojave Desert and Great Basin of California, Arizona, and Nevada. Lineation and imbrication indicate a source region near the southern tip of Nevada. The optimum intersection of magnetic lineations lies in the southern Black Mountains of Arizona on the eastern side of the Colorado River extensional corridor. -from Authors |
| Genre: | Article |
| ProdID: | 70016395 |
| Citation Author: | Hillhouse, J. W.; Wells, R. E. |
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| Citation Issue: | B7 |
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| Citation Language: | English |
| Citation Larger Work Title: | Journal of Geophysical Research |
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| Citation Search Results Text: | Magnetic fabric, flow directions, and source area of the Lower Miocene Peach Springs Tuff in Arizona, California, and Nevada; 1991; Article; Journal; Journal of Geophysical Research; Hillhouse, J. W.; Wells, R. E. |
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| Citation Volume: | 96 |
| Citation Year: | 1991 |
| Type: | citation/reference |
| Text: | Magnetic fabric, flow directions, and source area of the Lower Miocene Peach Springs Tuff in Arizona, California, and Nevada; 1991; Article; Journal; Journal of Geophysical Research; Hillhouse, J. W.; Wells, R. E. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1991 00:00 -0600 |
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