| Abstract: | The lower Paleozoic rocks that host gold deposits along the Getchell gold belt in Humboldt County, Nevada, represent several allochthonous terranes rather than a sequence of continuous deposition. The term "terrane‘ is used only in a descriptive sense. Evidence for allochthonous terranes in this area includes fault boundaries and differences in age, lithology, and structural style among several rock sequences. -from Authors |
| Genre: | Article |
| ProdID: | 70016748 |
| Citation Author: | Madden-Mcguire, D. J.; Marsh, S. P. |
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| Citation End Page: | 492 |
| Citation Issue: | 5 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geology |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Lower Paleozoic host rocks in the Getchell gold belt: several distinct allochthons or a sequence of continuous sedimentation?; 1991; Article; Journal; Geology; Madden-Mcguire, D. J.; Marsh, S. P. |
| Citation Start Page: | 489 |
| Citation Volume: | 19 |
| Citation Year: | 1991 |
| Type: | citation/reference |
| Text: | Lower Paleozoic host rocks in the Getchell gold belt: several distinct allochthons or a sequence of continuous sedimentation?; 1991; Article; Journal; Geology; Madden-Mcguire, D. J.; Marsh, S. P. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1991 00:00 -0600 |
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