| Abstract: | The Neogene Humboldt (Eel River) Basin is located along the north-eastern margin of the Pacific Ocean within the Cascadia subduction zone. This sedimentary basin originated near the base of the accretionary prism in post-Eocene time. Subduction processes since that time have elevated strata in the south-eastern portion of the basin above sea level. High-resolution chronostratigraphic data from the onshore portion of the Humboldt Basin enable correlation of time-equivalent lithofacies across the palaeomargin, reconstruction of slope-basin evolution, and preliminary delineation of climatic and tectonic influence on lithological variation. -from Author |
| Genre: | Article |
| ProdID: | 70018813 |
| Citation Author: | McCrory, P. A. |
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| Citation End Page: | 247 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Sedimentology |
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| Citation Number Of Pages: | 25 |
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| Citation Search Results Text: | Evolution of a trench-slope basin within the Cascadia subduction margin: the Neogene Humboldt Basin, California; 1995; Article; Journal; Sedimentology; McCrory, P. A. |
| Citation Start Page: | 223 |
| Citation Volume: | 42 |
| Citation Year: | 1995 |
| Type: | citation/reference |
| Text: | Evolution of a trench-slope basin within the Cascadia subduction margin: the Neogene Humboldt Basin, California; 1995; Article; Journal; Sedimentology; McCrory, P. A. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1995 00:00 -0600 |
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