| Abstract: | Two upper Cenozoic depositional sequences of principally marine strata about 4000m thick overlie accreted basement terranes of the Central and Coastal belts of the Franciscan Complex in the onshore-offshore Eel River basin of northwestern California. The older depositional sequence is early to middle Miocene in age and represents slope basin and slope-blanket deposition, whereas the younger sequence, late Miocene to middle Pleistocene in age, consists largely of forearc basin deposits. -from Author |
| Genre: | Article |
| ProdID: | 70016594 |
| Citation Author: | Clarke, Jr, S. H. |
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| Citation End Page: | 224 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | American Association of Petroleum Geologists Bulletin |
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| Citation Number Of Pages: | 26 |
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| Citation Search Results Text: | Geology of the Eel River basin and adjacent region: implications for late Cenozoic tectonics of the southern Cascadia subduction zone and Mendocino triple junction; 1992; Article; Journal; American Association of Petroleum Geologists Bulletin; Clarke, Jr, S. H. |
| Citation Start Page: | 199 |
| Citation Volume: | 76 |
| Citation Year: | 1992 |
| Type: | citation/reference |
| Text: | Geology of the Eel River basin and adjacent region: implications for late Cenozoic tectonics of the southern Cascadia subduction zone and Mendocino triple junction; 1992; Article; Journal; American Association of Petroleum Geologists Bulletin; Clarke, Jr, S. H. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Wed, 1 Jan 1992 00:00 -0600 |
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