Geology of the Eel River basin and adjacent region: Implications for late Cenozoic tectonics of the southern Cascadia subduction zone and Mendocino triple junction

S. H. Clarke

doi:10.1306/bdff87ae-1718-11d7-8645000102c1865d

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Geology of the Eel River basin and adjacent region: Implications for late Cenozoic tectonics of the southern Cascadia subduction zone and Mendocino triple junction

S. H. Clarke

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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

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American Association of Petroleum Geologists Bulletin Article

Source-reported bounding extent: 39° to 42° latitude; -125° to -123.75° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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S. H. Clarke. 1992. Geology of the Eel River basin and adjacent region: Implications for late Cenozoic tectonics of the southern Cascadia subduction zone and Mendocino triple junction. https://doi.org/10.1306/bdff87ae-1718-11d7-8645000102c1865d

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