| Abstract: | The 1983 Coalinga earthquake occurred at the eastern boundary of the California Coast Ranges in response to northeast directed thrusting. Such movements over the past 2 Ma have produced Coalinga anticline by folding above the blind eastern tip of the Coalinga thrust zone. The 600-km length of the Coast Ranges boundary shares a common structural setting that involves westward upturn of Cenozoic and Cretaceous strata at the eastern front of the Coast Ranges and a major, southwest facing step in the basement surface beneath the western Great Valley. Like Coalinga anticline, Pliocene and Quaternary folding and faulting along the rest of the boundary also result from northeast-southwest compression acting nearly perpendicular to the strike of the San Andreas fault. We suggest that much of this deformation is related to active thrusts beneath the eastern Coast Ranges. The step in the basement surface beneath the Great Valley seems to have controlled the distribution of this deformation and the shape of the Coast Ranges boundary. -Authors |
| Genre: | Article |
| ProdID: | 70016442 |
| Citation Author: | Wentworth, C. M.; Zoback, M. D. |
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| Citation End Page: | 246 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Tectonics |
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| Citation Number Of Pages: | 10 |
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| Citation Search Results Text: | The style of late Cenozoic deformation at the eastern front of the California Coast Ranges; 1989; Article; Journal; Tectonics; Wentworth, C. M.; Zoback, M. D. |
| Citation Start Page: | 237 |
| Citation Volume: | 8 |
| Citation Year: | 1989 |
| Type: | citation/reference |
| Text: | The style of late Cenozoic deformation at the eastern front of the California Coast Ranges; 1989; Article; Journal; Tectonics; Wentworth, C. M.; Zoback, M. D. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1989 00:00 -0600 |
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