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• W2006597718 abstract "Research Article| March 01, 1992 Deep crustal structure and tectonics in the offshore southern Santa Maria Basin, California Craig Nicholson; Craig Nicholson 1Institute for Crustal Studies, University of California, Santa Barbara, California 93106 Search for other works by this author on: GSW Google Scholar Christopher C. Sorlien; Christopher C. Sorlien 1Institute for Crustal Studies, University of California, Santa Barbara, California 93106 Search for other works by this author on: GSW Google Scholar Bruce P. Luyendyk Bruce P. Luyendyk 1Institute for Crustal Studies, University of California, Santa Barbara, California 93106 Search for other works by this author on: GSW Google Scholar Author and Article Information Craig Nicholson 1Institute for Crustal Studies, University of California, Santa Barbara, California 93106 Christopher C. Sorlien 1Institute for Crustal Studies, University of California, Santa Barbara, California 93106 Bruce P. Luyendyk 1Institute for Crustal Studies, University of California, Santa Barbara, California 93106 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1992) 20 (3): 239–242. https://doi.org/10.1130/0091-7613(1992)020<0239:DCSATI>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Craig Nicholson, Christopher C. Sorlien, Bruce P. Luyendyk; Deep crustal structure and tectonics in the offshore southern Santa Maria Basin, California. Geology 1992;; 20 (3): 239–242. doi: https://doi.org/10.1130/0091-7613(1992)020<0239:DCSATI>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Reprocessed deep-penetration seismic reflection profiles across the offshore southern Santa Maria Basin suggest a complex history of tectonic deformation. The top of subducted oceanic crust, imaged at the north end of EDGE line RU-10, is disrupted and eventually disappears to the south. Farther south, a strong lower crustal reflection ramps up and may reflect a possible north-dipping low- angle detachment, or a change in crustal geometry associated with the subducted Morro Fracture Zone. Above a time-transgressive unconformity, Miocene and younger sediments onlap to the south and water bottom deepens, suggesting a major regional tilt reversal in post-Miocene time. Below the unconformity, basement is displaced by largely northwest-striking normal faults that we believe form tilted crustal blocks; it is possible that Cretaceous and Paleogene sections are preserved in resulting half-grabens. Some of these normal faults, including splays off the outer Santa Lucia Bank fault system, were reactivated as minor reverse faults in post-Miocene time. There is no evidence that requires any post-17.5 Ma tectonostratigraphic terrane boundary through this area; rather, much of the structure of the southern Santa Maria Basin appears to be continuous with the rotated Western Transverse Ranges and northern Channel Islands. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2006597718 title "Deep crustal structure and tectonics in the offshore southern Santa Maria Basin, California" @default.
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