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- W2090435358 abstract "Understanding the relative motion between the Pacific plate and its neighboring plates inthe Paleogene has important consequences for deciphering the relationship between absoluteand relative plate motions in the Pacific Ocean basin, the history of circum-Pacific subduction,and the cause of the Hawaiian-Emperor bend (HEB). We quantitatively model the Farallon/Vancouver-Pacific-Antarctic seafloor spreading history from 67 to 33 Ma based on a comprehensivesynthesis of magnetic anomaly and fracture identifications. We find a well-constrainedincrease from 75 ± 5 mm/yr to 101 ± 5 mm/yr in Pacific-Farallon full spreading rates between57.6 Ma and 55.9 Ma, followed by a stepwise increase to 182 ± 2 mm/yr from 49.7 to 40.1 Ma.The increases in Pacific-Farallon spreading rates are not accompanied by any statistically significantchange in spreading direction. The 57.6–55.9 Ma surge of Pacific-Farallon spreadingreflects an eastward acceleration in Farallon plate motion, as it precedes west Pacific subductioninitiation and is not associated with any significant change in Pacific-Antarctic spreading.We interpret the increase in Pacific-Farallon spreading rates after ca. 50 Ma as a consequenceof further acceleration in Farallon plate motion. We find no indication of a major change inPacific plate absolute motion at this time. Our model suggests that changes in relative motiondirection between the Pacific and Farallon and Pacific and Antarctic plates were insignificantaround the formation time of the HEB (ca. 47.5 Ma), and the bend is largely a consequence ofHawaiian hotspot motion, which ceased rapid motion after 47 Ma." @default.
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- W2090435358 date "2016-03-22" @default.
- W2090435358 modified "2023-09-23" @default.
- W2090435358 title "Revision of Paleogene plate motions in the Pacific and implications for the Hawaiian-Emperor bend: REPLY" @default.
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- W2090435358 doi "https://doi.org/10.1130/g37828y.1" @default.
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