Climate Change Data Portal
DOI | 10.1093/gji/ggw271 |
Anisotropy from SKS splitting across the Pacific-North America plate boundary offshore southern California | |
Ramsay, Joseph; Kohler, Monica D.; Davis, Paul M.; Wang, Xinguo; Holt, William; Weeraratne, Dayanthie S. | |
通讯作者 | Kohler, MD (通讯作者) |
发表日期 | 2016 |
ISSN | 0956-540X |
EISSN | 1365-246X |
起始页码 | 244 |
结束页码 | 258 |
卷号 | 207期号:1 |
英文摘要 | SKS arrivals from ocean bottom seismometer (OBS) data from an offshore southern California deployment are analysed for shear wave splitting. The project involved 34 OBSs deployed for 12 months in a region extending up to 500 km west of the coastline into the oceanic Pacific plate. The measurement process consisted of removing the effects of anisotropy using a range of values for splitting fast directions and delay times to minimize energy along the transverse seismometer axis. Computed splitting parameters are unexpectedly similar to onland parameters, exhibiting WSW-ENE fast polarization directions and delays between 0.8 and 1.8 s, even for oceanic plate sites. This is the first SKS splitting study to extend across the entire boundary between the North America and Pacific plates, into the oceanic part of the Pacific plate. The splitting results show that the fast direction of anisotropy on the Pacific plate does not align with absolute plate motion (APM), and they extend the trend of anisotropy in southern California an additional 500 km west, well onto the oceanic Pacific plate. We model the finite strain and anisotropy within the asthenosphere associated with density-buoyancy driven mantle flow and the effects of APM. In the absence of plate motion effects, such buoyancy driven mantle flow would be NE-directed beneath the Pacific plate observations. The best-fit patterns of mantle flow are inferred from the tomography-based models that show primary influences from foundering higher-density zones associated with the history of subduction beneath North America. The new offshore SKS measurements, when combined with measurements onshore within the plate boundary zone, indicate that dramatic lateral variations in density-driven upper-mantle flow are required from offshore California into the plate boundary zone in California and western Basin and Range. |
关键词 | SEISMIC ANISOTROPYMANTLE FLOWOLIVINE POLYCRYSTALSJOINT INVERSIONUNITED-STATESFINITE STRAINWAVESHEARBENEATHDYNAMICS |
英文关键词 | Body waves; Seismic anisotropy; Continental margins: transform; Dynamics of lithosphere and mantle; Pacific Ocean |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000384651200017 |
来源期刊 | GEOPHYSICAL JOURNAL INTERNATIONAL
![]() |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258849 |
推荐引用方式 GB/T 7714 | Ramsay, Joseph,Kohler, Monica D.,Davis, Paul M.,et al. Anisotropy from SKS splitting across the Pacific-North America plate boundary offshore southern California[J]. 中国科学院青藏高原研究所,2016,207(1). |
APA | Ramsay, Joseph,Kohler, Monica D.,Davis, Paul M.,Wang, Xinguo,Holt, William,&Weeraratne, Dayanthie S..(2016).Anisotropy from SKS splitting across the Pacific-North America plate boundary offshore southern California.GEOPHYSICAL JOURNAL INTERNATIONAL,207(1). |
MLA | Ramsay, Joseph,et al."Anisotropy from SKS splitting across the Pacific-North America plate boundary offshore southern California".GEOPHYSICAL JOURNAL INTERNATIONAL 207.1(2016). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。