ar velocity jump of about 2 % at about 100–145km above the core–mantle boundary and a thin (30-km thick) basal layer with a shear Seismic results have consi stently shown two prom- anomaly ” and the “Pacific anomaly”. The geographic boundary, structural features and velocity structure of the “Africa...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.507.3676 2023-05-15T18:21:07+02:00 Ocean Here Lianxing Wen B Tianyu Zheng A The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.3676 http://geophysics.geo.sunysb.edu/wen/Reprints/HeEA06EPSL.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.3676 http://geophysics.geo.sunysb.edu/wen/Reprints/HeEA06EPSL.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://geophysics.geo.sunysb.edu/wen/Reprints/HeEA06EPSL.pdf shear wave velocity structure core–mantle boundary Pacific anomaly compositional anomaly African anomaly very-low velocity province text 2006 ftciteseerx 2016-01-08T09:26:22Z ar velocity jump of about 2 % at about 100–145km above the core–mantle boundary and a thin (30-km thick) basal layer with a shear Seismic results have consi stently shown two prom- anomaly ” and the “Pacific anomaly”. The geographic boundary, structural features and velocity structure of the “African anomaly ” have been extensively studied and Earth and Planetary Science Lettersinent low-velocity anomalies in the lower mantle, withwave velocity reduction of −13%. Stacked seismic data sampling the middle of the anomaly, however, show no evidence for any internal discontinuity with a velocity decrease greater than −2 % in the middle of the anomaly. Overall, the seismic data sampling the base of the “Pacific anomaly ” can be explained by a negative shear-velocity gradient from 0 % to −1 % (top) to −13 % (bottom) in the lowermost 220 km of the mantle, similar to those of a very-low velocity province beneath the South Atlantic Ocean and the Indian Ocean. Such a strong negative shear-velocity gradient can be explained by partial melting of a compositional anomaly produced early in the Earth's history located within a bottom thermal boundary layer. Our travel time data also exhibit small-scale Text South Atlantic Ocean Unknown Indian Pacific |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
shear wave velocity structure core–mantle boundary Pacific anomaly compositional anomaly African anomaly very-low velocity province |
spellingShingle |
shear wave velocity structure core–mantle boundary Pacific anomaly compositional anomaly African anomaly very-low velocity province Ocean Here Lianxing Wen B Tianyu Zheng A |
topic_facet |
shear wave velocity structure core–mantle boundary Pacific anomaly compositional anomaly African anomaly very-low velocity province |
description |
ar velocity jump of about 2 % at about 100–145km above the core–mantle boundary and a thin (30-km thick) basal layer with a shear Seismic results have consi stently shown two prom- anomaly ” and the “Pacific anomaly”. The geographic boundary, structural features and velocity structure of the “African anomaly ” have been extensively studied and Earth and Planetary Science Lettersinent low-velocity anomalies in the lower mantle, withwave velocity reduction of −13%. Stacked seismic data sampling the middle of the anomaly, however, show no evidence for any internal discontinuity with a velocity decrease greater than −2 % in the middle of the anomaly. Overall, the seismic data sampling the base of the “Pacific anomaly ” can be explained by a negative shear-velocity gradient from 0 % to −1 % (top) to −13 % (bottom) in the lowermost 220 km of the mantle, similar to those of a very-low velocity province beneath the South Atlantic Ocean and the Indian Ocean. Such a strong negative shear-velocity gradient can be explained by partial melting of a compositional anomaly produced early in the Earth's history located within a bottom thermal boundary layer. Our travel time data also exhibit small-scale |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Ocean Here Lianxing Wen B Tianyu Zheng A |
author_facet |
Ocean Here Lianxing Wen B Tianyu Zheng A |
author_sort |
Ocean Here |
publishDate |
2006 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.3676 http://geophysics.geo.sunysb.edu/wen/Reprints/HeEA06EPSL.pdf |
geographic |
Indian Pacific |
geographic_facet |
Indian Pacific |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_source |
http://geophysics.geo.sunysb.edu/wen/Reprints/HeEA06EPSL.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.507.3676 http://geophysics.geo.sunysb.edu/wen/Reprints/HeEA06EPSL.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766200221054795776 |