Detection Of The Mid-mantle Scatterers With Seismic Array Data Processing Techniques | Posted on:2017-05-20 | Degree:Master | Type:Thesis | Country:China | Candidate:Z T Yang | Full Text:PDF | GTID:2180330485491482 | Subject:Marine science | Abstract/Summary: | PDF Full Text Request | The fate of subducted slabs is enigmatic, yet intriguing. We analyse seismic arrivals at-20-50 s after the direct P wave in an array in northeast China (NECESS Array) recordings of four deep earthquakes occurring beneath the west-central Pacific subduction zones (from the eastern Indonesia to Tonga region). We employ the array analysing techniques of fourth root vespagram and beam-forming analysis to constrain the slowness and backazimuth of later arrivals. Our analyses reveal that these arrivals have a slightly lower slowness value than the direct P wave and the backazimuth deviates slightly from the great circle direction. Along with calculation of 1-D synthetic seismograms, we conclude that the later arrival is corresponding to an energy of S-to-P converted at a scatterer below the sources. Total five scatterers are detected at depths varying from ~700 to 1110 km in the study region. The past subducted oceanic crust most likely accounts for the seismic scatterers trapped in the mid-mantle beneath the west-central subduction zones. Our observation in turn reflects that oceanic crust at least partly separated from subducted oceanic lithosphere and may be trapped substantially in the mid-mantle surrounding subduction zones, in particular in the western Pacific subduction zones. | Keywords/Search Tags: | Composition of the oceanic crust, Body waves, Subduction zone processes, Seismic array data, Mantle structures | PDF Full Text Request | Related items |
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