Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefield
Abstract In order to investigate the small-scale scattering heterogeneities underneath the northern Tien Shan, we analyze the P wavefield from teleseismic events. By using the teleseismic fluctuation method, we separate the total wavefield into coherent and fluctuating parts in the frequency band of...
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Online Access: | https://doi.org/10.1186/s40623-020-1136-1 |
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doaj-d5897926114b430f8400034cce867a232021-02-07T12:48:34ZengSpringerOpenEarth, Planets and Space1880-59812020-02-0172111610.1186/s40623-020-1136-1Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefieldXiaolong Ma0Zongying Huang1State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of SciencesState Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of SciencesAbstract In order to investigate the small-scale scattering heterogeneities underneath the northern Tien Shan, we analyze the P wavefield from teleseismic events. By using the teleseismic fluctuation method, we separate the total wavefield into coherent and fluctuating parts in the frequency band of 0.1–8.0 Hz. Subsequently, we investigate the scattering characteristics by analyzing the frequency-dependent intensities of the coherent and fluctuating wavefield between 0.3 and 2.5 Hz. We further constrain the velocity perturbations and correlation lengths by modeling the P-wave coda envelope with the Monte Carlo simulation. Strong scattering heterogeneities are revealed beneath the northern Tien Shan. The preferred scattering model can be described as a ~ 55- to 130-km-thick randomly heterogeneous layer with velocity perturbations of 6–9% and correlation lengths on the order of 0.4 km. We attribute these small-scale scatterers to isolated melt pockets from the upwelling hot mantle materials.https://doi.org/10.1186/s40623-020-1136-1P-wave codaSmall-scale scattering heterogeneitiesRandom mediaMonte Carlo simulationMelt pocketsUpwelling mantle materials |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Xiaolong Ma Zongying Huang |
spellingShingle |
Xiaolong Ma Zongying Huang Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefield Earth, Planets and Space P-wave coda Small-scale scattering heterogeneities Random media Monte Carlo simulation Melt pockets Upwelling mantle materials |
author_facet |
Xiaolong Ma Zongying Huang |
author_sort |
Xiaolong Ma |
title |
Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefield |
title_short |
Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefield |
title_full |
Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefield |
title_fullStr |
Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefield |
title_full_unstemmed |
Small-scale scattering heterogeneities beneath the northern Tien Shan from the teleseismic P wavefield |
title_sort |
small-scale scattering heterogeneities beneath the northern tien shan from the teleseismic p wavefield |
publisher |
SpringerOpen |
series |
Earth, Planets and Space |
issn |
1880-5981 |
publishDate |
2020-02-01 |
description |
Abstract In order to investigate the small-scale scattering heterogeneities underneath the northern Tien Shan, we analyze the P wavefield from teleseismic events. By using the teleseismic fluctuation method, we separate the total wavefield into coherent and fluctuating parts in the frequency band of 0.1–8.0 Hz. Subsequently, we investigate the scattering characteristics by analyzing the frequency-dependent intensities of the coherent and fluctuating wavefield between 0.3 and 2.5 Hz. We further constrain the velocity perturbations and correlation lengths by modeling the P-wave coda envelope with the Monte Carlo simulation. Strong scattering heterogeneities are revealed beneath the northern Tien Shan. The preferred scattering model can be described as a ~ 55- to 130-km-thick randomly heterogeneous layer with velocity perturbations of 6–9% and correlation lengths on the order of 0.4 km. We attribute these small-scale scatterers to isolated melt pockets from the upwelling hot mantle materials. |
topic |
P-wave coda Small-scale scattering heterogeneities Random media Monte Carlo simulation Melt pockets Upwelling mantle materials |
url |
https://doi.org/10.1186/s40623-020-1136-1 |
work_keys_str_mv |
AT xiaolongma smallscalescatteringheterogeneitiesbeneaththenortherntienshanfromtheteleseismicpwavefield AT zongyinghuang smallscalescatteringheterogeneitiesbeneaththenortherntienshanfromtheteleseismicpwavefield |
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1724280794825883648 |