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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Main Authors: Xiaolong Ma, Zongying Huang
Format: Article
Language:English
Published: SpringerOpen 2020-02-01
Series:Earth, Planets and Space
Subjects:
Online Access:https://doi.org/10.1186/s40623-020-1136-1
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spelling 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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