Broad-band Rayleigh wave tomography of Taiwan and its implications on gravity anomalies

We construct the first broad‐band surface wave group velocity dispersion maps for the entire island of Taiwan using the ambient seismic noise tomography. Continuous data from three island‐wide broad‐band networks are used. In particular, taking advantage of the temporary arrays deployed by the TAiwa...

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Veröffentlicht in:Geophysical research letters 2012-03, Vol.39 (5), p.n/a
Hauptverfasser: Huang, Tzu-Ying, Gung, Yuancheng, Liang, Wen-Tzong, Chiao, Ling-Yun, Teng, Louis S.
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container_issue 5
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creator Huang, Tzu-Ying
Gung, Yuancheng
Liang, Wen-Tzong
Chiao, Ling-Yun
Teng, Louis S.
description We construct the first broad‐band surface wave group velocity dispersion maps for the entire island of Taiwan using the ambient seismic noise tomography. Continuous data from three island‐wide broad‐band networks are used. In particular, taking advantage of the temporary arrays deployed by the TAiwan Integrated GEodynamics Research project (TAIGER), we have collected an unprecedented data amount for the noise tomography in Taiwan. We construct 2D group velocity maps for Rayleigh waves from 4 to 20 seconds using a wavelet‐based multi‐scale inversion technique. Patterns of lateral variations of our shorter period (
doi_str_mv 10.1029/2011GL050727
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Continuous data from three island‐wide broad‐band networks are used. In particular, taking advantage of the temporary arrays deployed by the TAiwan Integrated GEodynamics Research project (TAIGER), we have collected an unprecedented data amount for the noise tomography in Taiwan. We construct 2D group velocity maps for Rayleigh waves from 4 to 20 seconds using a wavelet‐based multi‐scale inversion technique. Patterns of lateral variations of our shorter period (&lt;10 seconds) model demonstrate very good correlation with the surficial geology, whereas the overall structure, albeit with much better resolution in the shallow depth, is generally consistent with previously established body wave models. Besides seismic structure, our model also provides vital constraint on resolving the long‐lasting controversy about most prominent Bouguer gravity anomaly in central Taiwan, implying that it is likely caused by a deeper mountain root. With regard to various scenarios of the tectonic evolution of Taiwan, our results seem to favor the lithospheric collision model that invokes significant crustal thickening during the collisional orogeny. Key Points Resolve the long‐lasting controversy about the largest gravity anomaly in Taiwan Build the first surface wave model of Taiwan with unprecedented dense data set Provide important implications to the tectonic evolution of Taiwan</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2011GL050727</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>ambient seismic noises ; Construction ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Geodetics ; Geology ; Gravity ; Gravity anomalies ; gravity anomaly ; Mountains ; multi-scale tomography ; Noise ; Orogeny ; Rayleigh waves ; Research projects ; Seismic engineering ; Seismic phenomena ; Seismology ; Surface waves ; TAIGER ; Tomography ; Wave velocity</subject><ispartof>Geophysical research letters, 2012-03, Vol.39 (5), p.n/a</ispartof><rights>Copyright 2012 by the American Geophysical Union</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4675-21aa7f017bbb85ced8d38a6cb9acb97137b4062b1b22a59794ede44d10b8ad1f3</citedby><cites>FETCH-LOGICAL-a4675-21aa7f017bbb85ced8d38a6cb9acb97137b4062b1b22a59794ede44d10b8ad1f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2011GL050727$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2011GL050727$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11514,27924,27925,45574,45575,46409,46468,46833,46892</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=25974762$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Huang, Tzu-Ying</creatorcontrib><creatorcontrib>Gung, Yuancheng</creatorcontrib><creatorcontrib>Liang, Wen-Tzong</creatorcontrib><creatorcontrib>Chiao, Ling-Yun</creatorcontrib><creatorcontrib>Teng, Louis S.</creatorcontrib><title>Broad-band Rayleigh wave tomography of Taiwan and its implications on gravity anomalies</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>We construct the first broad‐band surface wave group velocity dispersion maps for the entire island of Taiwan using the ambient seismic noise tomography. Continuous data from three island‐wide broad‐band networks are used. In particular, taking advantage of the temporary arrays deployed by the TAiwan Integrated GEodynamics Research project (TAIGER), we have collected an unprecedented data amount for the noise tomography in Taiwan. We construct 2D group velocity maps for Rayleigh waves from 4 to 20 seconds using a wavelet‐based multi‐scale inversion technique. Patterns of lateral variations of our shorter period (&lt;10 seconds) model demonstrate very good correlation with the surficial geology, whereas the overall structure, albeit with much better resolution in the shallow depth, is generally consistent with previously established body wave models. Besides seismic structure, our model also provides vital constraint on resolving the long‐lasting controversy about most prominent Bouguer gravity anomaly in central Taiwan, implying that it is likely caused by a deeper mountain root. With regard to various scenarios of the tectonic evolution of Taiwan, our results seem to favor the lithospheric collision model that invokes significant crustal thickening during the collisional orogeny. 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Res. Lett</addtitle><date>2012-03</date><risdate>2012</risdate><volume>39</volume><issue>5</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>We construct the first broad‐band surface wave group velocity dispersion maps for the entire island of Taiwan using the ambient seismic noise tomography. Continuous data from three island‐wide broad‐band networks are used. In particular, taking advantage of the temporary arrays deployed by the TAiwan Integrated GEodynamics Research project (TAIGER), we have collected an unprecedented data amount for the noise tomography in Taiwan. We construct 2D group velocity maps for Rayleigh waves from 4 to 20 seconds using a wavelet‐based multi‐scale inversion technique. Patterns of lateral variations of our shorter period (&lt;10 seconds) model demonstrate very good correlation with the surficial geology, whereas the overall structure, albeit with much better resolution in the shallow depth, is generally consistent with previously established body wave models. Besides seismic structure, our model also provides vital constraint on resolving the long‐lasting controversy about most prominent Bouguer gravity anomaly in central Taiwan, implying that it is likely caused by a deeper mountain root. With regard to various scenarios of the tectonic evolution of Taiwan, our results seem to favor the lithospheric collision model that invokes significant crustal thickening during the collisional orogeny. Key Points Resolve the long‐lasting controversy about the largest gravity anomaly in Taiwan Build the first surface wave model of Taiwan with unprecedented dense data set Provide important implications to the tectonic evolution of Taiwan</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2011GL050727</doi><tpages>6</tpages><oa>free_for_read</oa></addata></record>
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source Wiley Journals; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Wiley Free Content; Wiley-Blackwell AGU Digital Library
subjects ambient seismic noises
Construction
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geodetics
Geology
Gravity
Gravity anomalies
gravity anomaly
Mountains
multi-scale tomography
Noise
Orogeny
Rayleigh waves
Research projects
Seismic engineering
Seismic phenomena
Seismology
Surface waves
TAIGER
Tomography
Wave velocity
title Broad-band Rayleigh wave tomography of Taiwan and its implications on gravity anomalies
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