The shear wave velocity structure of the crust and uppermost mantle beneath Tagaytay, Philippines inferred from receiver function analysis
Depths of the partially melted zone and the Moho discontinuity are probably at 18 kilometers and 34 kilometers, respectively beneath Tagaytay seismic station, Luzon, Philippines. This conclusion is based on the shear‐wave velocity structure determined in this study, which indicates the presence of a...
Gespeichert in:
| Veröffentlicht in: | Geophysical research letters 1995-12, Vol.22 (23), p.3143-3146 |
|---|---|
| Hauptverfasser: | , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 3146 |
|---|---|
| container_issue | 23 |
| container_start_page | 3143 |
| container_title | Geophysical research letters |
| container_volume | 22 |
| creator | Besana, G. M. Shibutani, T. Hirano, N. Ando, M. Bautista, B. Narag, I. Punongbayan, R. S. |
| description | Depths of the partially melted zone and the Moho discontinuity are probably at 18 kilometers and 34 kilometers, respectively beneath Tagaytay seismic station, Luzon, Philippines. This conclusion is based on the shear‐wave velocity structure determined in this study, which indicates the presence of a low‐velocity zone and high‐velocity zone at these depths. The shear wave velocity model was derived from the inversion of five receiver functions of teleseismic earthquakes recorded by the broadband seismometer at Tagaytay. However, due to the very limited information to constrain our initial model, other models with comparable waveform fit were also obtained but with deeper low velocity zone and shallower Moho. |
| doi_str_mv | 10.1029/95GL03319 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1531017900</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1531017900</sourcerecordid><originalsourceid>FETCH-LOGICAL-a4552-13719ea0f6ae7ea2e216f05a7bd3a1cc6a6c223a64097a0701a28e63667f1c773</originalsourceid><addsrcrecordid>eNp1kM1uEzEURi0EEiGw4A28YAESU_yTseMlqkooCqVCaZG6sW6da2KY8Qy2J2VeoU_NoFTZdeVr6Zyz-Ah5zdkJZ8J8MPVqzaTk5gmZcbNYVEvG9FMyY8xMt9DqOXmR8y_GmGSSz8j9Zoc07xASvYM90j02nQtlpLmkwZUhIe08LRPk0pALhbilQ99jarvp10IsDdJbjAhlRzfwE8YC43t6uQtN6PsQMdMQPaaEW-pT19KEDsMeE_VDdCV0cUpCM-aQX5JnHpqMrx7eObn6dLY5_Vytv63OTz-uK1jUtai41NwgMK8ANYJAwZVnNejbrQTunALlhJCgFsxoYJpxEEtUUintudNazsnbQ7dP3Z8Bc7FtyA6bBiJ2Q7a8lpxxbaaJ5uTdAXWpyzmht30KLaTRcmb_722Pe0_sm4csZAeNTxBdyEdBGKnFRM7JyQG7Cw2Oj_fs6vt6uZRiEqqDEHLBv0cB0m-rtNS1_XGxsjdK35jrL5f2q_wHzkuekg</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1531017900</pqid></control><display><type>article</type><title>The shear wave velocity structure of the crust and uppermost mantle beneath Tagaytay, Philippines inferred from receiver function analysis</title><source>Wiley-Blackwell Journals</source><creator>Besana, G. M. ; Shibutani, T. ; Hirano, N. ; Ando, M. ; Bautista, B. ; Narag, I. ; Punongbayan, R. S.</creator><creatorcontrib>Besana, G. M. ; Shibutani, T. ; Hirano, N. ; Ando, M. ; Bautista, B. ; Narag, I. ; Punongbayan, R. S.</creatorcontrib><description>Depths of the partially melted zone and the Moho discontinuity are probably at 18 kilometers and 34 kilometers, respectively beneath Tagaytay seismic station, Luzon, Philippines. This conclusion is based on the shear‐wave velocity structure determined in this study, which indicates the presence of a low‐velocity zone and high‐velocity zone at these depths. The shear wave velocity model was derived from the inversion of five receiver functions of teleseismic earthquakes recorded by the broadband seismometer at Tagaytay. However, due to the very limited information to constrain our initial model, other models with comparable waveform fit were also obtained but with deeper low velocity zone and shallower Moho.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/95GL03319</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Earth sciences ; Earth, ocean, space ; Earthquakes ; Earthquakes, seismology ; Exact sciences and technology ; Internal geophysics ; Moho discontinuity ; Philippines ; Receivers ; Seismic phenomena ; Solid-earth geophysics, tectonophysics, gravimetry ; Sound waves ; Stations ; Waveforms</subject><ispartof>Geophysical research letters, 1995-12, Vol.22 (23), p.3143-3146</ispartof><rights>1995 American Geophysical Union. All Rights Reserved</rights><rights>1996 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4552-13719ea0f6ae7ea2e216f05a7bd3a1cc6a6c223a64097a0701a28e63667f1c773</citedby><cites>FETCH-LOGICAL-a4552-13719ea0f6ae7ea2e216f05a7bd3a1cc6a6c223a64097a0701a28e63667f1c773</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%2F95GL03319$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F95GL03319$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=2937203$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Besana, G. M.</creatorcontrib><creatorcontrib>Shibutani, T.</creatorcontrib><creatorcontrib>Hirano, N.</creatorcontrib><creatorcontrib>Ando, M.</creatorcontrib><creatorcontrib>Bautista, B.</creatorcontrib><creatorcontrib>Narag, I.</creatorcontrib><creatorcontrib>Punongbayan, R. S.</creatorcontrib><title>The shear wave velocity structure of the crust and uppermost mantle beneath Tagaytay, Philippines inferred from receiver function analysis</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>Depths of the partially melted zone and the Moho discontinuity are probably at 18 kilometers and 34 kilometers, respectively beneath Tagaytay seismic station, Luzon, Philippines. This conclusion is based on the shear‐wave velocity structure determined in this study, which indicates the presence of a low‐velocity zone and high‐velocity zone at these depths. The shear wave velocity model was derived from the inversion of five receiver functions of teleseismic earthquakes recorded by the broadband seismometer at Tagaytay. However, due to the very limited information to constrain our initial model, other models with comparable waveform fit were also obtained but with deeper low velocity zone and shallower Moho.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Exact sciences and technology</subject><subject>Internal geophysics</subject><subject>Moho discontinuity</subject><subject>Philippines</subject><subject>Receivers</subject><subject>Seismic phenomena</subject><subject>Solid-earth geophysics, tectonophysics, gravimetry</subject><subject>Sound waves</subject><subject>Stations</subject><subject>Waveforms</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1995</creationdate><recordtype>article</recordtype><recordid>eNp1kM1uEzEURi0EEiGw4A28YAESU_yTseMlqkooCqVCaZG6sW6da2KY8Qy2J2VeoU_NoFTZdeVr6Zyz-Ah5zdkJZ8J8MPVqzaTk5gmZcbNYVEvG9FMyY8xMt9DqOXmR8y_GmGSSz8j9Zoc07xASvYM90j02nQtlpLmkwZUhIe08LRPk0pALhbilQ99jarvp10IsDdJbjAhlRzfwE8YC43t6uQtN6PsQMdMQPaaEW-pT19KEDsMeE_VDdCV0cUpCM-aQX5JnHpqMrx7eObn6dLY5_Vytv63OTz-uK1jUtai41NwgMK8ANYJAwZVnNejbrQTunALlhJCgFsxoYJpxEEtUUintudNazsnbQ7dP3Z8Bc7FtyA6bBiJ2Q7a8lpxxbaaJ5uTdAXWpyzmht30KLaTRcmb_722Pe0_sm4csZAeNTxBdyEdBGKnFRM7JyQG7Cw2Oj_fs6vt6uZRiEqqDEHLBv0cB0m-rtNS1_XGxsjdK35jrL5f2q_wHzkuekg</recordid><startdate>19951201</startdate><enddate>19951201</enddate><creator>Besana, G. M.</creator><creator>Shibutani, T.</creator><creator>Hirano, N.</creator><creator>Ando, M.</creator><creator>Bautista, B.</creator><creator>Narag, I.</creator><creator>Punongbayan, R. S.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>19951201</creationdate><title>The shear wave velocity structure of the crust and uppermost mantle beneath Tagaytay, Philippines inferred from receiver function analysis</title><author>Besana, G. M. ; Shibutani, T. ; Hirano, N. ; Ando, M. ; Bautista, B. ; Narag, I. ; Punongbayan, R. S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4552-13719ea0f6ae7ea2e216f05a7bd3a1cc6a6c223a64097a0701a28e63667f1c773</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1995</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Earthquakes</topic><topic>Earthquakes, seismology</topic><topic>Exact sciences and technology</topic><topic>Internal geophysics</topic><topic>Moho discontinuity</topic><topic>Philippines</topic><topic>Receivers</topic><topic>Seismic phenomena</topic><topic>Solid-earth geophysics, tectonophysics, gravimetry</topic><topic>Sound waves</topic><topic>Stations</topic><topic>Waveforms</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Besana, G. M.</creatorcontrib><creatorcontrib>Shibutani, T.</creatorcontrib><creatorcontrib>Hirano, N.</creatorcontrib><creatorcontrib>Ando, M.</creatorcontrib><creatorcontrib>Bautista, B.</creatorcontrib><creatorcontrib>Narag, I.</creatorcontrib><creatorcontrib>Punongbayan, R. S.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Besana, G. M.</au><au>Shibutani, T.</au><au>Hirano, N.</au><au>Ando, M.</au><au>Bautista, B.</au><au>Narag, I.</au><au>Punongbayan, R. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The shear wave velocity structure of the crust and uppermost mantle beneath Tagaytay, Philippines inferred from receiver function analysis</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>1995-12-01</date><risdate>1995</risdate><volume>22</volume><issue>23</issue><spage>3143</spage><epage>3146</epage><pages>3143-3146</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>Depths of the partially melted zone and the Moho discontinuity are probably at 18 kilometers and 34 kilometers, respectively beneath Tagaytay seismic station, Luzon, Philippines. This conclusion is based on the shear‐wave velocity structure determined in this study, which indicates the presence of a low‐velocity zone and high‐velocity zone at these depths. The shear wave velocity model was derived from the inversion of five receiver functions of teleseismic earthquakes recorded by the broadband seismometer at Tagaytay. However, due to the very limited information to constrain our initial model, other models with comparable waveform fit were also obtained but with deeper low velocity zone and shallower Moho.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/95GL03319</doi><tpages>4</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0094-8276 |
| ispartof | Geophysical research letters, 1995-12, Vol.22 (23), p.3143-3146 |
| issn | 0094-8276 1944-8007 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1531017900 |
| source | Wiley-Blackwell Journals |
| subjects | Earth sciences Earth, ocean, space Earthquakes Earthquakes, seismology Exact sciences and technology Internal geophysics Moho discontinuity Philippines Receivers Seismic phenomena Solid-earth geophysics, tectonophysics, gravimetry Sound waves Stations Waveforms |
| title | The shear wave velocity structure of the crust and uppermost mantle beneath Tagaytay, Philippines inferred from receiver function analysis |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-04T19%3A22%3A49IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20shear%20wave%20velocity%20structure%20of%20the%20crust%20and%20uppermost%20mantle%20beneath%20Tagaytay,%20Philippines%20inferred%20from%20receiver%20function%20analysis&rft.jtitle=Geophysical%20research%20letters&rft.au=Besana,%20G.%20M.&rft.date=1995-12-01&rft.volume=22&rft.issue=23&rft.spage=3143&rft.epage=3146&rft.pages=3143-3146&rft.issn=0094-8276&rft.eissn=1944-8007&rft.coden=GPRLAJ&rft_id=info:doi/10.1029/95GL03319&rft_dat=%3Cproquest_cross%3E1531017900%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1531017900&rft_id=info:pmid/&rfr_iscdi=true |