Seismic Interferometry in Linear Radon Domain Applying to Noise Passive Data
We explored a new method for noise passive data to retrieve the virtual-source gathers in linear Radon domain. Seismic interferometry based on the cross correlation algorithm can be viewed as cancellation of a common part of a raypath from a physical source to two different receivers, and a stacking...
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Veröffentlicht in: | IEEE geoscience and remote sensing letters 2022, Vol.19, p.1-5 |
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description | We explored a new method for noise passive data to retrieve the virtual-source gathers in linear Radon domain. Seismic interferometry based on the cross correlation algorithm can be viewed as cancellation of a common part of a raypath from a physical source to two different receivers, and a stacking operator is then applied to the crosscorrelagram to take advantage of the contributions from all the sources. As the contributions of retrieving the virtual-shot gathers mainly come from the stationary-phase point, limited passive data with the same ray-parameter plays the major role. That is, the interference effects of most of passive data are counteracted through stacking with each other. Seismic interferometry in linear-Radon domain is proposed for selecting traces with the same ray parameters to retrieve the virtual-shot gathers. As the common-receiver gathers are needed by linear-Radon interferometry, a rearranged operator is used to rearrange noise passive data according to the periodicity. In this way, the common-receiver gathers of noise passive data can be obtained. Then, the common-receiver gathers are transformed into linear-Radon domain and the selected-ray range is used for cross correlation, which can save the computation time significantly. That has important practical significance in processing noise passive data. |
doi_str_mv | 10.1109/LGRS.2021.3088141 |
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Seismic interferometry based on the cross correlation algorithm can be viewed as cancellation of a common part of a raypath from a physical source to two different receivers, and a stacking operator is then applied to the crosscorrelagram to take advantage of the contributions from all the sources. As the contributions of retrieving the virtual-shot gathers mainly come from the stationary-phase point, limited passive data with the same ray-parameter plays the major role. That is, the interference effects of most of passive data are counteracted through stacking with each other. Seismic interferometry in linear-Radon domain is proposed for selecting traces with the same ray parameters to retrieve the virtual-shot gathers. As the common-receiver gathers are needed by linear-Radon interferometry, a rearranged operator is used to rearrange noise passive data according to the periodicity. In this way, the common-receiver gathers of noise passive data can be obtained. Then, the common-receiver gathers are transformed into linear-Radon domain and the selected-ray range is used for cross correlation, which can save the computation time significantly. That has important practical significance in processing noise passive data.</description><identifier>ISSN: 1545-598X</identifier><identifier>EISSN: 1558-0571</identifier><identifier>DOI: 10.1109/LGRS.2021.3088141</identifier><identifier>CODEN: IGRSBY</identifier><language>eng</language><publisher>Piscataway: IEEE</publisher><subject>Algorithms ; Computation ; Computational efficiency ; Correlation ; Cross correlation ; Domains ; Interferometry ; linear-Radon transform ; Noise ; noise passive-seismic data ; Parameters ; Periodicity ; Radon ; rearrange operator ; Receivers ; seismic interferometry ; Stacking ; Time-domain analysis ; Transforms</subject><ispartof>IEEE geoscience and remote sensing letters, 2022, Vol.19, p.1-5</ispartof><rights>Copyright The Institute of Electrical and Electronics Engineers, Inc. (IEEE) 2022</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c245t-9e78ae7397756796e653cf2ed71675385e6a7f8e44914ae3158fd716268052ec3</cites><orcidid>0000-0003-1374-7499 ; 0000-0001-8369-5255</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://ieeexplore.ieee.org/document/9461868$$EHTML$$P50$$Gieee$$H</linktohtml><link.rule.ids>314,776,780,792,4010,27900,27901,27902,54733</link.rule.ids><linktorsrc>$$Uhttps://ieeexplore.ieee.org/document/9461868$$EView_record_in_IEEE$$FView_record_in_$$GIEEE</linktorsrc></links><search><creatorcontrib>Wang, Xiannan</creatorcontrib><creatorcontrib>Zhang, Jian</creatorcontrib><creatorcontrib>Guo, Cean</creatorcontrib><creatorcontrib>Zhao, Shuang</creatorcontrib><creatorcontrib>Cheng, Hao</creatorcontrib><title>Seismic Interferometry in Linear Radon Domain Applying to Noise Passive Data</title><title>IEEE geoscience and remote sensing letters</title><addtitle>LGRS</addtitle><description>We explored a new method for noise passive data to retrieve the virtual-source gathers in linear Radon domain. Seismic interferometry based on the cross correlation algorithm can be viewed as cancellation of a common part of a raypath from a physical source to two different receivers, and a stacking operator is then applied to the crosscorrelagram to take advantage of the contributions from all the sources. As the contributions of retrieving the virtual-shot gathers mainly come from the stationary-phase point, limited passive data with the same ray-parameter plays the major role. That is, the interference effects of most of passive data are counteracted through stacking with each other. Seismic interferometry in linear-Radon domain is proposed for selecting traces with the same ray parameters to retrieve the virtual-shot gathers. As the common-receiver gathers are needed by linear-Radon interferometry, a rearranged operator is used to rearrange noise passive data according to the periodicity. In this way, the common-receiver gathers of noise passive data can be obtained. Then, the common-receiver gathers are transformed into linear-Radon domain and the selected-ray range is used for cross correlation, which can save the computation time significantly. That has important practical significance in processing noise passive data.</description><subject>Algorithms</subject><subject>Computation</subject><subject>Computational efficiency</subject><subject>Correlation</subject><subject>Cross correlation</subject><subject>Domains</subject><subject>Interferometry</subject><subject>linear-Radon transform</subject><subject>Noise</subject><subject>noise passive-seismic data</subject><subject>Parameters</subject><subject>Periodicity</subject><subject>Radon</subject><subject>rearrange operator</subject><subject>Receivers</subject><subject>seismic interferometry</subject><subject>Stacking</subject><subject>Time-domain analysis</subject><subject>Transforms</subject><issn>1545-598X</issn><issn>1558-0571</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>RIE</sourceid><recordid>eNo9kN9LwzAQgIMoOKd_gPgS8Lkzl-ZXH8emc1BUNgXfQuiukrE2M-mE_fe2THy64-67O-4j5BbYBIAVD-VitZ5wxmGSM2NAwBkZgZQmY1LD-ZALmcnCfF6Sq5S2jHFhjB6Rco0-Nb6iy7bDWGMMDXbxSH1LS9-ii3TlNqGl89C4vjbd73dH337RLtCX4BPSN5eS_0E6d527Jhe12yW8-Ytj8vH0-D57zsrXxXI2LbOKC9llBWrjUOeF1lLpQqGSeVVz3GhQWuZGonK6NihEAcJhDtLUQ48rwyTHKh-T-9PefQzfB0yd3YZDbPuTlqv-a4Ae7Ck4UVUMKUWs7T76xsWjBWYHaXaQZgdp9k9aP3N3mvGI-M8XQoFRJv8FcvtmwA</recordid><startdate>2022</startdate><enddate>2022</enddate><creator>Wang, Xiannan</creator><creator>Zhang, Jian</creator><creator>Guo, Cean</creator><creator>Zhao, Shuang</creator><creator>Cheng, Hao</creator><general>IEEE</general><general>The Institute of Electrical and Electronics Engineers, Inc. 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Seismic interferometry based on the cross correlation algorithm can be viewed as cancellation of a common part of a raypath from a physical source to two different receivers, and a stacking operator is then applied to the crosscorrelagram to take advantage of the contributions from all the sources. As the contributions of retrieving the virtual-shot gathers mainly come from the stationary-phase point, limited passive data with the same ray-parameter plays the major role. That is, the interference effects of most of passive data are counteracted through stacking with each other. Seismic interferometry in linear-Radon domain is proposed for selecting traces with the same ray parameters to retrieve the virtual-shot gathers. As the common-receiver gathers are needed by linear-Radon interferometry, a rearranged operator is used to rearrange noise passive data according to the periodicity. In this way, the common-receiver gathers of noise passive data can be obtained. Then, the common-receiver gathers are transformed into linear-Radon domain and the selected-ray range is used for cross correlation, which can save the computation time significantly. That has important practical significance in processing noise passive data.</abstract><cop>Piscataway</cop><pub>IEEE</pub><doi>10.1109/LGRS.2021.3088141</doi><tpages>5</tpages><orcidid>https://orcid.org/0000-0003-1374-7499</orcidid><orcidid>https://orcid.org/0000-0001-8369-5255</orcidid></addata></record> |
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subjects | Algorithms Computation Computational efficiency Correlation Cross correlation Domains Interferometry linear-Radon transform Noise noise passive-seismic data Parameters Periodicity Radon rearrange operator Receivers seismic interferometry Stacking Time-domain analysis Transforms |
title | Seismic Interferometry in Linear Radon Domain Applying to Noise Passive Data |
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