Reverse‐time migration from rugged topography using irregular, unstructured mesh
ABSTRACT We developed a reverse‐time migration scheme that can image regions with rugged topography without requiring any approximations by adopting an irregular, unstructured‐grid modelling scheme. This grid, which can accurately describe surface topography and interfaces between high‐velocity‐cont...
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Veröffentlicht in: | Geophysical Prospecting 2017-03, Vol.65 (2), p.453-466 |
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creator | Liu, Qiancheng Zhang, Jianfeng Gao, Hongwei |
description | ABSTRACT
We developed a reverse‐time migration scheme that can image regions with rugged topography without requiring any approximations by adopting an irregular, unstructured‐grid modelling scheme. This grid, which can accurately describe surface topography and interfaces between high‐velocity‐contrast regions, is generated by Delaunay triangulation combined with the centroidal Voronoi tessellation method. The grid sizes vary according to the migration velocities, resulting in significant reduction of the number of discretized nodes compared with the number of nodes in the conventional regular‐grid scheme, particularly in the case wherein high near‐surface velocities exist. Moreover, the time sampling rate can be reduced substantially. The grid method, together with the irregular perfectly matched layer absorbing boundary condition, enables the proposed scheme to image regions of interest using curved artificial boundaries with fewer discretized nodes. We tested the proposed scheme using the 2D SEG Foothill synthetic dataset. |
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We developed a reverse‐time migration scheme that can image regions with rugged topography without requiring any approximations by adopting an irregular, unstructured‐grid modelling scheme. This grid, which can accurately describe surface topography and interfaces between high‐velocity‐contrast regions, is generated by Delaunay triangulation combined with the centroidal Voronoi tessellation method. The grid sizes vary according to the migration velocities, resulting in significant reduction of the number of discretized nodes compared with the number of nodes in the conventional regular‐grid scheme, particularly in the case wherein high near‐surface velocities exist. Moreover, the time sampling rate can be reduced substantially. The grid method, together with the irregular perfectly matched layer absorbing boundary condition, enables the proposed scheme to image regions of interest using curved artificial boundaries with fewer discretized nodes. We tested the proposed scheme using the 2D SEG Foothill synthetic dataset.</description><identifier>ISSN: 0016-8025</identifier><identifier>EISSN: 1365-2478</identifier><identifier>DOI: 10.1111/1365-2478.12415</identifier><identifier>CODEN: GPPRAR</identifier><language>eng</language><publisher>Houten: Wiley Subscription Services, Inc</publisher><subject>Foothills ; Geophysics ; Grid method ; Migration ; Near surface ; Reduction ; Reverse‐time migration ; Sampling ; Topography ; Unstructured mesh</subject><ispartof>Geophysical Prospecting, 2017-03, Vol.65 (2), p.453-466</ispartof><rights>2016 European Association of Geoscientists & Engineers</rights><rights>2017 European Association of Geoscientists & Engineers</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4045-5b0138b0683bff9a2e422e2c6da3c094d53936e833185848c83b34a47b4fe693</citedby><cites>FETCH-LOGICAL-a4045-5b0138b0683bff9a2e422e2c6da3c094d53936e833185848c83b34a47b4fe693</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2F1365-2478.12415$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2F1365-2478.12415$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Liu, Qiancheng</creatorcontrib><creatorcontrib>Zhang, Jianfeng</creatorcontrib><creatorcontrib>Gao, Hongwei</creatorcontrib><title>Reverse‐time migration from rugged topography using irregular, unstructured mesh</title><title>Geophysical Prospecting</title><description>ABSTRACT
We developed a reverse‐time migration scheme that can image regions with rugged topography without requiring any approximations by adopting an irregular, unstructured‐grid modelling scheme. This grid, which can accurately describe surface topography and interfaces between high‐velocity‐contrast regions, is generated by Delaunay triangulation combined with the centroidal Voronoi tessellation method. The grid sizes vary according to the migration velocities, resulting in significant reduction of the number of discretized nodes compared with the number of nodes in the conventional regular‐grid scheme, particularly in the case wherein high near‐surface velocities exist. Moreover, the time sampling rate can be reduced substantially. The grid method, together with the irregular perfectly matched layer absorbing boundary condition, enables the proposed scheme to image regions of interest using curved artificial boundaries with fewer discretized nodes. We tested the proposed scheme using the 2D SEG Foothill synthetic dataset.</description><subject>Foothills</subject><subject>Geophysics</subject><subject>Grid method</subject><subject>Migration</subject><subject>Near surface</subject><subject>Reduction</subject><subject>Reverse‐time migration</subject><subject>Sampling</subject><subject>Topography</subject><subject>Unstructured mesh</subject><issn>0016-8025</issn><issn>1365-2478</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNqN0c1KAzEQB_AgCtbq2euCFw9um-_NHqVoFQSl9B6y29ntlv0y2Si9-Qg-o09iasWDF80lMPz-ITOD0DnBExLOlDApYsoTNSGUE3GARj-VQzTCmMhYYSqO0YlzG4wZFoKP0GIBL2AdfLy9D1UDUVOV1gxV10aF7ZrI-rKEVTR0fRfq_XobeVe1ZVRZC6Wvjb2KfOsG6_PB2wAbcOtTdFSY2sHZ9z1Gy9ub5ewufnic38-uH2LDMRexyDBhKsNSsawoUkOBUwo0lyvDcpzylWApk6AYI0oorvLgGDc8yXgBMmVjdLl_trfdswc36KZyOdS1aaHzThOlOKFpIpN_0IQqJiQWgV78opvO2zb0EZQUCePhP0FN9yq3nXMWCt3bqjF2qwnWu23o3ez1bvb6axshIfaJ16qG7V9cz58W-9wngvaLzA</recordid><startdate>201703</startdate><enddate>201703</enddate><creator>Liu, Qiancheng</creator><creator>Zhang, Jianfeng</creator><creator>Gao, Hongwei</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope></search><sort><creationdate>201703</creationdate><title>Reverse‐time migration from rugged topography using irregular, unstructured mesh</title><author>Liu, Qiancheng ; Zhang, Jianfeng ; Gao, Hongwei</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4045-5b0138b0683bff9a2e422e2c6da3c094d53936e833185848c83b34a47b4fe693</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Foothills</topic><topic>Geophysics</topic><topic>Grid method</topic><topic>Migration</topic><topic>Near surface</topic><topic>Reduction</topic><topic>Reverse‐time migration</topic><topic>Sampling</topic><topic>Topography</topic><topic>Unstructured mesh</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Qiancheng</creatorcontrib><creatorcontrib>Zhang, Jianfeng</creatorcontrib><creatorcontrib>Gao, Hongwei</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geophysical Prospecting</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Qiancheng</au><au>Zhang, Jianfeng</au><au>Gao, Hongwei</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Reverse‐time migration from rugged topography using irregular, unstructured mesh</atitle><jtitle>Geophysical Prospecting</jtitle><date>2017-03</date><risdate>2017</risdate><volume>65</volume><issue>2</issue><spage>453</spage><epage>466</epage><pages>453-466</pages><issn>0016-8025</issn><eissn>1365-2478</eissn><coden>GPPRAR</coden><abstract>ABSTRACT
We developed a reverse‐time migration scheme that can image regions with rugged topography without requiring any approximations by adopting an irregular, unstructured‐grid modelling scheme. This grid, which can accurately describe surface topography and interfaces between high‐velocity‐contrast regions, is generated by Delaunay triangulation combined with the centroidal Voronoi tessellation method. The grid sizes vary according to the migration velocities, resulting in significant reduction of the number of discretized nodes compared with the number of nodes in the conventional regular‐grid scheme, particularly in the case wherein high near‐surface velocities exist. Moreover, the time sampling rate can be reduced substantially. The grid method, together with the irregular perfectly matched layer absorbing boundary condition, enables the proposed scheme to image regions of interest using curved artificial boundaries with fewer discretized nodes. We tested the proposed scheme using the 2D SEG Foothill synthetic dataset.</abstract><cop>Houten</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1111/1365-2478.12415</doi><tpages>14</tpages></addata></record> |
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subjects | Foothills Geophysics Grid method Migration Near surface Reduction Reverse‐time migration Sampling Topography Unstructured mesh |
title | Reverse‐time migration from rugged topography using irregular, unstructured mesh |
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