Converted-wave diodic moveout and application in the land gas cloud area
PS converted-waves (C-waves) have been commonly used to image through gas clouds but the C-wave imaging may also be degraded by the diodic effect introduced by the gas cloud. It may be compensated for using a velocity perturbation method which decouples the diodic moveout into two parts: the base ve...
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description | PS converted-waves (C-waves) have been commonly used to image through gas clouds but the C-wave imaging may also be degraded by the diodic effect introduced by the gas cloud. It may be compensated for using a velocity perturbation method which decouples the diodic moveout into two parts: the base velocity and the velocity perturbation. Gas clouds are widely distributed in the Sanhu area in the Qaidam basin of northwest China which is rich in natural gas. A land 2D3C seismic dataset is analyzed from the Sanhu area and significant diodic effects are observed in the data which harm the C-wave imaging. The diodic correction is applied to this data and the resultant C-wave imaging and the details of the reservoir structure are significantly improved. The diodic moveout plays an important role in working out the residual shear wave statics and the association of diodic correction and shear wave residual statics computation is a key step of C-wave high fidelity imaging in the gas cloud area. Finally, the new process workflow with diodic moveout is given. |
doi_str_mv | 10.1007/s11770-011-0291-3 |
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It may be compensated for using a velocity perturbation method which decouples the diodic moveout into two parts: the base velocity and the velocity perturbation. Gas clouds are widely distributed in the Sanhu area in the Qaidam basin of northwest China which is rich in natural gas. A land 2D3C seismic dataset is analyzed from the Sanhu area and significant diodic effects are observed in the data which harm the C-wave imaging. The diodic correction is applied to this data and the resultant C-wave imaging and the details of the reservoir structure are significantly improved. The diodic moveout plays an important role in working out the residual shear wave statics and the association of diodic correction and shear wave residual statics computation is a key step of C-wave high fidelity imaging in the gas cloud area. Finally, the new process workflow with diodic moveout is given.</description><identifier>ISSN: 1672-7975</identifier><identifier>EISSN: 1993-0658</identifier><identifier>DOI: 10.1007/s11770-011-0291-3</identifier><language>eng</language><publisher>Heidelberg: Chinese Geophysical Society</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Gases ; Geophysics ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Natural gas ; Velocity</subject><ispartof>Applied geophysics, 2011-09, Vol.8 (3), p.171-180</ispartof><rights>Editorial Office of Applied Geophysics and Springer-Verlag Berlin Heidelberg 2011</rights><rights>Copyright © Wanfang Data Co. Ltd. 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Geophys</addtitle><description>PS converted-waves (C-waves) have been commonly used to image through gas clouds but the C-wave imaging may also be degraded by the diodic effect introduced by the gas cloud. It may be compensated for using a velocity perturbation method which decouples the diodic moveout into two parts: the base velocity and the velocity perturbation. Gas clouds are widely distributed in the Sanhu area in the Qaidam basin of northwest China which is rich in natural gas. A land 2D3C seismic dataset is analyzed from the Sanhu area and significant diodic effects are observed in the data which harm the C-wave imaging. The diodic correction is applied to this data and the resultant C-wave imaging and the details of the reservoir structure are significantly improved. The diodic moveout plays an important role in working out the residual shear wave statics and the association of diodic correction and shear wave residual statics computation is a key step of C-wave high fidelity imaging in the gas cloud area. Finally, the new process workflow with diodic moveout is given.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Gases</subject><subject>Geophysics</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Natural gas</subject><subject>Velocity</subject><issn>1672-7975</issn><issn>1993-0658</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kV9LwzAUxYsoOKcfwLfii0_Rm__Nowx1wsAXfQ5pk86OrtmSbmPf3pSKA8GnGy6_c3KSk2W3GB4wgHyMGEsJCDBGQBRG9CybYKUoAsGL83QWkiCpJL_MrmJcAQhKBJtk85nv9i70zqKD2bvcNt42Vb72e-d3fW46m5vNpm0q0ze-y5su779c3g77pYl51fpdIoIz19lFbdrobn7mNPt8ef6YzdHi_fVt9rRAhgHpkZGkEAqXQgCueWkllCBLzh3D1haKsJoScLx01DDKBcHOUkOBG6tEhVVBp9n96HswXW26pV75XejSjfp4tNtDS9IXAAWgJ3IT_HbnYq_XTaxcm8Knt0WtOBNMEhg87_6Qv6aFKhhQxkmC8AhVwccYXK03oVmbcNQY9NCBHjvQKYAeOtBDBDJqYmK7pQsn4_9F36qPhx4</recordid><startdate>20110901</startdate><enddate>20110901</enddate><creator>Zhang, Si-Hai</creator><creator>Li, Xiang-Yang</creator><creator>Dai, Heng-Chang</creator><general>Chinese Geophysical Society</general><general>Springer Nature B.V</general><general>State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249 China</general><general>CNPC Key Laboratory of Geophysical Prospecting, China University of Petroleum, Beijing 102249 China%CNPC Key Laboratory of Geophysical Prospecting, China University of Petroleum, Beijing 102249 China</general><general>Edinburgh Anisotropy Project, British Geophysical Survey, Edinburgh EH9 3LA, U.K.%Edinburgh Anisotropy Project, British Geophysical Survey, Edinburgh EH9 3LA, U.K</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20110901</creationdate><title>Converted-wave diodic moveout and application in the land gas cloud area</title><author>Zhang, Si-Hai ; 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Geophys</stitle><date>2011-09-01</date><risdate>2011</risdate><volume>8</volume><issue>3</issue><spage>171</spage><epage>180</epage><pages>171-180</pages><issn>1672-7975</issn><eissn>1993-0658</eissn><abstract>PS converted-waves (C-waves) have been commonly used to image through gas clouds but the C-wave imaging may also be degraded by the diodic effect introduced by the gas cloud. It may be compensated for using a velocity perturbation method which decouples the diodic moveout into two parts: the base velocity and the velocity perturbation. Gas clouds are widely distributed in the Sanhu area in the Qaidam basin of northwest China which is rich in natural gas. A land 2D3C seismic dataset is analyzed from the Sanhu area and significant diodic effects are observed in the data which harm the C-wave imaging. The diodic correction is applied to this data and the resultant C-wave imaging and the details of the reservoir structure are significantly improved. The diodic moveout plays an important role in working out the residual shear wave statics and the association of diodic correction and shear wave residual statics computation is a key step of C-wave high fidelity imaging in the gas cloud area. Finally, the new process workflow with diodic moveout is given.</abstract><cop>Heidelberg</cop><pub>Chinese Geophysical Society</pub><doi>10.1007/s11770-011-0291-3</doi><tpages>10</tpages></addata></record> |
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title | Converted-wave diodic moveout and application in the land gas cloud area |
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