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Amplitude spectrum compensation and phase spectrum correction of seismic data based on the generalized S transform
We propose a method for the compensation and phase correction of the amplitude spectrum based on the generalized S transform. The compensation of the amplitude spectrum within a reliable frequency range of the seismic record is performed in the S domain to restore the amplitude spectrum of reflectio...
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| Published in: | Applied geophysics 2014-12, Vol.11 (4), p.468-478 |
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| Main Authors: | , , , , , |
| Format: | Article |
| Language: | English |
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| cited_by | cdi_FETCH-LOGICAL-a437t-e3cc81caed967645ad6f9d2e7b7143f87ce8a07a85c3b729965e6d9f7cf2c4e33 |
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| cites | cdi_FETCH-LOGICAL-a437t-e3cc81caed967645ad6f9d2e7b7143f87ce8a07a85c3b729965e6d9f7cf2c4e33 |
| container_end_page | 478 |
| container_issue | 4 |
| container_start_page | 468 |
| container_title | Applied geophysics |
| container_volume | 11 |
| creator | Zhou, Huai-Lai Wang, Jun Wang, Ming-Chun Shen, Ming-Cheng Zhang, Xin-Kun Liang, Ping |
| description | We propose a method for the compensation and phase correction of the amplitude spectrum based on the generalized
S
transform. The compensation of the amplitude spectrum within a reliable frequency range of the seismic record is performed in the
S
domain to restore the amplitude spectrum of reflection. We use spectral simulation methods to fit the time-dependent amplitude spectrum and compensate for the amplitude attenuation owing to absorption. We use phase scanning to select the time-, space-, and frequencydependent phases correction based on the parsimony criterion and eliminate the residual phase effect of the wavelet in the
S
domain. The method does not directly calculate the
Q
value; thus, it can be applied to the case of variable
Q
. The comparison of the theory model and field data verify that the proposed method can recover the amplitude spectrum of the strata reflectivity, while eliminating the effect of the residual phase of the wavelet. Thus, the wavelet approaches the zero-phase wavelet and, the seismic resolution is improved. |
| doi_str_mv | 10.1007/s11770-014-0456-y |
| format | article |
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S
transform. The compensation of the amplitude spectrum within a reliable frequency range of the seismic record is performed in the
S
domain to restore the amplitude spectrum of reflection. We use spectral simulation methods to fit the time-dependent amplitude spectrum and compensate for the amplitude attenuation owing to absorption. We use phase scanning to select the time-, space-, and frequencydependent phases correction based on the parsimony criterion and eliminate the residual phase effect of the wavelet in the
S
domain. The method does not directly calculate the
Q
value; thus, it can be applied to the case of variable
Q
. The comparison of the theory model and field data verify that the proposed method can recover the amplitude spectrum of the strata reflectivity, while eliminating the effect of the residual phase of the wavelet. Thus, the wavelet approaches the zero-phase wavelet and, the seismic resolution is improved.</description><identifier>ISSN: 1672-7975</identifier><identifier>EISSN: 1993-0658</identifier><identifier>DOI: 10.1007/s11770-014-0456-y</identifier><language>eng</language><publisher>Heidelberg: Chinese Geophysical Society</publisher><subject>Amplitudes ; Compensation ; Earth and Environmental Science ; Earth Sciences ; Frequency ranges ; Geophysics ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Mathematical models ; Phase transformations ; Reflection ; Seismology ; Spectrum analysis ; Transforms ; Wavelet ; Wavelet transforms</subject><ispartof>Applied geophysics, 2014-12, Vol.11 (4), p.468-478</ispartof><rights>Editorial Office of Applied Geophysics and Springer-Verlag Berlin Heidelberg 2014</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a437t-e3cc81caed967645ad6f9d2e7b7143f87ce8a07a85c3b729965e6d9f7cf2c4e33</citedby><cites>FETCH-LOGICAL-a437t-e3cc81caed967645ad6f9d2e7b7143f87ce8a07a85c3b729965e6d9f7cf2c4e33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/yydqwl/yydqwl.jpg</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Zhou, Huai-Lai</creatorcontrib><creatorcontrib>Wang, Jun</creatorcontrib><creatorcontrib>Wang, Ming-Chun</creatorcontrib><creatorcontrib>Shen, Ming-Cheng</creatorcontrib><creatorcontrib>Zhang, Xin-Kun</creatorcontrib><creatorcontrib>Liang, Ping</creatorcontrib><title>Amplitude spectrum compensation and phase spectrum correction of seismic data based on the generalized S transform</title><title>Applied geophysics</title><addtitle>Appl. Geophys</addtitle><description>We propose a method for the compensation and phase correction of the amplitude spectrum based on the generalized
S
transform. The compensation of the amplitude spectrum within a reliable frequency range of the seismic record is performed in the
S
domain to restore the amplitude spectrum of reflection. We use spectral simulation methods to fit the time-dependent amplitude spectrum and compensate for the amplitude attenuation owing to absorption. We use phase scanning to select the time-, space-, and frequencydependent phases correction based on the parsimony criterion and eliminate the residual phase effect of the wavelet in the
S
domain. The method does not directly calculate the
Q
value; thus, it can be applied to the case of variable
Q
. The comparison of the theory model and field data verify that the proposed method can recover the amplitude spectrum of the strata reflectivity, while eliminating the effect of the residual phase of the wavelet. Thus, the wavelet approaches the zero-phase wavelet and, the seismic resolution is improved.</description><subject>Amplitudes</subject><subject>Compensation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Frequency ranges</subject><subject>Geophysics</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Mathematical models</subject><subject>Phase transformations</subject><subject>Reflection</subject><subject>Seismology</subject><subject>Spectrum analysis</subject><subject>Transforms</subject><subject>Wavelet</subject><subject>Wavelet transforms</subject><issn>1672-7975</issn><issn>1993-0658</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqFkU-L1TAUxYsoOI5-AHcBF7rpePO_WQ6Do8KAC3Ud8pKbNx3atJO0DPXTm0dFdEBc5ZLzOzeHnKZ5TeGCAuj3hVKtoQUqWhBStduT5owaw1tQsntaZ6VZq42Wz5sXpdwBKM6UOGvy5TgP_bIGJGVGv-R1JH4aZ0zFLf2UiEuBzLeu_KXnXMeTOkVSsC9j70lwiyOHCgZSheUWyRETZjf0P-rVV7Jkl0qc8viyeRbdUPDVr_O8-X794dvVp_bmy8fPV5c3rRNcLy1y7zvqHQajtBLSBRVNYKgPmgoeO-2xc6BdJz0_aGaMkqiCidpH5gVyft683fc-uBRdOtq7ac2pvmi3Ldw_DKx-FgigrJLvdnLO0_2KZbFjXzwOg0s4rcXSDjquOTX0_6hSALIDqSv65hH6OwBVQnDOpDylpDvl81RKxmjn3I8ub5aCPVVr92ptTWtP1dqtetjuKZVNR8x_bP6n6SfMUagW</recordid><startdate>20141201</startdate><enddate>20141201</enddate><creator>Zhou, Huai-Lai</creator><creator>Wang, Jun</creator><creator>Wang, Ming-Chun</creator><creator>Shen, Ming-Cheng</creator><creator>Zhang, Xin-Kun</creator><creator>Liang, Ping</creator><general>Chinese Geophysical Society</general><general>Springer Nature B.V</general><general>State Key Laboratory of 0il and Gas Reservoir Geology and Exploitation, CDUT, Chengdu 610059, China.%Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China.%Exploration and Development Institute of Bohai 0il Field of CN00C Co., Ltd Tianjin Branch, Tianjing 300452, China.%College of Geophysics, Chengdu University of Technology, Chengdu 610059, China.%College of Energy Resource, Chengdu University of Technology, Chengdu 610059, China</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>FR3</scope><scope>KR7</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20141201</creationdate><title>Amplitude spectrum compensation and phase spectrum correction of seismic data based on the generalized S transform</title><author>Zhou, Huai-Lai ; Wang, Jun ; Wang, Ming-Chun ; Shen, Ming-Cheng ; Zhang, Xin-Kun ; Liang, Ping</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a437t-e3cc81caed967645ad6f9d2e7b7143f87ce8a07a85c3b729965e6d9f7cf2c4e33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Amplitudes</topic><topic>Compensation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Frequency ranges</topic><topic>Geophysics</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Mathematical models</topic><topic>Phase transformations</topic><topic>Reflection</topic><topic>Seismology</topic><topic>Spectrum analysis</topic><topic>Transforms</topic><topic>Wavelet</topic><topic>Wavelet transforms</topic><toplevel>online_resources</toplevel><creatorcontrib>Zhou, Huai-Lai</creatorcontrib><creatorcontrib>Wang, Jun</creatorcontrib><creatorcontrib>Wang, Ming-Chun</creatorcontrib><creatorcontrib>Shen, Ming-Cheng</creatorcontrib><creatorcontrib>Zhang, Xin-Kun</creatorcontrib><creatorcontrib>Liang, Ping</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Science Database (ProQuest)</collection><collection>ProQuest advanced technologies & aerospace journals</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Applied geophysics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhou, Huai-Lai</au><au>Wang, Jun</au><au>Wang, Ming-Chun</au><au>Shen, Ming-Cheng</au><au>Zhang, Xin-Kun</au><au>Liang, Ping</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Amplitude spectrum compensation and phase spectrum correction of seismic data based on the generalized S transform</atitle><jtitle>Applied geophysics</jtitle><stitle>Appl. Geophys</stitle><date>2014-12-01</date><risdate>2014</risdate><volume>11</volume><issue>4</issue><spage>468</spage><epage>478</epage><pages>468-478</pages><issn>1672-7975</issn><eissn>1993-0658</eissn><abstract>We propose a method for the compensation and phase correction of the amplitude spectrum based on the generalized
S
transform. The compensation of the amplitude spectrum within a reliable frequency range of the seismic record is performed in the
S
domain to restore the amplitude spectrum of reflection. We use spectral simulation methods to fit the time-dependent amplitude spectrum and compensate for the amplitude attenuation owing to absorption. We use phase scanning to select the time-, space-, and frequencydependent phases correction based on the parsimony criterion and eliminate the residual phase effect of the wavelet in the
S
domain. The method does not directly calculate the
Q
value; thus, it can be applied to the case of variable
Q
. The comparison of the theory model and field data verify that the proposed method can recover the amplitude spectrum of the strata reflectivity, while eliminating the effect of the residual phase of the wavelet. Thus, the wavelet approaches the zero-phase wavelet and, the seismic resolution is improved.</abstract><cop>Heidelberg</cop><pub>Chinese Geophysical Society</pub><doi>10.1007/s11770-014-0456-y</doi><tpages>11</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1672-7975 |
| ispartof | Applied geophysics, 2014-12, Vol.11 (4), p.468-478 |
| issn | 1672-7975 1993-0658 |
| language | eng |
| recordid | cdi_wanfang_journals_yydqwl201404012 |
| source | Springer Nature |
| subjects | Amplitudes Compensation Earth and Environmental Science Earth Sciences Frequency ranges Geophysics Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Mathematical models Phase transformations Reflection Seismology Spectrum analysis Transforms Wavelet Wavelet transforms |
| title | Amplitude spectrum compensation and phase spectrum correction of seismic data based on the generalized S transform |
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