Discussion on the applicability of 90° phase conversion technique in seismic sedimentology
Since 1998, domestic and foreign scholars have conducted more systematic research on the theory and application technology of seismic sedimentology, and 90° phase conversion has been proposed as one of the core technologies of seismic sedimentology. But in actual research and application, the techno...
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creator | Zhao, Pingqi Li, Xiaoliang Zong, Jie Huang, Fang Wu, Jizhong Yang, Fei Yu, Gaoming Wei, Pengpeng |
description | Since 1998, domestic and foreign scholars have conducted more systematic research on the theory and application technology of seismic sedimentology, and 90° phase conversion has been proposed as one of the core technologies of seismic sedimentology. But in actual research and application, the technology has not achieved the expected results. The 90° phase conversion intends to give the meaning of the seismic reflection event representing the stratum interface to the lithologic strata by means of phase shift. Due to the complexity and change of the underground strata, there are usually multiple lithology frequent thin interbeds. Therefore, the event axis in the seismic profile is the combined effect of multiple sets of thin interbeds. The seismic data after 90° phase conversion cannot convert the original seismic data from interface seismic profile to lithologic stratigraphic profile, and lacks clear geological meaning. Its application ability in seismic structure interpretation and seismic lithology interpretation is very limited. Therefore, it is difficult to become an applied technology of seismic sedimentology. Therefore, it is not appropriate to use the 90° phase conversion technology as the core technology of seismic sedimentology. This technology neither improves the seismic data resolution capability nor accurately converts the seismic profile into a lithological profile. |
doi_str_mv | 10.1088/1755-1315/692/4/042127 |
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But in actual research and application, the technology has not achieved the expected results. The 90° phase conversion intends to give the meaning of the seismic reflection event representing the stratum interface to the lithologic strata by means of phase shift. Due to the complexity and change of the underground strata, there are usually multiple lithology frequent thin interbeds. Therefore, the event axis in the seismic profile is the combined effect of multiple sets of thin interbeds. The seismic data after 90° phase conversion cannot convert the original seismic data from interface seismic profile to lithologic stratigraphic profile, and lacks clear geological meaning. Its application ability in seismic structure interpretation and seismic lithology interpretation is very limited. Therefore, it is difficult to become an applied technology of seismic sedimentology. Therefore, it is not appropriate to use the 90° phase conversion technology as the core technology of seismic sedimentology. This technology neither improves the seismic data resolution capability nor accurately converts the seismic profile into a lithological profile.</description><identifier>ISSN: 1755-1307</identifier><identifier>EISSN: 1755-1315</identifier><identifier>DOI: 10.1088/1755-1315/692/4/042127</identifier><language>eng</language><publisher>Bristol: IOP Publishing</publisher><subject>Conversion ; Lithology ; Sedimentology ; Seismic analysis ; Seismic surveys ; Strata ; Stratigraphy ; Technology</subject><ispartof>IOP conference series. Earth and environmental science, 2021-03, Vol.692 (4), p.42127</ispartof><rights>2021. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). 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Earth and environmental science</title><description>Since 1998, domestic and foreign scholars have conducted more systematic research on the theory and application technology of seismic sedimentology, and 90° phase conversion has been proposed as one of the core technologies of seismic sedimentology. But in actual research and application, the technology has not achieved the expected results. The 90° phase conversion intends to give the meaning of the seismic reflection event representing the stratum interface to the lithologic strata by means of phase shift. Due to the complexity and change of the underground strata, there are usually multiple lithology frequent thin interbeds. Therefore, the event axis in the seismic profile is the combined effect of multiple sets of thin interbeds. The seismic data after 90° phase conversion cannot convert the original seismic data from interface seismic profile to lithologic stratigraphic profile, and lacks clear geological meaning. Its application ability in seismic structure interpretation and seismic lithology interpretation is very limited. Therefore, it is difficult to become an applied technology of seismic sedimentology. Therefore, it is not appropriate to use the 90° phase conversion technology as the core technology of seismic sedimentology. This technology neither improves the seismic data resolution capability nor accurately converts the seismic profile into a lithological profile.</description><subject>Conversion</subject><subject>Lithology</subject><subject>Sedimentology</subject><subject>Seismic analysis</subject><subject>Seismic surveys</subject><subject>Strata</subject><subject>Stratigraphy</subject><subject>Technology</subject><issn>1755-1307</issn><issn>1755-1315</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</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>eNo9kNFKwzAUhoMoOKevIAGva3OSpmkuZeoUBt7olRchTROX0TU16YS9lc_gk9k6GRz4D_w_5_x8CF0DuQVSVTkIzjNgwPNS0rzISUGBihM0Oxqnx52Ic3SR0oaQUhRMztD7vU9ml5IPHR5nWFus-771Rte-9cMeB4cl-fnG_Voni03ovmz8Sw_WrDv_ubPYdzhZn7bejNr4re2G0IaP_SU6c7pN9upf5-jt8eF18ZStXpbPi7tVZuhYKKsMK6UGWzEnCmIdJ64WXIJrGDHQlNo1peXASe2cYGVFagkawDrjZGNBsjm6OdztYxj7pEFtwi5240tFOVAqZVFNqfKQMjGkFK1TffRbHfcKiJpAqomRmnipEaQq1AEk-wVi_2gF</recordid><startdate>20210301</startdate><enddate>20210301</enddate><creator>Zhao, Pingqi</creator><creator>Li, Xiaoliang</creator><creator>Zong, Jie</creator><creator>Huang, Fang</creator><creator>Wu, Jizhong</creator><creator>Yang, Fei</creator><creator>Yu, Gaoming</creator><creator>Wei, Pengpeng</creator><general>IOP Publishing</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PYCSY</scope></search><sort><creationdate>20210301</creationdate><title>Discussion on the applicability of 90° phase conversion technique in seismic sedimentology</title><author>Zhao, Pingqi ; Li, Xiaoliang ; Zong, Jie ; Huang, Fang ; Wu, Jizhong ; Yang, Fei ; Yu, Gaoming ; Wei, Pengpeng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2307-8c369a1e83f740ef50fb7591fd30c1d6afd6e5150bff73680b91a11efcf9de193</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Conversion</topic><topic>Lithology</topic><topic>Sedimentology</topic><topic>Seismic analysis</topic><topic>Seismic surveys</topic><topic>Strata</topic><topic>Stratigraphy</topic><topic>Technology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhao, Pingqi</creatorcontrib><creatorcontrib>Li, Xiaoliang</creatorcontrib><creatorcontrib>Zong, Jie</creatorcontrib><creatorcontrib>Huang, Fang</creatorcontrib><creatorcontrib>Wu, Jizhong</creatorcontrib><creatorcontrib>Yang, Fei</creatorcontrib><creatorcontrib>Yu, Gaoming</creatorcontrib><creatorcontrib>Wei, Pengpeng</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content 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 China</collection><collection>Environmental Science Collection</collection><jtitle>IOP conference series. Earth and environmental science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhao, Pingqi</au><au>Li, Xiaoliang</au><au>Zong, Jie</au><au>Huang, Fang</au><au>Wu, Jizhong</au><au>Yang, Fei</au><au>Yu, Gaoming</au><au>Wei, Pengpeng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Discussion on the applicability of 90° phase conversion technique in seismic sedimentology</atitle><jtitle>IOP conference series. Earth and environmental science</jtitle><date>2021-03-01</date><risdate>2021</risdate><volume>692</volume><issue>4</issue><spage>42127</spage><pages>42127-</pages><issn>1755-1307</issn><eissn>1755-1315</eissn><abstract>Since 1998, domestic and foreign scholars have conducted more systematic research on the theory and application technology of seismic sedimentology, and 90° phase conversion has been proposed as one of the core technologies of seismic sedimentology. But in actual research and application, the technology has not achieved the expected results. The 90° phase conversion intends to give the meaning of the seismic reflection event representing the stratum interface to the lithologic strata by means of phase shift. Due to the complexity and change of the underground strata, there are usually multiple lithology frequent thin interbeds. Therefore, the event axis in the seismic profile is the combined effect of multiple sets of thin interbeds. The seismic data after 90° phase conversion cannot convert the original seismic data from interface seismic profile to lithologic stratigraphic profile, and lacks clear geological meaning. Its application ability in seismic structure interpretation and seismic lithology interpretation is very limited. Therefore, it is difficult to become an applied technology of seismic sedimentology. Therefore, it is not appropriate to use the 90° phase conversion technology as the core technology of seismic sedimentology. This technology neither improves the seismic data resolution capability nor accurately converts the seismic profile into a lithological profile.</abstract><cop>Bristol</cop><pub>IOP Publishing</pub><doi>10.1088/1755-1315/692/4/042127</doi><oa>free_for_read</oa></addata></record> |
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subjects | Conversion Lithology Sedimentology Seismic analysis Seismic surveys Strata Stratigraphy Technology |
title | Discussion on the applicability of 90° phase conversion technique in seismic sedimentology |
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