Channel Sandstone Architecture Characterization by Seismic Simulation
To describe the distribution of sandstone reservoirs between wells finely, this paper takes the sandstone reservoir of Layer N m II-4 in Qinhuangdao 32–6 Oilfield for example, and uses the seismic forward simulation and well loggings to study the channel sandstone reservoir. Under the guidance of th...
Gespeichert in:
| Veröffentlicht in: | Journal of earth science (Wuhan, China) China), 2019-08, Vol.30 (4), p.799-808 |
|---|---|
| Hauptverfasser: | , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 808 |
|---|---|
| container_issue | 4 |
| container_start_page | 799 |
| container_title | Journal of earth science (Wuhan, China) |
| container_volume | 30 |
| creator | Liang, Hongwei Zhao, Xiaoqing Mu, Longxin Fan, Zifei Zhao, Lun Wu, Shenghe |
| description | To describe the distribution of sandstone reservoirs between wells finely, this paper takes the sandstone reservoir of Layer N
m
II-4 in Qinhuangdao 32–6 Oilfield for example, and uses the seismic forward simulation and well loggings to study the channel sandstone reservoir. Under the guidance of the modern rivers and outcrops sandstone distribution pattern, the predicting limitations of the seismic forward simulation about channel sandstone boundaries such as mudstone interlayer between channel sandstone and elevation distance between adjacent channel sandstone are clear. The research shows that the mudstone interlayer can be described by seismic forward simulation seismic when the mudstone interlayer is thicker than 2 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak when the main frequency of seismic data is nearly 60 Hz. And the elevation distance between adjacent channel sandstone can be described by the seismic forward simulation when elevation distance is longer than 6 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak. And the seismic waveform features of single channel sandstone boundaries such as elevation distance between channels, overbank sandstone and abandoned channels. Under the study mentioned above, the single channel boundaries are described in Layer N
m
II-4 of Qinhuangdao 32–6 Oilfield, and the predicting boundaries are confirmed by the chemical tracers. The results show that the channel sandstone reservoir architecture characterization can be improved by the seismic forward simulation. |
| doi_str_mv | 10.1007/s12583-017-0971-x |
| format | Article |
| fullrecord | <record><control><sourceid>wanfang_jour_proqu</sourceid><recordid>TN_cdi_wanfang_journals_dqkx_e201904010</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><wanfj_id>dqkx_e201904010</wanfj_id><sourcerecordid>dqkx_e201904010</sourcerecordid><originalsourceid>FETCH-LOGICAL-a371t-ada33117163be0fabc05452de4a7a889899c645cd7dcda161ccd7b53d78fcb283</originalsourceid><addsrcrecordid>eNp1kE9LAzEQxYMoWGo_gLcFD56imWR3kz2WUv9AwUMVegvZJNtubbNtsoutn960K3hyLjPM_N4beAjdAnkAQvhjAJoJhglwTAoO-HCBBiByjgFgcRnnnKc4FXxxjUYhrEksRrkAPkDTyUo5ZzfJXDkT2sbZZOz1qm6tbjtvk3j2SrfW19-qrRuXlMdkbuuwrXUyr7fd5ry9QVeV2gQ7-u1D9PE0fZ-84Nnb8-tkPMOKcWixMooxAA45Ky2pVKlJlmbU2FRxJUQhikLnaaYNN9ooyEHHscyY4aLSJRVsiO573y_lKuWWct103sWP0uw_D9JSAgVJCZBI3vXkzjf7zob2D6U0P0HZ2Q96SvsmBG8rufP1VvmjBCJP0co-Whmjlado5SFqaK8JkXVL6_-c_xf9AJz8fHA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2269040528</pqid></control><display><type>article</type><title>Channel Sandstone Architecture Characterization by Seismic Simulation</title><source>SpringerLink Journals (MCLS)</source><source>Alma/SFX Local Collection</source><creator>Liang, Hongwei ; Zhao, Xiaoqing ; Mu, Longxin ; Fan, Zifei ; Zhao, Lun ; Wu, Shenghe</creator><creatorcontrib>Liang, Hongwei ; Zhao, Xiaoqing ; Mu, Longxin ; Fan, Zifei ; Zhao, Lun ; Wu, Shenghe</creatorcontrib><description>To describe the distribution of sandstone reservoirs between wells finely, this paper takes the sandstone reservoir of Layer N
m
II-4 in Qinhuangdao 32–6 Oilfield for example, and uses the seismic forward simulation and well loggings to study the channel sandstone reservoir. Under the guidance of the modern rivers and outcrops sandstone distribution pattern, the predicting limitations of the seismic forward simulation about channel sandstone boundaries such as mudstone interlayer between channel sandstone and elevation distance between adjacent channel sandstone are clear. The research shows that the mudstone interlayer can be described by seismic forward simulation seismic when the mudstone interlayer is thicker than 2 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak when the main frequency of seismic data is nearly 60 Hz. And the elevation distance between adjacent channel sandstone can be described by the seismic forward simulation when elevation distance is longer than 6 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak. And the seismic waveform features of single channel sandstone boundaries such as elevation distance between channels, overbank sandstone and abandoned channels. Under the study mentioned above, the single channel boundaries are described in Layer N
m
II-4 of Qinhuangdao 32–6 Oilfield, and the predicting boundaries are confirmed by the chemical tracers. The results show that the channel sandstone reservoir architecture characterization can be improved by the seismic forward simulation.</description><identifier>ISSN: 1674-487X</identifier><identifier>EISSN: 1867-111X</identifier><identifier>DOI: 10.1007/s12583-017-0971-x</identifier><language>eng</language><publisher>Wuhan: China University of Geosciences</publisher><subject>Architecture ; Biogeosciences ; Boundaries ; Channels ; Distance ; Distribution ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Geology ; Geotechnical Engineering & Applied Earth Sciences ; Interlayers ; Mudstone ; Oil and gas fields ; Oil field equipment ; Oil fields ; Organic chemistry ; Outcrops ; Reservoirs ; Rivers ; Sandstone ; Sedimentary rocks ; Seismic data ; Seismic simulators ; Simulation ; Tracers</subject><ispartof>Journal of earth science (Wuhan, China), 2019-08, Vol.30 (4), p.799-808</ispartof><rights>China University of Geosciences (Wuhan) and Springer-Verlag GmbH Germany, Part of Springer Nature 2019</rights><rights>Copyright Springer Nature B.V. 2019</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a371t-ada33117163be0fabc05452de4a7a889899c645cd7dcda161ccd7b53d78fcb283</citedby><cites>FETCH-LOGICAL-a371t-ada33117163be0fabc05452de4a7a889899c645cd7dcda161ccd7b53d78fcb283</cites><orcidid>0000-0001-5523-3053</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/dqkx-e/dqkx-e.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12583-017-0971-x$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12583-017-0971-x$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Liang, Hongwei</creatorcontrib><creatorcontrib>Zhao, Xiaoqing</creatorcontrib><creatorcontrib>Mu, Longxin</creatorcontrib><creatorcontrib>Fan, Zifei</creatorcontrib><creatorcontrib>Zhao, Lun</creatorcontrib><creatorcontrib>Wu, Shenghe</creatorcontrib><title>Channel Sandstone Architecture Characterization by Seismic Simulation</title><title>Journal of earth science (Wuhan, China)</title><addtitle>J. Earth Sci</addtitle><description>To describe the distribution of sandstone reservoirs between wells finely, this paper takes the sandstone reservoir of Layer N
m
II-4 in Qinhuangdao 32–6 Oilfield for example, and uses the seismic forward simulation and well loggings to study the channel sandstone reservoir. Under the guidance of the modern rivers and outcrops sandstone distribution pattern, the predicting limitations of the seismic forward simulation about channel sandstone boundaries such as mudstone interlayer between channel sandstone and elevation distance between adjacent channel sandstone are clear. The research shows that the mudstone interlayer can be described by seismic forward simulation seismic when the mudstone interlayer is thicker than 2 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak when the main frequency of seismic data is nearly 60 Hz. And the elevation distance between adjacent channel sandstone can be described by the seismic forward simulation when elevation distance is longer than 6 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak. And the seismic waveform features of single channel sandstone boundaries such as elevation distance between channels, overbank sandstone and abandoned channels. Under the study mentioned above, the single channel boundaries are described in Layer N
m
II-4 of Qinhuangdao 32–6 Oilfield, and the predicting boundaries are confirmed by the chemical tracers. The results show that the channel sandstone reservoir architecture characterization can be improved by the seismic forward simulation.</description><subject>Architecture</subject><subject>Biogeosciences</subject><subject>Boundaries</subject><subject>Channels</subject><subject>Distance</subject><subject>Distribution</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Interlayers</subject><subject>Mudstone</subject><subject>Oil and gas fields</subject><subject>Oil field equipment</subject><subject>Oil fields</subject><subject>Organic chemistry</subject><subject>Outcrops</subject><subject>Reservoirs</subject><subject>Rivers</subject><subject>Sandstone</subject><subject>Sedimentary rocks</subject><subject>Seismic data</subject><subject>Seismic simulators</subject><subject>Simulation</subject><subject>Tracers</subject><issn>1674-487X</issn><issn>1867-111X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp1kE9LAzEQxYMoWGo_gLcFD56imWR3kz2WUv9AwUMVegvZJNtubbNtsoutn960K3hyLjPM_N4beAjdAnkAQvhjAJoJhglwTAoO-HCBBiByjgFgcRnnnKc4FXxxjUYhrEksRrkAPkDTyUo5ZzfJXDkT2sbZZOz1qm6tbjtvk3j2SrfW19-qrRuXlMdkbuuwrXUyr7fd5ry9QVeV2gQ7-u1D9PE0fZ-84Nnb8-tkPMOKcWixMooxAA45Ky2pVKlJlmbU2FRxJUQhikLnaaYNN9ooyEHHscyY4aLSJRVsiO573y_lKuWWct103sWP0uw_D9JSAgVJCZBI3vXkzjf7zob2D6U0P0HZ2Q96SvsmBG8rufP1VvmjBCJP0co-Whmjlado5SFqaK8JkXVL6_-c_xf9AJz8fHA</recordid><startdate>20190801</startdate><enddate>20190801</enddate><creator>Liang, Hongwei</creator><creator>Zhao, Xiaoqing</creator><creator>Mu, Longxin</creator><creator>Fan, Zifei</creator><creator>Zhao, Lun</creator><creator>Wu, Shenghe</creator><general>China University of Geosciences</general><general>Springer Nature B.V</general><general>Research Institute of Petroleum Exploration and Development, Beijing 100083, China%Geophysical Research Center, Bureau of Geophysical Prospecting Incorporation, CNPC, Baoding 072751, China%College of Geosciences, China University of Petroleum, Beijing 102249, China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TN</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>SOI</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope><orcidid>https://orcid.org/0000-0001-5523-3053</orcidid></search><sort><creationdate>20190801</creationdate><title>Channel Sandstone Architecture Characterization by Seismic Simulation</title><author>Liang, Hongwei ; Zhao, Xiaoqing ; Mu, Longxin ; Fan, Zifei ; Zhao, Lun ; Wu, Shenghe</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a371t-ada33117163be0fabc05452de4a7a889899c645cd7dcda161ccd7b53d78fcb283</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Architecture</topic><topic>Biogeosciences</topic><topic>Boundaries</topic><topic>Channels</topic><topic>Distance</topic><topic>Distribution</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Interlayers</topic><topic>Mudstone</topic><topic>Oil and gas fields</topic><topic>Oil field equipment</topic><topic>Oil fields</topic><topic>Organic chemistry</topic><topic>Outcrops</topic><topic>Reservoirs</topic><topic>Rivers</topic><topic>Sandstone</topic><topic>Sedimentary rocks</topic><topic>Seismic data</topic><topic>Seismic simulators</topic><topic>Simulation</topic><topic>Tracers</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liang, Hongwei</creatorcontrib><creatorcontrib>Zhao, Xiaoqing</creatorcontrib><creatorcontrib>Mu, Longxin</creatorcontrib><creatorcontrib>Fan, Zifei</creatorcontrib><creatorcontrib>Zhao, Lun</creatorcontrib><creatorcontrib>Wu, Shenghe</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace 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><collection>Advanced Technologies Database with Aerospace</collection><collection>Environment 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>Journal of earth science (Wuhan, China)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liang, Hongwei</au><au>Zhao, Xiaoqing</au><au>Mu, Longxin</au><au>Fan, Zifei</au><au>Zhao, Lun</au><au>Wu, Shenghe</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Channel Sandstone Architecture Characterization by Seismic Simulation</atitle><jtitle>Journal of earth science (Wuhan, China)</jtitle><stitle>J. Earth Sci</stitle><date>2019-08-01</date><risdate>2019</risdate><volume>30</volume><issue>4</issue><spage>799</spage><epage>808</epage><pages>799-808</pages><issn>1674-487X</issn><eissn>1867-111X</eissn><abstract>To describe the distribution of sandstone reservoirs between wells finely, this paper takes the sandstone reservoir of Layer N
m
II-4 in Qinhuangdao 32–6 Oilfield for example, and uses the seismic forward simulation and well loggings to study the channel sandstone reservoir. Under the guidance of the modern rivers and outcrops sandstone distribution pattern, the predicting limitations of the seismic forward simulation about channel sandstone boundaries such as mudstone interlayer between channel sandstone and elevation distance between adjacent channel sandstone are clear. The research shows that the mudstone interlayer can be described by seismic forward simulation seismic when the mudstone interlayer is thicker than 2 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak when the main frequency of seismic data is nearly 60 Hz. And the elevation distance between adjacent channel sandstone can be described by the seismic forward simulation when elevation distance is longer than 6 m and the channel sandstone is thicker than 10 m because of the appearance of the seismic peak. And the seismic waveform features of single channel sandstone boundaries such as elevation distance between channels, overbank sandstone and abandoned channels. Under the study mentioned above, the single channel boundaries are described in Layer N
m
II-4 of Qinhuangdao 32–6 Oilfield, and the predicting boundaries are confirmed by the chemical tracers. The results show that the channel sandstone reservoir architecture characterization can be improved by the seismic forward simulation.</abstract><cop>Wuhan</cop><pub>China University of Geosciences</pub><doi>10.1007/s12583-017-0971-x</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0001-5523-3053</orcidid></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1674-487X |
| ispartof | Journal of earth science (Wuhan, China), 2019-08, Vol.30 (4), p.799-808 |
| issn | 1674-487X 1867-111X |
| language | eng |
| recordid | cdi_wanfang_journals_dqkx_e201904010 |
| source | SpringerLink Journals (MCLS); Alma/SFX Local Collection |
| subjects | Architecture Biogeosciences Boundaries Channels Distance Distribution Earth and Environmental Science Earth Sciences Geochemistry Geology Geotechnical Engineering & Applied Earth Sciences Interlayers Mudstone Oil and gas fields Oil field equipment Oil fields Organic chemistry Outcrops Reservoirs Rivers Sandstone Sedimentary rocks Seismic data Seismic simulators Simulation Tracers |
| title | Channel Sandstone Architecture Characterization by Seismic Simulation |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-29T00%3A57%3A52IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Channel%20Sandstone%20Architecture%20Characterization%20by%20Seismic%20Simulation&rft.jtitle=Journal%20of%20earth%20science%20(Wuhan,%20China)&rft.au=Liang,%20Hongwei&rft.date=2019-08-01&rft.volume=30&rft.issue=4&rft.spage=799&rft.epage=808&rft.pages=799-808&rft.issn=1674-487X&rft.eissn=1867-111X&rft_id=info:doi/10.1007/s12583-017-0971-x&rft_dat=%3Cwanfang_jour_proqu%3Edqkx_e201904010%3C/wanfang_jour_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2269040528&rft_id=info:pmid/&rft_wanfj_id=dqkx_e201904010&rfr_iscdi=true |