Seismic sequence and depositional evolution of slope basins in mid-northern margin of the South China Sea
As one of the biggest marginal seas in the western Pacific margin, the South China Sea （SCS） experienced continental rifting and seafloor spreading during the Cenozoic. The northern continental margin of the SCS is classified as a passive continental margin. However, its depositional and structural...
Gespeichert in:
| Veröffentlicht in: | Chinese journal of oceanology and limnology 2011-09, Vol.29 (5), p.1113-1127 |
|---|---|
| 1. Verfasser: | |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1127 |
|---|---|
| container_issue | 5 |
| container_start_page | 1113 |
| container_title | Chinese journal of oceanology and limnology |
| container_volume | 29 |
| creator | 黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇 |
| description | As one of the biggest marginal seas in the western Pacific margin, the South China Sea （SCS） experienced continental rifting and seafloor spreading during the Cenozoic. The northern continental margin of the SCS is classified as a passive continental margin. However, its depositional and structural evolution remains controversial, especially in the deep slope area. The lack of data hindered the correlation between continental shelf and oceanic basin, and prevented the establishment of sequence stratigraphic frame of the whole margin. The slope basins in the mid-northern margin of SCS developed in the Cenozoic; the sediments and basin infill recorded the geological history of the continental margin and the SCS spreading. Using multi-channel seismic dataset acquired in three survey cruises during 1987 to 2004, combined with the data of ODP Leg 184 core and industrial wells, we carried out the sequence stratigraphic division and correlation of the Cenozoic in the middle-northern margin of SCS with seismic profiles and sedimentary facies. We interpreted the seismic reflection properties including continuity, amplitude, fi＇equency, reflection terminals, and 15 sequence boundaries of the Cenozoic in the study area, and correlated the well data in geological age. The depositional environment changed from river and lake, shallow bay to open-deep sea, in correspondence to tectonic events of syn-rifting, early drifting, and late drifting stages of basin evolution. |
| doi_str_mv | 10.1007/s00343-011-0208-2 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_881458347</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>38981792</cqvip_id><sourcerecordid>907174213</sourcerecordid><originalsourceid>FETCH-LOGICAL-c373t-116f71589a8e04382f461db26cb659efd6347714c00a443eeb641317cb4048c63</originalsourceid><addsrcrecordid>eNp9kM2LFDEQxYO44Li7f4C36MVTtPLRneQog1-w4GHcc0inq2ey9CSzSbfgf2_GWRQ8eKoq-L16vEfIKw7vOIB-XwGkkgw4ZyDAMPGMbLi1knUA3XOyAdEppqCzL8jLWh8abRXYDYk7jPUYA634uGIKSH0a6YinXOMSc_IzxR95Xs87zROtcz4hHXyNqdKY6DGOLOWyHLC0w5d9_I21m-7yuhzo9hCTpzv0N-Rq8nPF26d5Te4_ffy-_cLuvn3-uv1wx4LUcmGc95PmnbHeIChpxKR6Pg6iD0PfWZzGXiqtuQoAXimJOPSKS67DoECZ0Mtr8vby91Ryi1QXd4w14Dz7hHmtzoLmWgkuG_nmH_Ihr6VFrs4YrjrTnBrEL1AoudaCkzuV2IL-dBzcuXp3qd616t25eieaRlw0tbFpj-Xv4_-JXj8ZHXLaPzbdHydprOHaCvkLGDaQtQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>881458347</pqid></control><display><type>article</type><title>Seismic sequence and depositional evolution of slope basins in mid-northern margin of the South China Sea</title><source>SpringerLink Journals</source><source>Alma/SFX Local Collection</source><source>ProQuest Central</source><creator>黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇</creator><creatorcontrib>黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇</creatorcontrib><description>As one of the biggest marginal seas in the western Pacific margin, the South China Sea （SCS） experienced continental rifting and seafloor spreading during the Cenozoic. The northern continental margin of the SCS is classified as a passive continental margin. However, its depositional and structural evolution remains controversial, especially in the deep slope area. The lack of data hindered the correlation between continental shelf and oceanic basin, and prevented the establishment of sequence stratigraphic frame of the whole margin. The slope basins in the mid-northern margin of SCS developed in the Cenozoic; the sediments and basin infill recorded the geological history of the continental margin and the SCS spreading. Using multi-channel seismic dataset acquired in three survey cruises during 1987 to 2004, combined with the data of ODP Leg 184 core and industrial wells, we carried out the sequence stratigraphic division and correlation of the Cenozoic in the middle-northern margin of SCS with seismic profiles and sedimentary facies. We interpreted the seismic reflection properties including continuity, amplitude, fi＇equency, reflection terminals, and 15 sequence boundaries of the Cenozoic in the study area, and correlated the well data in geological age. The depositional environment changed from river and lake, shallow bay to open-deep sea, in correspondence to tectonic events of syn-rifting, early drifting, and late drifting stages of basin evolution.</description><identifier>ISSN: 0254-4059</identifier><identifier>ISSN: 2096-5508</identifier><identifier>EISSN: 1993-5005</identifier><identifier>EISSN: 2523-3521</identifier><identifier>DOI: 10.1007/s00343-011-0208-2</identifier><language>eng</language><publisher>Heidelberg: SP Science Press</publisher><subject>Basins ; Brackish ; Cenozoic ; Cenozoic Era ; Continental margins ; Continental shelves ; Correlation ; Cruises ; Deep sea ; Earth and Environmental Science ; Earth Sciences ; Evolution ; Geological history ; Geological time ; Geology ; Inland waters ; Lakes ; Marginal seas ; Marine ; Ocean basins ; Ocean floor ; Oceanography ; Redevelopment ; Reflection ; Rifting ; Sea floor spreading ; Seafloor spreading ; Sedimentary facies ; Sediments ; Seismic analysis ; Seismic profiles ; Seismic surveys ; Seismology ; Sequencing ; Stratigraphy ; Tectonics ; Well data ; 中国南海 ; 保证金 ; 南海北部 ; 地震序列 ; 大洋盆地 ; 大陆裂谷 ; 层序地层划分 ; 沉积演化</subject><ispartof>Chinese journal of oceanology and limnology, 2011-09, Vol.29 (5), p.1113-1127</ispartof><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2011</rights><rights>Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag Berlin Heidelberg 2011.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c373t-116f71589a8e04382f461db26cb659efd6347714c00a443eeb641317cb4048c63</citedby><cites>FETCH-LOGICAL-c373t-116f71589a8e04382f461db26cb659efd6347714c00a443eeb641317cb4048c63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/84119X/84119X.jpg</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/881458347/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/881458347?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,776,780,21367,27901,27902,33721,43781,74045</link.rule.ids></links><search><creatorcontrib>黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇</creatorcontrib><title>Seismic sequence and depositional evolution of slope basins in mid-northern margin of the South China Sea</title><title>Chinese journal of oceanology and limnology</title><addtitle>Chin. J. Ocean. Limnol</addtitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><description>As one of the biggest marginal seas in the western Pacific margin, the South China Sea （SCS） experienced continental rifting and seafloor spreading during the Cenozoic. The northern continental margin of the SCS is classified as a passive continental margin. However, its depositional and structural evolution remains controversial, especially in the deep slope area. The lack of data hindered the correlation between continental shelf and oceanic basin, and prevented the establishment of sequence stratigraphic frame of the whole margin. The slope basins in the mid-northern margin of SCS developed in the Cenozoic; the sediments and basin infill recorded the geological history of the continental margin and the SCS spreading. Using multi-channel seismic dataset acquired in three survey cruises during 1987 to 2004, combined with the data of ODP Leg 184 core and industrial wells, we carried out the sequence stratigraphic division and correlation of the Cenozoic in the middle-northern margin of SCS with seismic profiles and sedimentary facies. We interpreted the seismic reflection properties including continuity, amplitude, fi＇equency, reflection terminals, and 15 sequence boundaries of the Cenozoic in the study area, and correlated the well data in geological age. The depositional environment changed from river and lake, shallow bay to open-deep sea, in correspondence to tectonic events of syn-rifting, early drifting, and late drifting stages of basin evolution.</description><subject>Basins</subject><subject>Brackish</subject><subject>Cenozoic</subject><subject>Cenozoic Era</subject><subject>Continental margins</subject><subject>Continental shelves</subject><subject>Correlation</subject><subject>Cruises</subject><subject>Deep sea</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evolution</subject><subject>Geological history</subject><subject>Geological time</subject><subject>Geology</subject><subject>Inland waters</subject><subject>Lakes</subject><subject>Marginal seas</subject><subject>Marine</subject><subject>Ocean basins</subject><subject>Ocean floor</subject><subject>Oceanography</subject><subject>Redevelopment</subject><subject>Reflection</subject><subject>Rifting</subject><subject>Sea floor spreading</subject><subject>Seafloor spreading</subject><subject>Sedimentary facies</subject><subject>Sediments</subject><subject>Seismic analysis</subject><subject>Seismic profiles</subject><subject>Seismic surveys</subject><subject>Seismology</subject><subject>Sequencing</subject><subject>Stratigraphy</subject><subject>Tectonics</subject><subject>Well data</subject><subject>中国南海</subject><subject>保证金</subject><subject>南海北部</subject><subject>地震序列</subject><subject>大洋盆地</subject><subject>大陆裂谷</subject><subject>层序地层划分</subject><subject>沉积演化</subject><issn>0254-4059</issn><issn>2096-5508</issn><issn>1993-5005</issn><issn>2523-3521</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kM2LFDEQxYO44Li7f4C36MVTtPLRneQog1-w4GHcc0inq2ey9CSzSbfgf2_GWRQ8eKoq-L16vEfIKw7vOIB-XwGkkgw4ZyDAMPGMbLi1knUA3XOyAdEppqCzL8jLWh8abRXYDYk7jPUYA634uGIKSH0a6YinXOMSc_IzxR95Xs87zROtcz4hHXyNqdKY6DGOLOWyHLC0w5d9_I21m-7yuhzo9hCTpzv0N-Rq8nPF26d5Te4_ffy-_cLuvn3-uv1wx4LUcmGc95PmnbHeIChpxKR6Pg6iD0PfWZzGXiqtuQoAXimJOPSKS67DoECZ0Mtr8vby91Ryi1QXd4w14Dz7hHmtzoLmWgkuG_nmH_Ihr6VFrs4YrjrTnBrEL1AoudaCkzuV2IL-dBzcuXp3qd616t25eieaRlw0tbFpj-Xv4_-JXj8ZHXLaPzbdHydprOHaCvkLGDaQtQ</recordid><startdate>20110901</startdate><enddate>20110901</enddate><creator>黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇</creator><general>SP Science Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7QL</scope><scope>7SN</scope><scope>7TN</scope><scope>7U7</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>M7N</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20110901</creationdate><title>Seismic sequence and depositional evolution of slope basins in mid-northern margin of the South China Sea</title><author>黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c373t-116f71589a8e04382f461db26cb659efd6347714c00a443eeb641317cb4048c63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Basins</topic><topic>Brackish</topic><topic>Cenozoic</topic><topic>Cenozoic Era</topic><topic>Continental margins</topic><topic>Continental shelves</topic><topic>Correlation</topic><topic>Cruises</topic><topic>Deep sea</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Evolution</topic><topic>Geological history</topic><topic>Geological time</topic><topic>Geology</topic><topic>Inland waters</topic><topic>Lakes</topic><topic>Marginal seas</topic><topic>Marine</topic><topic>Ocean basins</topic><topic>Ocean floor</topic><topic>Oceanography</topic><topic>Redevelopment</topic><topic>Reflection</topic><topic>Rifting</topic><topic>Sea floor spreading</topic><topic>Seafloor spreading</topic><topic>Sedimentary facies</topic><topic>Sediments</topic><topic>Seismic analysis</topic><topic>Seismic profiles</topic><topic>Seismic surveys</topic><topic>Seismology</topic><topic>Sequencing</topic><topic>Stratigraphy</topic><topic>Tectonics</topic><topic>Well data</topic><topic>中国南海</topic><topic>保证金</topic><topic>南海北部</topic><topic>地震序列</topic><topic>大洋盆地</topic><topic>大陆裂谷</topic><topic>层序地层划分</topic><topic>沉积演化</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Toxicology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>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 Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</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><jtitle>Chinese journal of oceanology and limnology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>黎明碧 金翔龙 李家彪 丁巍伟 方银霞 刘建华 唐勇</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seismic sequence and depositional evolution of slope basins in mid-northern margin of the South China Sea</atitle><jtitle>Chinese journal of oceanology and limnology</jtitle><stitle>Chin. J. Ocean. Limnol</stitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><date>2011-09-01</date><risdate>2011</risdate><volume>29</volume><issue>5</issue><spage>1113</spage><epage>1127</epage><pages>1113-1127</pages><issn>0254-4059</issn><issn>2096-5508</issn><eissn>1993-5005</eissn><eissn>2523-3521</eissn><abstract>As one of the biggest marginal seas in the western Pacific margin, the South China Sea （SCS） experienced continental rifting and seafloor spreading during the Cenozoic. The northern continental margin of the SCS is classified as a passive continental margin. However, its depositional and structural evolution remains controversial, especially in the deep slope area. The lack of data hindered the correlation between continental shelf and oceanic basin, and prevented the establishment of sequence stratigraphic frame of the whole margin. The slope basins in the mid-northern margin of SCS developed in the Cenozoic; the sediments and basin infill recorded the geological history of the continental margin and the SCS spreading. Using multi-channel seismic dataset acquired in three survey cruises during 1987 to 2004, combined with the data of ODP Leg 184 core and industrial wells, we carried out the sequence stratigraphic division and correlation of the Cenozoic in the middle-northern margin of SCS with seismic profiles and sedimentary facies. We interpreted the seismic reflection properties including continuity, amplitude, fi＇equency, reflection terminals, and 15 sequence boundaries of the Cenozoic in the study area, and correlated the well data in geological age. The depositional environment changed from river and lake, shallow bay to open-deep sea, in correspondence to tectonic events of syn-rifting, early drifting, and late drifting stages of basin evolution.</abstract><cop>Heidelberg</cop><pub>SP Science Press</pub><doi>10.1007/s00343-011-0208-2</doi><tpages>15</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0254-4059 |
| ispartof | Chinese journal of oceanology and limnology, 2011-09, Vol.29 (5), p.1113-1127 |
| issn | 0254-4059 2096-5508 1993-5005 2523-3521 |
| language | eng |
| recordid | cdi_proquest_journals_881458347 |
| source | SpringerLink Journals; Alma/SFX Local Collection; ProQuest Central |
| subjects | Basins Brackish Cenozoic Cenozoic Era Continental margins Continental shelves Correlation Cruises Deep sea Earth and Environmental Science Earth Sciences Evolution Geological history Geological time Geology Inland waters Lakes Marginal seas Marine Ocean basins Ocean floor Oceanography Redevelopment Reflection Rifting Sea floor spreading Seafloor spreading Sedimentary facies Sediments Seismic analysis Seismic profiles Seismic surveys Seismology Sequencing Stratigraphy Tectonics Well data 中国南海 保证金 南海北部 地震序列 大洋盆地 大陆裂谷 层序地层划分 沉积演化 |
| title | Seismic sequence and depositional evolution of slope basins in mid-northern margin of the South China Sea |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-31T00%3A41%3A51IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Seismic%20sequence%20and%20depositional%20evolution%20of%20slope%20basins%20in%20mid-northern%20margin%20of%20the%20South%20China%20Sea&rft.jtitle=Chinese%20journal%20of%20oceanology%20and%20limnology&rft.au=%E9%BB%8E%E6%98%8E%E7%A2%A7%20%E9%87%91%E7%BF%94%E9%BE%99%20%E6%9D%8E%E5%AE%B6%E5%BD%AA%20%E4%B8%81%E5%B7%8D%E4%BC%9F%20%E6%96%B9%E9%93%B6%E9%9C%9E%20%E5%88%98%E5%BB%BA%E5%8D%8E%20%E5%94%90%E5%8B%87&rft.date=2011-09-01&rft.volume=29&rft.issue=5&rft.spage=1113&rft.epage=1127&rft.pages=1113-1127&rft.issn=0254-4059&rft.eissn=1993-5005&rft_id=info:doi/10.1007/s00343-011-0208-2&rft_dat=%3Cproquest_cross%3E907174213%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=881458347&rft_id=info:pmid/&rft_cqvip_id=38981792&rfr_iscdi=true |