Late Quaternary Seismic Stratigraphy of the Eastern Bengal Shelf
An ultra-high-resolution seismic study of the eastern Bengal Shelf with the parametric narrow-beam echosounder Parasound allows the interpretation of late Quaternary depositional patterns in terms of seismic stratigraphy. Accommodation space was still present on the outer shelf during the last lowst...
Gespeichert in:
| Veröffentlicht in: | Marine geophysical researches 1998-02, Vol.20 (1), p.57-71 |
|---|---|
| Hauptverfasser: | , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 71 |
|---|---|
| container_issue | 1 |
| container_start_page | 57 |
| container_title | Marine geophysical researches |
| container_volume | 20 |
| creator | Hübscher, C Breitzke, M Michels, K Kudrass, H R Spiess, V Wiedicke, M |
| description | An ultra-high-resolution seismic study of the eastern Bengal Shelf with the parametric narrow-beam echosounder Parasound allows the interpretation of late Quaternary depositional patterns in terms of seismic stratigraphy. Accommodation space was still present on the outer shelf during the last lowstand, where a prograding delta developed in the western survey area. Oolitic beach ridges were later formed on top of this lowstand delta. Farther east, large parts of the shelf were exposed to subaerial erosion and a river system extended seaward across the area. A subaqueous highstand delta prograded southwards following the maximum transgression about 7,000 years ago. Its foreset beds exhibit acoustic voids very likely generated by sediment liquefaction, possibly caused by episodic energetic events such as major cyclones and/or earthquakes. Bottomset sediments extend seaward close to the shelf break in the west, whereas no Holocene sediments cover the outer shelf in the east.[PUBLICATION ABSTRACT] |
| doi_str_mv | 10.1023/A:1004375908399 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_miscellaneous_17166751</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2143052161</sourcerecordid><originalsourceid>FETCH-LOGICAL-a234t-a26d4a35bb20cd927055e26baf9412a032196ecc72687e1cf8a92c07435e45f93</originalsourceid><addsrcrecordid>eNpdjz1PwzAQhi0EEqEws1oMbIGzHccxE6UqH1IkhAJzdHEvTaq0KXEy9N_XCCaG9zmd7tFJL2PXAu4ESHU_fxAAiTLaQqasPWGR0EbFoDNxyiIAqWMllT5nF95vIOyZhYg95jgS_5gChx0OB15Q67et48U44NiuB9w3B97XfGyIL9H_aPyJdmvseNFQV1-ysxo7T1d_c8a-npefi9c4f395W8zzGKVKxsB0laDSVSXBraw0oDXJtMLaJkIiKClsSs4ZmWaGhKsztNKBSZSmRNdWzdjt79_90H9P5Mdy23pHXYc76idfCiPS1GgRxJt_4qafQrfOl-FsZYhWRwRzVy8</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>751925195</pqid></control><display><type>article</type><title>Late Quaternary Seismic Stratigraphy of the Eastern Bengal Shelf</title><source>SpringerLink Journals</source><creator>Hübscher, C ; Breitzke, M ; Michels, K ; Kudrass, H R ; Spiess, V ; Wiedicke, M</creator><creatorcontrib>Hübscher, C ; Breitzke, M ; Michels, K ; Kudrass, H R ; Spiess, V ; Wiedicke, M</creatorcontrib><description>An ultra-high-resolution seismic study of the eastern Bengal Shelf with the parametric narrow-beam echosounder Parasound allows the interpretation of late Quaternary depositional patterns in terms of seismic stratigraphy. Accommodation space was still present on the outer shelf during the last lowstand, where a prograding delta developed in the western survey area. Oolitic beach ridges were later formed on top of this lowstand delta. Farther east, large parts of the shelf were exposed to subaerial erosion and a river system extended seaward across the area. A subaqueous highstand delta prograded southwards following the maximum transgression about 7,000 years ago. Its foreset beds exhibit acoustic voids very likely generated by sediment liquefaction, possibly caused by episodic energetic events such as major cyclones and/or earthquakes. Bottomset sediments extend seaward close to the shelf break in the west, whereas no Holocene sediments cover the outer shelf in the east.[PUBLICATION ABSTRACT]</description><identifier>ISSN: 0025-3235</identifier><identifier>EISSN: 1573-0581</identifier><identifier>DOI: 10.1023/A:1004375908399</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Beach ridges ; Earthquakes ; Echosounders ; Geology ; Holocene ; Liquefaction ; Marine ; Quaternary ; Sediments ; Seismic activity ; Seismology ; Stratigraphy</subject><ispartof>Marine geophysical researches, 1998-02, Vol.20 (1), p.57-71</ispartof><rights>Kluwer Academic Publishers 1998</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Hübscher, C</creatorcontrib><creatorcontrib>Breitzke, M</creatorcontrib><creatorcontrib>Michels, K</creatorcontrib><creatorcontrib>Kudrass, H R</creatorcontrib><creatorcontrib>Spiess, V</creatorcontrib><creatorcontrib>Wiedicke, M</creatorcontrib><title>Late Quaternary Seismic Stratigraphy of the Eastern Bengal Shelf</title><title>Marine geophysical researches</title><description>An ultra-high-resolution seismic study of the eastern Bengal Shelf with the parametric narrow-beam echosounder Parasound allows the interpretation of late Quaternary depositional patterns in terms of seismic stratigraphy. Accommodation space was still present on the outer shelf during the last lowstand, where a prograding delta developed in the western survey area. Oolitic beach ridges were later formed on top of this lowstand delta. Farther east, large parts of the shelf were exposed to subaerial erosion and a river system extended seaward across the area. A subaqueous highstand delta prograded southwards following the maximum transgression about 7,000 years ago. Its foreset beds exhibit acoustic voids very likely generated by sediment liquefaction, possibly caused by episodic energetic events such as major cyclones and/or earthquakes. Bottomset sediments extend seaward close to the shelf break in the west, whereas no Holocene sediments cover the outer shelf in the east.[PUBLICATION ABSTRACT]</description><subject>Beach ridges</subject><subject>Earthquakes</subject><subject>Echosounders</subject><subject>Geology</subject><subject>Holocene</subject><subject>Liquefaction</subject><subject>Marine</subject><subject>Quaternary</subject><subject>Sediments</subject><subject>Seismic activity</subject><subject>Seismology</subject><subject>Stratigraphy</subject><issn>0025-3235</issn><issn>1573-0581</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNpdjz1PwzAQhi0EEqEws1oMbIGzHccxE6UqH1IkhAJzdHEvTaq0KXEy9N_XCCaG9zmd7tFJL2PXAu4ESHU_fxAAiTLaQqasPWGR0EbFoDNxyiIAqWMllT5nF95vIOyZhYg95jgS_5gChx0OB15Q67et48U44NiuB9w3B97XfGyIL9H_aPyJdmvseNFQV1-ysxo7T1d_c8a-npefi9c4f395W8zzGKVKxsB0laDSVSXBraw0oDXJtMLaJkIiKClsSs4ZmWaGhKsztNKBSZSmRNdWzdjt79_90H9P5Mdy23pHXYc76idfCiPS1GgRxJt_4qafQrfOl-FsZYhWRwRzVy8</recordid><startdate>19980201</startdate><enddate>19980201</enddate><creator>Hübscher, C</creator><creator>Breitzke, M</creator><creator>Michels, K</creator><creator>Kudrass, H R</creator><creator>Spiess, V</creator><creator>Wiedicke, M</creator><general>Springer Nature B.V</general><scope>3V.</scope><scope>7TG</scope><scope>7TN</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>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>19980201</creationdate><title>Late Quaternary Seismic Stratigraphy of the Eastern Bengal Shelf</title><author>Hübscher, C ; Breitzke, M ; Michels, K ; Kudrass, H R ; Spiess, V ; Wiedicke, M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a234t-a26d4a35bb20cd927055e26baf9412a032196ecc72687e1cf8a92c07435e45f93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>Beach ridges</topic><topic>Earthquakes</topic><topic>Echosounders</topic><topic>Geology</topic><topic>Holocene</topic><topic>Liquefaction</topic><topic>Marine</topic><topic>Quaternary</topic><topic>Sediments</topic><topic>Seismic activity</topic><topic>Seismology</topic><topic>Stratigraphy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hübscher, C</creatorcontrib><creatorcontrib>Breitzke, M</creatorcontrib><creatorcontrib>Michels, K</creatorcontrib><creatorcontrib>Kudrass, H R</creatorcontrib><creatorcontrib>Spiess, V</creatorcontrib><creatorcontrib>Wiedicke, M</creatorcontrib><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic 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>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>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</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>Marine geophysical researches</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hübscher, C</au><au>Breitzke, M</au><au>Michels, K</au><au>Kudrass, H R</au><au>Spiess, V</au><au>Wiedicke, M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Quaternary Seismic Stratigraphy of the Eastern Bengal Shelf</atitle><jtitle>Marine geophysical researches</jtitle><date>1998-02-01</date><risdate>1998</risdate><volume>20</volume><issue>1</issue><spage>57</spage><epage>71</epage><pages>57-71</pages><issn>0025-3235</issn><eissn>1573-0581</eissn><abstract>An ultra-high-resolution seismic study of the eastern Bengal Shelf with the parametric narrow-beam echosounder Parasound allows the interpretation of late Quaternary depositional patterns in terms of seismic stratigraphy. Accommodation space was still present on the outer shelf during the last lowstand, where a prograding delta developed in the western survey area. Oolitic beach ridges were later formed on top of this lowstand delta. Farther east, large parts of the shelf were exposed to subaerial erosion and a river system extended seaward across the area. A subaqueous highstand delta prograded southwards following the maximum transgression about 7,000 years ago. Its foreset beds exhibit acoustic voids very likely generated by sediment liquefaction, possibly caused by episodic energetic events such as major cyclones and/or earthquakes. Bottomset sediments extend seaward close to the shelf break in the west, whereas no Holocene sediments cover the outer shelf in the east.[PUBLICATION ABSTRACT]</abstract><cop>Dordrecht</cop><pub>Springer Nature B.V</pub><doi>10.1023/A:1004375908399</doi><tpages>15</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0025-3235 |
| ispartof | Marine geophysical researches, 1998-02, Vol.20 (1), p.57-71 |
| issn | 0025-3235 1573-0581 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_17166751 |
| source | SpringerLink Journals |
| subjects | Beach ridges Earthquakes Echosounders Geology Holocene Liquefaction Marine Quaternary Sediments Seismic activity Seismology Stratigraphy |
| title | Late Quaternary Seismic Stratigraphy of the Eastern Bengal Shelf |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-30T08%3A35%3A53IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Late%20Quaternary%20Seismic%20Stratigraphy%20of%20the%20Eastern%20Bengal%20Shelf&rft.jtitle=Marine%20geophysical%20researches&rft.au=H%C3%BCbscher,%20C&rft.date=1998-02-01&rft.volume=20&rft.issue=1&rft.spage=57&rft.epage=71&rft.pages=57-71&rft.issn=0025-3235&rft.eissn=1573-0581&rft_id=info:doi/10.1023/A:1004375908399&rft_dat=%3Cproquest%3E2143052161%3C/proquest%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=751925195&rft_id=info:pmid/&rfr_iscdi=true |