Seismic responses and forming conditions of the Oligocene shelf-edge delta and deepwater fan system in Changchang-Heshan sag,northern South China Sea

Seismic responses and forming conditions of the Oligocene shelf-edge delta and deepwater fan system in Changchang-Heshan sag,northern South China Sea

Changchang-Heshan sag is a deepwater sedimentary basin and located on the continental slope in the northern South China Sea.It is an important strategic exploration block after oil and gas explo-ration breakthrough in Baiyun and Liwan sags in adjacent deep-water regions.Guided by the theory of class...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Gu di li xue bao 2016-01, Vol.18 (3)
Hauptverfasser: Zhu, Xiaomin, Ge, Jiawang, Song, Shuang, Wang, Ruiliang, Yuan, Lizhong, Liu, Jun
Format: Artikel
Sprache:chi
Schlagworte:
Marine
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue 3
container_start_page
container_title Gu di li xue bao
container_volume 18
creator Zhu, Xiaomin
Ge, Jiawang
Song, Shuang
Wang, Ruiliang
Yuan, Lizhong
Liu, Jun
description Changchang-Heshan sag is a deepwater sedimentary basin and located on the continental slope in the northern South China Sea.It is an important strategic exploration block after oil and gas explo-ration breakthrough in Baiyun and Liwan sags in adjacent deep-water regions.Guided by the theory of classic sequence stratigraphy and based on the characteristics of the seismic reflection and stratigraphic cycles,the Oligocene Zhuhai Formation could be divided into six third-order sequences(namely ZHSQ1,ZHSQ2,ZHSQ3,ZHSQ4,ZHSQ5 and ZHSQ6 from bottom to top).Six types of seismic facies,including high continuity,weak-medium amplitude sheet seismic facies of shelf,S-shaped and oblique progradational seismic facies of shelf-edge,variable amplitude,medium continuity,mound-shaped bidirectional overlap seismic facies of continental slope and so on,are identified within the Zhuhai Formation.Sshaped and oblique progradational seismic facies represents shelf-edge delta,while mound-shaped bidirectional overlap seismic facies rep
format Article
fullrecord <record><control><sourceid>proquest</sourceid><recordid>TN_cdi_proquest_miscellaneous_1808732063</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1808732063</sourcerecordid><originalsourceid>FETCH-proquest_miscellaneous_18087320633</originalsourceid><addsrcrecordid>eNqVjD1Ow0AQhbcIUiLIHaakiKW1LcehjkDpKEwfDd7ZH2k9a3bWQhyE--IgLkDzXvF9723Urj72dVV3utuqvUh417ppuv5J6536HijIFEbIJHNiIQFkAzblKbCDMbEJJawAkoXiCV5jcGkkJhBP0VZkHIGhWPB3aIjmTyyUwSKDfEmhCQLD2SO78RbVhcTfGLoDp7x-ZoYhLcWvUmCEgfBB3VmMQvu_vlePL89v50s15_SxkJTrFGSkGJEpLXKtT_rUt40-tu0_1B-asFyT</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1808732063</pqid></control><display><type>article</type><title>Seismic responses and forming conditions of the Oligocene shelf-edge delta and deepwater fan system in Changchang-Heshan sag,northern South China Sea</title><source>Alma/SFX Local Collection</source><creator>Zhu, Xiaomin ; Ge, Jiawang ; Song, Shuang ; Wang, Ruiliang ; Yuan, Lizhong ; Liu, Jun</creator><creatorcontrib>Zhu, Xiaomin ; Ge, Jiawang ; Song, Shuang ; Wang, Ruiliang ; Yuan, Lizhong ; Liu, Jun</creatorcontrib><description>Changchang-Heshan sag is a deepwater sedimentary basin and located on the continental slope in the northern South China Sea.It is an important strategic exploration block after oil and gas explo-ration breakthrough in Baiyun and Liwan sags in adjacent deep-water regions.Guided by the theory of classic sequence stratigraphy and based on the characteristics of the seismic reflection and stratigraphic cycles,the Oligocene Zhuhai Formation could be divided into six third-order sequences(namely ZHSQ1,ZHSQ2,ZHSQ3,ZHSQ4,ZHSQ5 and ZHSQ6 from bottom to top).Six types of seismic facies,including high continuity,weak-medium amplitude sheet seismic facies of shelf,S-shaped and oblique progradational seismic facies of shelf-edge,variable amplitude,medium continuity,mound-shaped bidirectional overlap seismic facies of continental slope and so on,are identified within the Zhuhai Formation.Sshaped and oblique progradational seismic facies represents shelf-edge delta,while mound-shaped bidirectional overlap seismic facies rep</description><identifier>ISSN: 1671-1505</identifier><language>chi</language><subject>Marine</subject><ispartof>Gu di li xue bao, 2016-01, Vol.18 (3)</ispartof><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>314,780,784</link.rule.ids></links><search><creatorcontrib>Zhu, Xiaomin</creatorcontrib><creatorcontrib>Ge, Jiawang</creatorcontrib><creatorcontrib>Song, Shuang</creatorcontrib><creatorcontrib>Wang, Ruiliang</creatorcontrib><creatorcontrib>Yuan, Lizhong</creatorcontrib><creatorcontrib>Liu, Jun</creatorcontrib><title>Seismic responses and forming conditions of the Oligocene shelf-edge delta and deepwater fan system in Changchang-Heshan sag,northern South China Sea</title><title>Gu di li xue bao</title><description>Changchang-Heshan sag is a deepwater sedimentary basin and located on the continental slope in the northern South China Sea.It is an important strategic exploration block after oil and gas explo-ration breakthrough in Baiyun and Liwan sags in adjacent deep-water regions.Guided by the theory of classic sequence stratigraphy and based on the characteristics of the seismic reflection and stratigraphic cycles,the Oligocene Zhuhai Formation could be divided into six third-order sequences(namely ZHSQ1,ZHSQ2,ZHSQ3,ZHSQ4,ZHSQ5 and ZHSQ6 from bottom to top).Six types of seismic facies,including high continuity,weak-medium amplitude sheet seismic facies of shelf,S-shaped and oblique progradational seismic facies of shelf-edge,variable amplitude,medium continuity,mound-shaped bidirectional overlap seismic facies of continental slope and so on,are identified within the Zhuhai Formation.Sshaped and oblique progradational seismic facies represents shelf-edge delta,while mound-shaped bidirectional overlap seismic facies rep</description><subject>Marine</subject><issn>1671-1505</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqVjD1Ow0AQhbcIUiLIHaakiKW1LcehjkDpKEwfDd7ZH2k9a3bWQhyE--IgLkDzXvF9723Urj72dVV3utuqvUh417ppuv5J6536HijIFEbIJHNiIQFkAzblKbCDMbEJJawAkoXiCV5jcGkkJhBP0VZkHIGhWPB3aIjmTyyUwSKDfEmhCQLD2SO78RbVhcTfGLoDp7x-ZoYhLcWvUmCEgfBB3VmMQvu_vlePL89v50s15_SxkJTrFGSkGJEpLXKtT_rUt40-tu0_1B-asFyT</recordid><startdate>20160101</startdate><enddate>20160101</enddate><creator>Zhu, Xiaomin</creator><creator>Ge, Jiawang</creator><creator>Song, Shuang</creator><creator>Wang, Ruiliang</creator><creator>Yuan, Lizhong</creator><creator>Liu, Jun</creator><scope>7SN</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20160101</creationdate><title>Seismic responses and forming conditions of the Oligocene shelf-edge delta and deepwater fan system in Changchang-Heshan sag,northern South China Sea</title><author>Zhu, Xiaomin ; Ge, Jiawang ; Song, Shuang ; Wang, Ruiliang ; Yuan, Lizhong ; Liu, Jun</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-proquest_miscellaneous_18087320633</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi</language><creationdate>2016</creationdate><topic>Marine</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhu, Xiaomin</creatorcontrib><creatorcontrib>Ge, Jiawang</creatorcontrib><creatorcontrib>Song, Shuang</creatorcontrib><creatorcontrib>Wang, Ruiliang</creatorcontrib><creatorcontrib>Yuan, Lizhong</creatorcontrib><creatorcontrib>Liu, Jun</creatorcontrib><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Gu di li xue bao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhu, Xiaomin</au><au>Ge, Jiawang</au><au>Song, Shuang</au><au>Wang, Ruiliang</au><au>Yuan, Lizhong</au><au>Liu, Jun</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seismic responses and forming conditions of the Oligocene shelf-edge delta and deepwater fan system in Changchang-Heshan sag,northern South China Sea</atitle><jtitle>Gu di li xue bao</jtitle><date>2016-01-01</date><risdate>2016</risdate><volume>18</volume><issue>3</issue><issn>1671-1505</issn><abstract>Changchang-Heshan sag is a deepwater sedimentary basin and located on the continental slope in the northern South China Sea.It is an important strategic exploration block after oil and gas explo-ration breakthrough in Baiyun and Liwan sags in adjacent deep-water regions.Guided by the theory of classic sequence stratigraphy and based on the characteristics of the seismic reflection and stratigraphic cycles,the Oligocene Zhuhai Formation could be divided into six third-order sequences(namely ZHSQ1,ZHSQ2,ZHSQ3,ZHSQ4,ZHSQ5 and ZHSQ6 from bottom to top).Six types of seismic facies,including high continuity,weak-medium amplitude sheet seismic facies of shelf,S-shaped and oblique progradational seismic facies of shelf-edge,variable amplitude,medium continuity,mound-shaped bidirectional overlap seismic facies of continental slope and so on,are identified within the Zhuhai Formation.Sshaped and oblique progradational seismic facies represents shelf-edge delta,while mound-shaped bidirectional overlap seismic facies rep</abstract></addata></record>
fulltext fulltext
identifier ISSN: 1671-1505
ispartof Gu di li xue bao, 2016-01, Vol.18 (3)
issn 1671-1505
language chi
recordid cdi_proquest_miscellaneous_1808732063
source Alma/SFX Local Collection
subjects Marine
title Seismic responses and forming conditions of the Oligocene shelf-edge delta and deepwater fan system in Changchang-Heshan sag,northern 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=2024-12-26T00%3A29%3A32IST&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=Seismic%20responses%20and%20forming%20conditions%20of%20the%20Oligocene%20shelf-edge%20delta%20and%20deepwater%20fan%20system%20in%20Changchang-Heshan%20sag,northern%20South%20China%20Sea&rft.jtitle=Gu%20di%20li%20xue%20bao&rft.au=Zhu,%20Xiaomin&rft.date=2016-01-01&rft.volume=18&rft.issue=3&rft.issn=1671-1505&rft_id=info:doi/&rft_dat=%3Cproquest%3E1808732063%3C/proquest%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1808732063&rft_id=info:pmid/&rfr_iscdi=true