Late Cenozoic Geology and Paleo-environment Change in the Eastern Edge of Qinghai-Xizang Plateau
P5; There are late Cenozoic lacustrine deposits and loess and red clay and moraines in eastern edge of the Qinghai-Xizang Plateau. Various genetic sediments recorded rich information on late Cenozoic paleo-environment changes. Xigeda lacustrine formed during 4.2 Ma B.P.-2.6 Ma B.P. There were 9 peri...
Gespeichert in:
| Veröffentlicht in: | 地质学报（英文版） 2008, Vol.82 (5), p.959-966 |
|---|---|
| Hauptverfasser: | , , , , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 966 |
|---|---|
| container_issue | 5 |
| container_start_page | 959 |
| container_title | 地质学报（英文版） |
| container_volume | 82 |
| creator | ZHAO Zhizhong QIAO Yansong WANG Shubing YAO Haitao WANG Yan LI Chaozhu FU Jianli LIU Zongxiu LI Mingze MIAO Qi JIANG Fuchu |
| description | P5; There are late Cenozoic lacustrine deposits and loess and red clay and moraines in eastern edge of the Qinghai-Xizang Plateau. Various genetic sediments recorded rich information on late Cenozoic paleo-environment changes. Xigeda lacustrine formed during 4.2 Ma B.P.-2.6 Ma B.P. There were 9 periodic warm-cold alternations. Eolian deposition in western Sichuan began at 1.15 Ma B.P. The loess-soil sequences recorded successively 14 paleo-monsoon climate cycles. Laterite in Chengdu plain recorded 5 stages of paleoclimatic stages since 1.13 Ma B.P. There was an old glacial period of 4.3 Ma B.P. In eastern Qinghai-Xizang Plateau. During Quaternary, there are 5 extreme paleoclimatic events corresponding with 5 glaciations. |
| doi_str_mv | 10.3321/j.issn:1000-9515.2008.05.004 |
| format | Article |
| fullrecord | <record><control><sourceid>wanfang_jour</sourceid><recordid>TN_cdi_wanfang_journals_dzxb_e200805004</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><wanfj_id>dzxb_e200805004</wanfj_id><sourcerecordid>dzxb_e200805004</sourcerecordid><originalsourceid>FETCH-wanfang_journals_dzxb_e2008050043</originalsourceid><addsrcrecordid>eNqNjj1Pw0AQRK9IJELCf9gCicrHXsxFQGsZKCgSKUU6Z4PX9lnOnuRz-PCv5yJF1FQjvXkajVK3BnWaLs19q10I8mwQMXmyxuol4qNGqxEfJmr2x6_UdQgt4squjJ2p_TsNDBmLH737gFf2na9_gKSENXXsE5ZP13s5sgyQNSQ1gxMYGoacwsC9QF5G5ivYOKkbcsnOjVGDdReX6bRQ04q6wDeXnKu7l3ybvSVfJFX0itafeolNUY7fh4LPt9HG0-n_zV8SNE7X</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Late Cenozoic Geology and Paleo-environment Change in the Eastern Edge of Qinghai-Xizang Plateau</title><source>Wiley Online Library All Journals</source><source>Alma/SFX Local Collection</source><creator>ZHAO Zhizhong ; QIAO Yansong ; WANG Shubing ; YAO Haitao ; WANG Yan ; LI Chaozhu ; FU Jianli ; LIU Zongxiu ; LI Mingze ; MIAO Qi ; JIANG Fuchu</creator><creatorcontrib>ZHAO Zhizhong ; QIAO Yansong ; WANG Shubing ; YAO Haitao ; WANG Yan ; LI Chaozhu ; FU Jianli ; LIU Zongxiu ; LI Mingze ; MIAO Qi ; JIANG Fuchu</creatorcontrib><description>P5; There are late Cenozoic lacustrine deposits and loess and red clay and moraines in eastern edge of the Qinghai-Xizang Plateau. Various genetic sediments recorded rich information on late Cenozoic paleo-environment changes. Xigeda lacustrine formed during 4.2 Ma B.P.-2.6 Ma B.P. There were 9 periodic warm-cold alternations. Eolian deposition in western Sichuan began at 1.15 Ma B.P. The loess-soil sequences recorded successively 14 paleo-monsoon climate cycles. Laterite in Chengdu plain recorded 5 stages of paleoclimatic stages since 1.13 Ma B.P. There was an old glacial period of 4.3 Ma B.P. In eastern Qinghai-Xizang Plateau. During Quaternary, there are 5 extreme paleoclimatic events corresponding with 5 glaciations.</description><identifier>ISSN: 1000-9515</identifier><identifier>DOI: 10.3321/j.issn:1000-9515.2008.05.004</identifier><language>eng</language><publisher>Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China%Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China</publisher><ispartof>地质学报（英文版）, 2008, Vol.82 (5), p.959-966</ispartof><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/dzxb-e/dzxb-e.jpg</thumbnail><link.rule.ids>314,780,784,4024,27923,27924,27925</link.rule.ids></links><search><creatorcontrib>ZHAO Zhizhong</creatorcontrib><creatorcontrib>QIAO Yansong</creatorcontrib><creatorcontrib>WANG Shubing</creatorcontrib><creatorcontrib>YAO Haitao</creatorcontrib><creatorcontrib>WANG Yan</creatorcontrib><creatorcontrib>LI Chaozhu</creatorcontrib><creatorcontrib>FU Jianli</creatorcontrib><creatorcontrib>LIU Zongxiu</creatorcontrib><creatorcontrib>LI Mingze</creatorcontrib><creatorcontrib>MIAO Qi</creatorcontrib><creatorcontrib>JIANG Fuchu</creatorcontrib><title>Late Cenozoic Geology and Paleo-environment Change in the Eastern Edge of Qinghai-Xizang Plateau</title><title>地质学报（英文版）</title><description>P5; There are late Cenozoic lacustrine deposits and loess and red clay and moraines in eastern edge of the Qinghai-Xizang Plateau. Various genetic sediments recorded rich information on late Cenozoic paleo-environment changes. Xigeda lacustrine formed during 4.2 Ma B.P.-2.6 Ma B.P. There were 9 periodic warm-cold alternations. Eolian deposition in western Sichuan began at 1.15 Ma B.P. The loess-soil sequences recorded successively 14 paleo-monsoon climate cycles. Laterite in Chengdu plain recorded 5 stages of paleoclimatic stages since 1.13 Ma B.P. There was an old glacial period of 4.3 Ma B.P. In eastern Qinghai-Xizang Plateau. During Quaternary, there are 5 extreme paleoclimatic events corresponding with 5 glaciations.</description><issn>1000-9515</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNqNjj1Pw0AQRK9IJELCf9gCicrHXsxFQGsZKCgSKUU6Z4PX9lnOnuRz-PCv5yJF1FQjvXkajVK3BnWaLs19q10I8mwQMXmyxuol4qNGqxEfJmr2x6_UdQgt4squjJ2p_TsNDBmLH737gFf2na9_gKSENXXsE5ZP13s5sgyQNSQ1gxMYGoacwsC9QF5G5ivYOKkbcsnOjVGDdReX6bRQ04q6wDeXnKu7l3ybvSVfJFX0itafeolNUY7fh4LPt9HG0-n_zV8SNE7X</recordid><startdate>2008</startdate><enddate>2008</enddate><creator>ZHAO Zhizhong</creator><creator>QIAO Yansong</creator><creator>WANG Shubing</creator><creator>YAO Haitao</creator><creator>WANG Yan</creator><creator>LI Chaozhu</creator><creator>FU Jianli</creator><creator>LIU Zongxiu</creator><creator>LI Mingze</creator><creator>MIAO Qi</creator><creator>JIANG Fuchu</creator><general>Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China%Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China</general><general>Open Laboratory of Lake Sediment and Environment, Chinese Academy of Sciences, Nanjing 210008,Jiangsu, China</general><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>2008</creationdate><title>Late Cenozoic Geology and Paleo-environment Change in the Eastern Edge of Qinghai-Xizang Plateau</title><author>ZHAO Zhizhong ; QIAO Yansong ; WANG Shubing ; YAO Haitao ; WANG Yan ; LI Chaozhu ; FU Jianli ; LIU Zongxiu ; LI Mingze ; MIAO Qi ; JIANG Fuchu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-wanfang_journals_dzxb_e2008050043</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>ZHAO Zhizhong</creatorcontrib><creatorcontrib>QIAO Yansong</creatorcontrib><creatorcontrib>WANG Shubing</creatorcontrib><creatorcontrib>YAO Haitao</creatorcontrib><creatorcontrib>WANG Yan</creatorcontrib><creatorcontrib>LI Chaozhu</creatorcontrib><creatorcontrib>FU Jianli</creatorcontrib><creatorcontrib>LIU Zongxiu</creatorcontrib><creatorcontrib>LI Mingze</creatorcontrib><creatorcontrib>MIAO Qi</creatorcontrib><creatorcontrib>JIANG Fuchu</creatorcontrib><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>地质学报（英文版）</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>ZHAO Zhizhong</au><au>QIAO Yansong</au><au>WANG Shubing</au><au>YAO Haitao</au><au>WANG Yan</au><au>LI Chaozhu</au><au>FU Jianli</au><au>LIU Zongxiu</au><au>LI Mingze</au><au>MIAO Qi</au><au>JIANG Fuchu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Cenozoic Geology and Paleo-environment Change in the Eastern Edge of Qinghai-Xizang Plateau</atitle><jtitle>地质学报（英文版）</jtitle><date>2008</date><risdate>2008</risdate><volume>82</volume><issue>5</issue><spage>959</spage><epage>966</epage><pages>959-966</pages><issn>1000-9515</issn><abstract>P5; There are late Cenozoic lacustrine deposits and loess and red clay and moraines in eastern edge of the Qinghai-Xizang Plateau. Various genetic sediments recorded rich information on late Cenozoic paleo-environment changes. Xigeda lacustrine formed during 4.2 Ma B.P.-2.6 Ma B.P. There were 9 periodic warm-cold alternations. Eolian deposition in western Sichuan began at 1.15 Ma B.P. The loess-soil sequences recorded successively 14 paleo-monsoon climate cycles. Laterite in Chengdu plain recorded 5 stages of paleoclimatic stages since 1.13 Ma B.P. There was an old glacial period of 4.3 Ma B.P. In eastern Qinghai-Xizang Plateau. During Quaternary, there are 5 extreme paleoclimatic events corresponding with 5 glaciations.</abstract><pub>Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China%Institute of Geomechanics, Chinese Academy of Geosciences, Beijing 100081, China</pub><doi>10.3321/j.issn:1000-9515.2008.05.004</doi></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1000-9515 |
| ispartof | 地质学报（英文版）, 2008, Vol.82 (5), p.959-966 |
| issn | 1000-9515 |
| language | eng |
| recordid | cdi_wanfang_journals_dzxb_e200805004 |
| source | Wiley Online Library All Journals; Alma/SFX Local Collection |
| title | Late Cenozoic Geology and Paleo-environment Change in the Eastern Edge of Qinghai-Xizang Plateau |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T03%3A19%3A11IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Late%20Cenozoic%20Geology%20and%20Paleo-environment%20Change%20in%20the%20Eastern%20Edge%20of%20Qinghai-Xizang%20Plateau&rft.jtitle=%E5%9C%B0%E8%B4%A8%E5%AD%A6%E6%8A%A5%EF%BC%88%E8%8B%B1%E6%96%87%E7%89%88%EF%BC%89&rft.au=ZHAO%20Zhizhong&rft.date=2008&rft.volume=82&rft.issue=5&rft.spage=959&rft.epage=966&rft.pages=959-966&rft.issn=1000-9515&rft_id=info:doi/10.3321/j.issn:1000-9515.2008.05.004&rft_dat=%3Cwanfang_jour%3Edzxb_e200805004%3C/wanfang_jour%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_wanfj_id=dzxb_e200805004&rfr_iscdi=true |