An isotopic study of the S1 paleosol carbonates from the central Loess Plateau of North China
The loess-paleosol sequence in the central Loess Plateau of China is produced under arid to sub-humid climatic conditions and contains abundant carbonates. These carbonates could be partly detrital derived from provenance by aerosol and partly authigenic precipitated during weathering and pedogenesi...
Gespeichert in:
| Veröffentlicht in: | 中国科学通报：英文版 1996 (18), p.1542-1545 |
|---|---|
| 1. Verfasser: | |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1545 |
|---|---|
| container_issue | 18 |
| container_start_page | 1542 |
| container_title | 中国科学通报：英文版 |
| container_volume | |
| creator | 陈骏 安芷生 王洪涛 高燕 |
| description | The loess-paleosol sequence in the central Loess Plateau of China is produced under arid to sub-humid climatic conditions and contains abundant carbonates. These carbonates could be partly detrital derived from provenance by aerosol and partly authigenic precipitated during weathering and pedogenesis after deposition of the aerosol. Some previous studies have examined oxygen and carbon isotopic compositions of the carbonates by means of whole rock samples containing various amounts of detrital carbonates.This study separates authigenic carbonate from detrital one and only examines the former in order to investigate isotopic composition of the pedogenic carbonate and to discuss its relationships to the Asian paleomonsoon probably existing during the last interglacial time. |
| format | Article |
| fullrecord | <record><control><sourceid>chongqing</sourceid><recordid>TN_cdi_chongqing_primary_4001157409</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>4001157409</cqvip_id><sourcerecordid>4001157409</sourcerecordid><originalsourceid>FETCH-chongqing_primary_40011574093</originalsourceid><addsrcrecordid>eNqNjsEKgkAURWdRkJT_8KC1MOqIuAwpWkQEtY2YbNSJcZ7NGxf-fRZ9QKuzOOfCnbEg4UUWFUmeLlhI9OScx6JIBM8Ddt1Y0IQee10B-eExAtbgWwXnGHppFBIaqKS7o5VeEdQOu6-vlPVOGjigIoKTmawcPuMjOt9C2WorV2xeS0Mq_HHJ1rvtpdxHVYu2eWnb3HqnO-nGm5hOxVkueJH-V70BlM1CjQ</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>An isotopic study of the S1 paleosol carbonates from the central Loess Plateau of North China</title><source>Alma/SFX Local Collection</source><creator>陈骏 安芷生 王洪涛 高燕</creator><creatorcontrib>陈骏 安芷生 王洪涛 高燕</creatorcontrib><description>The loess-paleosol sequence in the central Loess Plateau of China is produced under arid to sub-humid climatic conditions and contains abundant carbonates. These carbonates could be partly detrital derived from provenance by aerosol and partly authigenic precipitated during weathering and pedogenesis after deposition of the aerosol. Some previous studies have examined oxygen and carbon isotopic compositions of the carbonates by means of whole rock samples containing various amounts of detrital carbonates.This study separates authigenic carbonate from detrital one and only examines the former in order to investigate isotopic composition of the pedogenic carbonate and to discuss its relationships to the Asian paleomonsoon probably existing during the last interglacial time.</description><identifier>ISSN: 2095-9273</identifier><language>eng</language><subject>carbonate ; isotopes ; paleoclimate ; paleomonsoon ; paleosol ; soil ; stable</subject><ispartof>中国科学通报：英文版, 1996 (18), p.1542-1545</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/86894X/86894X.jpg</thumbnail><link.rule.ids>314,776,780,4010</link.rule.ids></links><search><creatorcontrib>陈骏 安芷生 王洪涛 高燕</creatorcontrib><title>An isotopic study of the S1 paleosol carbonates from the central Loess Plateau of North China</title><title>中国科学通报：英文版</title><addtitle>Chinese Science Bulletin</addtitle><description>The loess-paleosol sequence in the central Loess Plateau of China is produced under arid to sub-humid climatic conditions and contains abundant carbonates. These carbonates could be partly detrital derived from provenance by aerosol and partly authigenic precipitated during weathering and pedogenesis after deposition of the aerosol. Some previous studies have examined oxygen and carbon isotopic compositions of the carbonates by means of whole rock samples containing various amounts of detrital carbonates.This study separates authigenic carbonate from detrital one and only examines the former in order to investigate isotopic composition of the pedogenic carbonate and to discuss its relationships to the Asian paleomonsoon probably existing during the last interglacial time.</description><subject>carbonate</subject><subject>isotopes</subject><subject>paleoclimate</subject><subject>paleomonsoon</subject><subject>paleosol</subject><subject>soil</subject><subject>stable</subject><issn>2095-9273</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1996</creationdate><recordtype>article</recordtype><recordid>eNqNjsEKgkAURWdRkJT_8KC1MOqIuAwpWkQEtY2YbNSJcZ7NGxf-fRZ9QKuzOOfCnbEg4UUWFUmeLlhI9OScx6JIBM8Ddt1Y0IQee10B-eExAtbgWwXnGHppFBIaqKS7o5VeEdQOu6-vlPVOGjigIoKTmawcPuMjOt9C2WorV2xeS0Mq_HHJ1rvtpdxHVYu2eWnb3HqnO-nGm5hOxVkueJH-V70BlM1CjQ</recordid><startdate>1996</startdate><enddate>1996</enddate><creator>陈骏 安芷生 王洪涛 高燕</creator><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope></search><sort><creationdate>1996</creationdate><title>An isotopic study of the S1 paleosol carbonates from the central Loess Plateau of North China</title><author>陈骏 安芷生 王洪涛 高燕</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-chongqing_primary_40011574093</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1996</creationdate><topic>carbonate</topic><topic>isotopes</topic><topic>paleoclimate</topic><topic>paleomonsoon</topic><topic>paleosol</topic><topic>soil</topic><topic>stable</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>陈骏 安芷生 王洪涛 高燕</creatorcontrib><collection>维普_期刊</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>维普中文期刊数据库</collection><collection>中文科技期刊数据库- 镜像站点</collection><jtitle>中国科学通报：英文版</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>陈骏 安芷生 王洪涛 高燕</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An isotopic study of the S1 paleosol carbonates from the central Loess Plateau of North China</atitle><jtitle>中国科学通报：英文版</jtitle><addtitle>Chinese Science Bulletin</addtitle><date>1996</date><risdate>1996</risdate><issue>18</issue><spage>1542</spage><epage>1545</epage><pages>1542-1545</pages><issn>2095-9273</issn><abstract>The loess-paleosol sequence in the central Loess Plateau of China is produced under arid to sub-humid climatic conditions and contains abundant carbonates. These carbonates could be partly detrital derived from provenance by aerosol and partly authigenic precipitated during weathering and pedogenesis after deposition of the aerosol. Some previous studies have examined oxygen and carbon isotopic compositions of the carbonates by means of whole rock samples containing various amounts of detrital carbonates.This study separates authigenic carbonate from detrital one and only examines the former in order to investigate isotopic composition of the pedogenic carbonate and to discuss its relationships to the Asian paleomonsoon probably existing during the last interglacial time.</abstract></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 2095-9273 |
| ispartof | 中国科学通报：英文版, 1996 (18), p.1542-1545 |
| issn | 2095-9273 |
| language | eng |
| recordid | cdi_chongqing_primary_4001157409 |
| source | Alma/SFX Local Collection |
| subjects | carbonate isotopes paleoclimate paleomonsoon paleosol soil stable |
| title | An isotopic study of the S1 paleosol carbonates from the central Loess Plateau of North China |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-11T22%3A58%3A00IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-chongqing&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=An%20isotopic%20study%20of%20the%20S1%20paleosol%20carbonates%20from%20the%20central%20Loess%20Plateau%20of%20North%20China&rft.jtitle=%E4%B8%AD%E5%9B%BD%E7%A7%91%E5%AD%A6%E9%80%9A%E6%8A%A5%EF%BC%9A%E8%8B%B1%E6%96%87%E7%89%88&rft.au=%E9%99%88%E9%AA%8F%20%E5%AE%89%E8%8A%B7%E7%94%9F%20%E7%8E%8B%E6%B4%AA%E6%B6%9B%20%E9%AB%98%E7%87%95&rft.date=1996&rft.issue=18&rft.spage=1542&rft.epage=1545&rft.pages=1542-1545&rft.issn=2095-9273&rft_id=info:doi/&rft_dat=%3Cchongqing%3E4001157409%3C/chongqing%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_cqvip_id=4001157409&rfr_iscdi=true |