A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE
Ⅰ. GEOLOGICAL BACKGROUND Covering an area of 1200 km~2, the Wugongshan migmatite-granite batholith is located on the northwestern margin of South China Caledonian folded region and the southern flank of Pingxiang-Guangfeng deep fault. It is characterized by the trinity of meta-sediments,
Gespeichert in:
| Veröffentlicht in: | 中国科学通报：英文版 1991 (24), p.2069-2072 |
|---|---|
| 1. Verfasser: | |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 2072 |
|---|---|
| container_issue | 24 |
| container_start_page | 2069 |
| container_title | 中国科学通报：英文版 |
| container_volume | |
| creator | 徐士进 沈渭洲 王银喜 杨杰东 李惠民 |
| description | Ⅰ. GEOLOGICAL BACKGROUND Covering an area of 1200 km~2, the Wugongshan migmatite-granite batholith is located on the northwestern margin of South China Caledonian folded region and the southern flank of Pingxiang-Guangfeng deep fault. It is characterized by the trinity of meta-sediments, |
| format | Article |
| fullrecord | <record><control><sourceid>chongqing</sourceid><recordid>TN_cdi_chongqing_primary_1005288865</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>1005288865</cqvip_id><sourcerecordid>1005288865</sourcerecordid><originalsourceid>FETCH-chongqing_primary_10052888653</originalsourceid><addsrcrecordid>eNpjYeA0MrA01bU0MjfmYOAtLs4yMDAwNLE0MjEw52SwcFQIDgl1iVTw91MI8XBV8EvRDS5S8Az2D_EPcFXwdwMLhoe6-_u5B3s4-in4err7OoZ4hrjyMLCmJeYUp_JCaW4GZTfXEGcP3eSM_Lz0wsy89PiCoszcxKLKeEMDA1MjCwsLM1Nj4lQBAI0gMBc</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE</title><source>Alma/SFX Local Collection</source><creator>徐士进 沈渭洲 王银喜 杨杰东 李惠民</creator><creatorcontrib>徐士进 沈渭洲 王银喜 杨杰东 李惠民</creatorcontrib><description>Ⅰ. GEOLOGICAL BACKGROUND Covering an area of 1200 km~2, the Wugongshan migmatite-granite batholith is located on the northwestern margin of South China Caledonian folded region and the southern flank of Pingxiang-Guangfeng deep fault. It is characterized by the trinity of meta-sediments,</description><identifier>ISSN: 2095-9273</identifier><language>eng</language><subject>isotope ; migmatite ; Nd-Sr ; Wugongshan</subject><ispartof>中国科学通报：英文版, 1991 (24), p.2069-2072</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>徐士进 沈渭洲 王银喜 杨杰东 李惠民</creatorcontrib><title>A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE</title><title>中国科学通报：英文版</title><addtitle>Chinese Science Bulletin</addtitle><description>Ⅰ. GEOLOGICAL BACKGROUND Covering an area of 1200 km~2, the Wugongshan migmatite-granite batholith is located on the northwestern margin of South China Caledonian folded region and the southern flank of Pingxiang-Guangfeng deep fault. It is characterized by the trinity of meta-sediments,</description><subject>isotope</subject><subject>migmatite</subject><subject>Nd-Sr</subject><subject>Wugongshan</subject><issn>2095-9273</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1991</creationdate><recordtype>article</recordtype><recordid>eNpjYeA0MrA01bU0MjfmYOAtLs4yMDAwNLE0MjEw52SwcFQIDgl1iVTw91MI8XBV8EvRDS5S8Az2D_EPcFXwdwMLhoe6-_u5B3s4-in4err7OoZ4hrjyMLCmJeYUp_JCaW4GZTfXEGcP3eSM_Lz0wsy89PiCoszcxKLKeEMDA1MjCwsLM1Nj4lQBAI0gMBc</recordid><startdate>1991</startdate><enddate>1991</enddate><creator>徐士进 沈渭洲 王银喜 杨杰东 李惠民</creator><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope></search><sort><creationdate>1991</creationdate><title>A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE</title><author>徐士进 沈渭洲 王银喜 杨杰东 李惠民</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-chongqing_primary_10052888653</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1991</creationdate><topic>isotope</topic><topic>migmatite</topic><topic>Nd-Sr</topic><topic>Wugongshan</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>徐士进 沈渭洲 王银喜 杨杰东 李惠民</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- 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>徐士进 沈渭洲 王银喜 杨杰东 李惠民</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE</atitle><jtitle>中国科学通报：英文版</jtitle><addtitle>Chinese Science Bulletin</addtitle><date>1991</date><risdate>1991</risdate><issue>24</issue><spage>2069</spage><epage>2072</epage><pages>2069-2072</pages><issn>2095-9273</issn><abstract>Ⅰ. GEOLOGICAL BACKGROUND Covering an area of 1200 km~2, the Wugongshan migmatite-granite batholith is located on the northwestern margin of South China Caledonian folded region and the southern flank of Pingxiang-Guangfeng deep fault. It is characterized by the trinity of meta-sediments,</abstract></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 2095-9273 |
| ispartof | 中国科学通报：英文版, 1991 (24), p.2069-2072 |
| issn | 2095-9273 |
| language | eng |
| recordid | cdi_chongqing_primary_1005288865 |
| source | Alma/SFX Local Collection |
| subjects | isotope migmatite Nd-Sr Wugongshan |
| title | A STUDY ON THE Nd-Sr ISOTOPE OF THE WUGONGSHAN MIGMATITE |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-09T02%3A34%3A45IST&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=A%20STUDY%20ON%20THE%20Nd-Sr%20ISOTOPE%20OF%20THE%20WUGONGSHAN%20MIGMATITE&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=%E5%BE%90%E5%A3%AB%E8%BF%9B%20%E6%B2%88%E6%B8%AD%E6%B4%B2%20%E7%8E%8B%E9%93%B6%E5%96%9C%20%E6%9D%A8%E6%9D%B0%E4%B8%9C%20%E6%9D%8E%E6%83%A0%E6%B0%91&rft.date=1991&rft.issue=24&rft.spage=2069&rft.epage=2072&rft.pages=2069-2072&rft.issn=2095-9273&rft_id=info:doi/&rft_dat=%3Cchongqing%3E1005288865%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=1005288865&rfr_iscdi=true |