New Zircon U-Pb Age of Granodiorite in Chifeng at the Northern Margin of North China Craton and Constraints on Plate Tectonic Evolution
Objective The North China Craton （NCC） is one of the oldest cratons in the world. The accretionary belt at its northern margin has been the focus of scholars both at home and abroad （Zhu Junbing and Ren Jishun, 2017）. In recent years, a series of Late Paleozoic-Mesozoic intrusions trending E-W have...
Gespeichert in:
| Veröffentlicht in: | Acta geologica Sinica (Beijing) 2018-02, Vol.92 (1), p.410-413 |
|---|---|
| Hauptverfasser: | , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 413 |
|---|---|
| container_issue | 1 |
| container_start_page | 410 |
| container_title | Acta geologica Sinica (Beijing) |
| container_volume | 92 |
| creator | CHEN, Jingsheng LI, Bin YANG, Hao LIU, Miao YANG, Fan LI, Wei WANG, Yan CUI, Tianri |
| description | Objective The North China Craton （NCC） is one of the oldest cratons in the world. The accretionary belt at its northern margin has been the focus of scholars both at home and abroad （Zhu Junbing and Ren Jishun, 2017）. In recent years, a series of Late Paleozoic-Mesozoic intrusions trending E-W have been discovered within the northern margin of the NCC, forming a magmatic belt. The study on the origin and tectonic setting of this magmatic belt not only has important significance for understanding the Late Paleozoic-Mesozoic tectonic evolution history of the northern margin of the NCC, but also can provide key constraints on the evolution of its surrounding Xing＇an- Mongolia orogenic belt and the Paleo-Asian Ocean. At present, no Devonian to early stage of Early Carboniferous intrusion has been reported within the northern margin of the NCC. |
| doi_str_mv | 10.1111/1755-6724.13521 |
| format | Article |
| fullrecord | <record><control><sourceid>wanfang_jour_proqu</sourceid><recordid>TN_cdi_wanfang_journals_dzxb_e201801031</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>674424544</cqvip_id><wanfj_id>dzxb_e201801031</wanfj_id><sourcerecordid>dzxb_e201801031</sourcerecordid><originalsourceid>FETCH-LOGICAL-c4451-cd45374ab870da805022b89aebb0f358e6913823bf727b631333e4e2a920e33b3</originalsourceid><addsrcrecordid>eNqFkU1P4zAQhi0E0kLhvFeLPXBKGX_F6bGKoLsSXxJw4WLZiZO66trgpMt2_8D-bRzawhFfxpp53ndGehH6TmBM0jsnUogsl5SPCROU7KHDj85--gNANhFEfENHXbcAyEVOxCH6f2Nf8ZOLVfD4MbszeNpaHBo8i9qH2oXoeoudx-XcNda3WPe4n1t8E2Iq0eNrHds0Tor31sB5jcuo-2SofY3L4Ls-auf7DqfW3VInwwdbpbmr8MWfsFz1LvhjdNDoZWdPtnWEHi8vHsqf2dXt7Fc5vcoqzgXJqpoLJrk2hYRaFyCAUlNMtDUGGiYKm08IKygzjaTS5Iwwxiy3VE8oWMYMG6Gzje-r9o32rVqEVfRpo6r__TXKUiAFEEjCEfqxIZ9jeFnZrv9EKUDBuJQwUOcbqoqh66Jt1HN0v3VcKwJqyEUNKaghBfWeS1Lk2wvc0q6_wtW0nN3vhKfbVfPg2xeXjt-Jc8k55YJz9gadUpkW</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2008347701</pqid></control><display><type>article</type><title>New Zircon U-Pb Age of Granodiorite in Chifeng at the Northern Margin of North China Craton and Constraints on Plate Tectonic Evolution</title><source>Wiley Online Library Journals Frontfile Complete</source><source>Alma/SFX Local Collection</source><creator>CHEN, Jingsheng ; LI, Bin ; YANG, Hao ; LIU, Miao ; YANG, Fan ; LI, Wei ; WANG, Yan ; CUI, Tianri</creator><creatorcontrib>CHEN, Jingsheng ; LI, Bin ; YANG, Hao ; LIU, Miao ; YANG, Fan ; LI, Wei ; WANG, Yan ; CUI, Tianri</creatorcontrib><description>Objective The North China Craton （NCC） is one of the oldest cratons in the world. The accretionary belt at its northern margin has been the focus of scholars both at home and abroad （Zhu Junbing and Ren Jishun, 2017）. In recent years, a series of Late Paleozoic-Mesozoic intrusions trending E-W have been discovered within the northern margin of the NCC, forming a magmatic belt. The study on the origin and tectonic setting of this magmatic belt not only has important significance for understanding the Late Paleozoic-Mesozoic tectonic evolution history of the northern margin of the NCC, but also can provide key constraints on the evolution of its surrounding Xing＇an- Mongolia orogenic belt and the Paleo-Asian Ocean. At present, no Devonian to early stage of Early Carboniferous intrusion has been reported within the northern margin of the NCC.</description><edition>English ed.</edition><identifier>ISSN: 1000-9515</identifier><identifier>EISSN: 1755-6724</identifier><identifier>DOI: 10.1111/1755-6724.13521</identifier><language>eng</language><publisher>Richmond: Wiley Subscription Services, Inc</publisher><subject>Cratons ; Plate tectonics ; Zircon</subject><ispartof>Acta geologica Sinica (Beijing), 2018-02, Vol.92 (1), p.410-413</ispartof><rights>2018 Geological Society of China</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4451-cd45374ab870da805022b89aebb0f358e6913823bf727b631333e4e2a920e33b3</citedby><cites>FETCH-LOGICAL-c4451-cd45374ab870da805022b89aebb0f358e6913823bf727b631333e4e2a920e33b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/86253X/86253X.jpg</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2F1755-6724.13521$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2F1755-6724.13521$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids></links><search><creatorcontrib>CHEN, Jingsheng</creatorcontrib><creatorcontrib>LI, Bin</creatorcontrib><creatorcontrib>YANG, Hao</creatorcontrib><creatorcontrib>LIU, Miao</creatorcontrib><creatorcontrib>YANG, Fan</creatorcontrib><creatorcontrib>LI, Wei</creatorcontrib><creatorcontrib>WANG, Yan</creatorcontrib><creatorcontrib>CUI, Tianri</creatorcontrib><title>New Zircon U-Pb Age of Granodiorite in Chifeng at the Northern Margin of North China Craton and Constraints on Plate Tectonic Evolution</title><title>Acta geologica Sinica (Beijing)</title><addtitle>Acta Geologica Sinica</addtitle><description>Objective The North China Craton （NCC） is one of the oldest cratons in the world. The accretionary belt at its northern margin has been the focus of scholars both at home and abroad （Zhu Junbing and Ren Jishun, 2017）. In recent years, a series of Late Paleozoic-Mesozoic intrusions trending E-W have been discovered within the northern margin of the NCC, forming a magmatic belt. The study on the origin and tectonic setting of this magmatic belt not only has important significance for understanding the Late Paleozoic-Mesozoic tectonic evolution history of the northern margin of the NCC, but also can provide key constraints on the evolution of its surrounding Xing＇an- Mongolia orogenic belt and the Paleo-Asian Ocean. At present, no Devonian to early stage of Early Carboniferous intrusion has been reported within the northern margin of the NCC.</description><subject>Cratons</subject><subject>Plate tectonics</subject><subject>Zircon</subject><issn>1000-9515</issn><issn>1755-6724</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNqFkU1P4zAQhi0E0kLhvFeLPXBKGX_F6bGKoLsSXxJw4WLZiZO66trgpMt2_8D-bRzawhFfxpp53ndGehH6TmBM0jsnUogsl5SPCROU7KHDj85--gNANhFEfENHXbcAyEVOxCH6f2Nf8ZOLVfD4MbszeNpaHBo8i9qH2oXoeoudx-XcNda3WPe4n1t8E2Iq0eNrHds0Tor31sB5jcuo-2SofY3L4Ls-auf7DqfW3VInwwdbpbmr8MWfsFz1LvhjdNDoZWdPtnWEHi8vHsqf2dXt7Fc5vcoqzgXJqpoLJrk2hYRaFyCAUlNMtDUGGiYKm08IKygzjaTS5Iwwxiy3VE8oWMYMG6Gzje-r9o32rVqEVfRpo6r__TXKUiAFEEjCEfqxIZ9jeFnZrv9EKUDBuJQwUOcbqoqh66Jt1HN0v3VcKwJqyEUNKaghBfWeS1Lk2wvc0q6_wtW0nN3vhKfbVfPg2xeXjt-Jc8k55YJz9gadUpkW</recordid><startdate>201802</startdate><enddate>201802</enddate><creator>CHEN, Jingsheng</creator><creator>LI, Bin</creator><creator>YANG, Hao</creator><creator>LIU, Miao</creator><creator>YANG, Fan</creator><creator>LI, Wei</creator><creator>WANG, Yan</creator><creator>CUI, Tianri</creator><general>Wiley Subscription Services, Inc</general><general>College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China%Shenyang Geological Survey Center of China Geological Survey, Shenyang 110034, Liaoning, China%College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China</general><general>Shenyang Geological Survey Center of China Geological Survey, Shenyang 110034, Liaoning, China</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>201802</creationdate><title>New Zircon U-Pb Age of Granodiorite in Chifeng at the Northern Margin of North China Craton and Constraints on Plate Tectonic Evolution</title><author>CHEN, Jingsheng ; LI, Bin ; YANG, Hao ; LIU, Miao ; YANG, Fan ; LI, Wei ; WANG, Yan ; CUI, Tianri</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4451-cd45374ab870da805022b89aebb0f358e6913823bf727b631333e4e2a920e33b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Cratons</topic><topic>Plate tectonics</topic><topic>Zircon</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>CHEN, Jingsheng</creatorcontrib><creatorcontrib>LI, Bin</creatorcontrib><creatorcontrib>YANG, Hao</creatorcontrib><creatorcontrib>LIU, Miao</creatorcontrib><creatorcontrib>YANG, Fan</creatorcontrib><creatorcontrib>LI, Wei</creatorcontrib><creatorcontrib>WANG, Yan</creatorcontrib><creatorcontrib>CUI, Tianri</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-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><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>Acta geologica Sinica (Beijing)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>CHEN, Jingsheng</au><au>LI, Bin</au><au>YANG, Hao</au><au>LIU, Miao</au><au>YANG, Fan</au><au>LI, Wei</au><au>WANG, Yan</au><au>CUI, Tianri</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>New Zircon U-Pb Age of Granodiorite in Chifeng at the Northern Margin of North China Craton and Constraints on Plate Tectonic Evolution</atitle><jtitle>Acta geologica Sinica (Beijing)</jtitle><addtitle>Acta Geologica Sinica</addtitle><date>2018-02</date><risdate>2018</risdate><volume>92</volume><issue>1</issue><spage>410</spage><epage>413</epage><pages>410-413</pages><issn>1000-9515</issn><eissn>1755-6724</eissn><abstract>Objective The North China Craton （NCC） is one of the oldest cratons in the world. The accretionary belt at its northern margin has been the focus of scholars both at home and abroad （Zhu Junbing and Ren Jishun, 2017）. In recent years, a series of Late Paleozoic-Mesozoic intrusions trending E-W have been discovered within the northern margin of the NCC, forming a magmatic belt. The study on the origin and tectonic setting of this magmatic belt not only has important significance for understanding the Late Paleozoic-Mesozoic tectonic evolution history of the northern margin of the NCC, but also can provide key constraints on the evolution of its surrounding Xing＇an- Mongolia orogenic belt and the Paleo-Asian Ocean. At present, no Devonian to early stage of Early Carboniferous intrusion has been reported within the northern margin of the NCC.</abstract><cop>Richmond</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1111/1755-6724.13521</doi><tpages>4</tpages><edition>English ed.</edition></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1000-9515 |
| ispartof | Acta geologica Sinica (Beijing), 2018-02, Vol.92 (1), p.410-413 |
| issn | 1000-9515 1755-6724 |
| language | eng |
| recordid | cdi_wanfang_journals_dzxb_e201801031 |
| source | Wiley Online Library Journals Frontfile Complete; Alma/SFX Local Collection |
| subjects | Cratons Plate tectonics Zircon |
| title | New Zircon U-Pb Age of Granodiorite in Chifeng at the Northern Margin of North China Craton and Constraints on Plate Tectonic Evolution |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-13T12%3A49%3A16IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=New%20Zircon%20U-Pb%20Age%20of%20Granodiorite%20in%20Chifeng%20at%20the%20Northern%20Margin%20of%20North%20China%20Craton%20and%20Constraints%20on%20Plate%20Tectonic%20Evolution&rft.jtitle=Acta%20geologica%20Sinica%20(Beijing)&rft.au=CHEN,%20Jingsheng&rft.date=2018-02&rft.volume=92&rft.issue=1&rft.spage=410&rft.epage=413&rft.pages=410-413&rft.issn=1000-9515&rft.eissn=1755-6724&rft_id=info:doi/10.1111/1755-6724.13521&rft_dat=%3Cwanfang_jour_proqu%3Edzxb_e201801031%3C/wanfang_jour_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2008347701&rft_id=info:pmid/&rft_cqvip_id=674424544&rft_wanfj_id=dzxb_e201801031&rfr_iscdi=true |