Detrital zircon age model of Ordovician Wenquan quartzite south of Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet： Constraint on tectonic affinity and source regions
Early to Middle Ordovician strata, including Wenquan quartzite, occur widely in the Himalaya, Lhasa, and south Qiangtang blocks. The Wenquan quartzite occurs on the south side of the Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet. A total of 145 analyses on detrital zircons from the quartzite...
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| Veröffentlicht in: | Science China. Earth sciences 2011-07, Vol.54 (7), p.1034-1042 |
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| creator | Dong, ChunYan Li, Cai Wan, YuSheng Wang, Wei Wu, YanWang Xie, HangQiang Liu, DunYi |
| description | Early to Middle Ordovician strata, including Wenquan quartzite, occur widely in the Himalaya, Lhasa, and south Qiangtang blocks. The Wenquan quartzite occurs on the south side of the Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet. A total of 145 analyses on detrital zircons from the quartzite show five age ranges of 520-700, ca. 800, 900-1100, 1800-1900, and 2400-2500 Ma, with particularly distinct age peaks of 625 and 950 Ma. The reliable youngest detrital zircon age is 525 Ma, and the oldest, 3180 Ma. Detrital zircons show large variations in Hf isotope composition, with depleted mantle model ages tDM（Hf） ranging from 750 to 3786 Ma. Based on data obtained in this study and by others, the main conclusions are as follows： 1） Low-grade metamorphic sedimentary rocks are distributed extensively in the south of the Lungmuco-Shuanghu Suture and are Phanerozoic in age; 2） Pan-African and Grenville-Jinning tectono-thermal events were well developed in the source region of the Wenquan quartzite; 3） the source region shows crustal addition and recycling of different periods; 4） Wenquan quartzite was derived from the Gondwana metamorphic basement, suggesting that the Qiangtang block is a Gondwanan fragment. |
| doi_str_mv | 10.1007/s11430-010-4166-x |
| format | Article |
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The Wenquan quartzite occurs on the south side of the Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet. A total of 145 analyses on detrital zircons from the quartzite show five age ranges of 520-700, ca. 800, 900-1100, 1800-1900, and 2400-2500 Ma, with particularly distinct age peaks of 625 and 950 Ma. The reliable youngest detrital zircon age is 525 Ma, and the oldest, 3180 Ma. Detrital zircons show large variations in Hf isotope composition, with depleted mantle model ages tDM（Hf） ranging from 750 to 3786 Ma. Based on data obtained in this study and by others, the main conclusions are as follows： 1） Low-grade metamorphic sedimentary rocks are distributed extensively in the south of the Lungmuco-Shuanghu Suture and are Phanerozoic in age; 2） Pan-African and Grenville-Jinning tectono-thermal events were well developed in the source region of the Wenquan quartzite; 3） the source region shows crustal addition and recycling of different periods; 4） Wenquan quartzite was derived from the Gondwana metamorphic basement, suggesting that the Qiangtang block is a Gondwanan fragment.</description><identifier>ISSN: 1674-7313</identifier><identifier>EISSN: 1869-1897</identifier><identifier>DOI: 10.1007/s11430-010-4166-x</identifier><language>eng</language><publisher>Heidelberg: SP Science China Press</publisher><subject>Earth and Environmental Science ; Earth Sciences ; Ordovician ; Research Paper ; Sedimentary rocks ; Zirconium ; 奥陶系 ; 模型构造 ; 温泉 ; 石英岩 ; 碎屑锆石 ; 缝合带 ; 羌塘地区 ; 锆石年龄</subject><ispartof>Science China. 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Earth sciences</title><addtitle>Sci. China Earth Sci</addtitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><description>Early to Middle Ordovician strata, including Wenquan quartzite, occur widely in the Himalaya, Lhasa, and south Qiangtang blocks. The Wenquan quartzite occurs on the south side of the Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet. A total of 145 analyses on detrital zircons from the quartzite show five age ranges of 520-700, ca. 800, 900-1100, 1800-1900, and 2400-2500 Ma, with particularly distinct age peaks of 625 and 950 Ma. The reliable youngest detrital zircon age is 525 Ma, and the oldest, 3180 Ma. Detrital zircons show large variations in Hf isotope composition, with depleted mantle model ages tDM（Hf） ranging from 750 to 3786 Ma. Based on data obtained in this study and by others, the main conclusions are as follows： 1） Low-grade metamorphic sedimentary rocks are distributed extensively in the south of the Lungmuco-Shuanghu Suture and are Phanerozoic in age; 2） Pan-African and Grenville-Jinning tectono-thermal events were well developed in the source region of the Wenquan quartzite; 3） the source region shows crustal addition and recycling of different periods; 4） Wenquan quartzite was derived from the Gondwana metamorphic basement, suggesting that the Qiangtang block is a Gondwanan fragment.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ordovician</subject><subject>Research Paper</subject><subject>Sedimentary rocks</subject><subject>Zirconium</subject><subject>奥陶系</subject><subject>模型构造</subject><subject>温泉</subject><subject>石英岩</subject><subject>碎屑锆石</subject><subject>缝合带</subject><subject>羌塘地区</subject><subject>锆石年龄</subject><issn>1674-7313</issn><issn>1869-1897</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kU1qHDEQhZuQQIzjA2SnZJVFlEitHkm9DJNfGDDBDlkKtbq6W6ZH8kjqYPsoOUROkDvlCqlhjA1eWCBVgb5Xr-BV1UvO3nHG1PvMeSMYZZzRhktJr55UR1zLlnLdqqfYS9VQJbh4Xp3kfMHwCPyp1VH15yOU5IudyY1PLgZiRyDb2MNM4kBOUx9_eedtID8h7Bas-KRy4wuQHJcy7anNEsbt4iI9m5AYp4WcLWVJQHwgZQLyHfVjwUtsAvuWnPsOyr-_v8k6hlyS9aEQdC7gSgzeETsMPvhyTWzo9y7JAUkweqRfVM8GO2c4ua3H1Y_Pn87XX-nm9Mu39YcNdUI1hWrlGO8aBmzVSWdtb1ets4Ora931PXfCdc5KLlunWQ_QdrbXnNfSMdGxruHiuHpzmHuZ4m6BXMzWZwfzbAPEJRuuVroWLWtrRF8_QC9w5YDbGa0wFqnUCiF-gFyKOScYzGXyW5uuDWdmn6E5ZGgwQ7PP0Fyhpj5oMrJhhHQ_-DHRq1ujKYZxh7o7J6FFrSRT4j9WTq_n</recordid><startdate>20110701</startdate><enddate>20110701</enddate><creator>Dong, ChunYan</creator><creator>Li, Cai</creator><creator>Wan, YuSheng</creator><creator>Wang, Wei</creator><creator>Wu, YanWang</creator><creator>Xie, HangQiang</creator><creator>Liu, DunYi</creator><general>SP Science China Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20110701</creationdate><title>Detrital zircon age model of Ordovician Wenquan quartzite south of Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet： Constraint on tectonic affinity and source regions</title><author>Dong, ChunYan ; Li, Cai ; Wan, YuSheng ; Wang, Wei ; Wu, YanWang ; Xie, HangQiang ; Liu, DunYi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c374t-87c01b40e05b6caada59cafc228bdd1c3cbca6169c80dee9bad81126c03b0b413</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ordovician</topic><topic>Research Paper</topic><topic>Sedimentary rocks</topic><topic>Zirconium</topic><topic>奥陶系</topic><topic>模型构造</topic><topic>温泉</topic><topic>石英岩</topic><topic>碎屑锆石</topic><topic>缝合带</topic><topic>羌塘地区</topic><topic>锆石年龄</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Dong, ChunYan</creatorcontrib><creatorcontrib>Li, Cai</creatorcontrib><creatorcontrib>Wan, YuSheng</creatorcontrib><creatorcontrib>Wang, Wei</creatorcontrib><creatorcontrib>Wu, YanWang</creatorcontrib><creatorcontrib>Xie, HangQiang</creatorcontrib><creatorcontrib>Liu, DunYi</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><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><jtitle>Science China. Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Dong, ChunYan</au><au>Li, Cai</au><au>Wan, YuSheng</au><au>Wang, Wei</au><au>Wu, YanWang</au><au>Xie, HangQiang</au><au>Liu, DunYi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Detrital zircon age model of Ordovician Wenquan quartzite south of Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet： Constraint on tectonic affinity and source regions</atitle><jtitle>Science China. Earth sciences</jtitle><stitle>Sci. China Earth Sci</stitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><date>2011-07-01</date><risdate>2011</risdate><volume>54</volume><issue>7</issue><spage>1034</spage><epage>1042</epage><pages>1034-1042</pages><issn>1674-7313</issn><eissn>1869-1897</eissn><abstract>Early to Middle Ordovician strata, including Wenquan quartzite, occur widely in the Himalaya, Lhasa, and south Qiangtang blocks. The Wenquan quartzite occurs on the south side of the Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet. A total of 145 analyses on detrital zircons from the quartzite show five age ranges of 520-700, ca. 800, 900-1100, 1800-1900, and 2400-2500 Ma, with particularly distinct age peaks of 625 and 950 Ma. The reliable youngest detrital zircon age is 525 Ma, and the oldest, 3180 Ma. Detrital zircons show large variations in Hf isotope composition, with depleted mantle model ages tDM（Hf） ranging from 750 to 3786 Ma. Based on data obtained in this study and by others, the main conclusions are as follows： 1） Low-grade metamorphic sedimentary rocks are distributed extensively in the south of the Lungmuco-Shuanghu Suture and are Phanerozoic in age; 2） Pan-African and Grenville-Jinning tectono-thermal events were well developed in the source region of the Wenquan quartzite; 3） the source region shows crustal addition and recycling of different periods; 4） Wenquan quartzite was derived from the Gondwana metamorphic basement, suggesting that the Qiangtang block is a Gondwanan fragment.</abstract><cop>Heidelberg</cop><pub>SP Science China Press</pub><doi>10.1007/s11430-010-4166-x</doi><tpages>9</tpages></addata></record> |
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| subjects | Earth and Environmental Science Earth Sciences Ordovician Research Paper Sedimentary rocks Zirconium 奥陶系 模型构造 温泉 石英岩 碎屑锆石 缝合带 羌塘地区 锆石年龄 |
| title | Detrital zircon age model of Ordovician Wenquan quartzite south of Lungmuco-Shuanghu Suture in the Qiangtang area, Tibet： Constraint on tectonic affinity and source regions |
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