Provenance and tectonic setting transition as recorded in the Neoproterozoic strata, western Jiangnan Orogen: Implications for South China within Rodinia

The Neoproterozoic Tonian strata (ca. 870–725 Ma) in the western Jiangnan Orogen archive the records of sedimentary provenance and tectonic setting which can be used to understand the geological evolution of the South China Continent. These strata are separated into the basement and cover sequences...

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Veröffentlicht in:Di xue qian yuan. 2019-09, Vol.10 (5), p.1823-1839
Hauptverfasser: Zhang, Jiawei, Ye, Taiping, Dai, Yaran, Chen, Jianshu, Zhang, Hui, Dai, Chuangu, Yuan, Guohua, Jiang, Kaiyuan
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container_title Di xue qian yuan.
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creator Zhang, Jiawei
Ye, Taiping
Dai, Yaran
Chen, Jianshu
Zhang, Hui
Dai, Chuangu
Yuan, Guohua
Jiang, Kaiyuan
description The Neoproterozoic Tonian strata (ca. 870–725 Ma) in the western Jiangnan Orogen archive the records of sedimentary provenance and tectonic setting which can be used to understand the geological evolution of the South China Continent. These strata are separated into the basement and cover sequences by a regional angular unconformity. The basement sequence can be subdivided into the lower and the upper parts by the widespread interbedded ca. 840 Ma basalt with pillow structure. In the present work, 234 concordant detrital zircon analyses are obtained from three Tonian sandstone samples in the Fanjingshan district, Guizhou Province. Combined with previous results, a total of 1736 analyses of detrital zircon U-Pb ages derived from 12 formations of Tonian strata in the western Jiangnan Orogen are used to decipher the integrated sedimentary and tectonic histories. The zircons from the lowermost part of the basement sequence (the Yujiagou Formation) show oval morphology and display two Paleoproterozoic age peaks at 2325 Ma and 1845 Ma which are similar with the detrital zircon age peaks from the Late Paleoproterozoic to Early Mesoproterozoic Dongchuan/Dahongshan/Hekou groups, suggesting a passive margin basin in which the sediments were mainly sourced from the southwestern Yangtze Block. However, the zircon age population of the lower part of the basement sequence (the Xiaojiahe, Huixiangping formations and their equivalents) indicates the sedimentary derivation from bidirectional sources (the ca. 870 Ma arc materials in the south and the old detritus from the southwestern Yangtze Block) which is consistent with a back arc setting for the deposition of the sediments. Zircons from the upper part of the basement sequence (the Duyantang Formation and its equivalent) show euhedral and subangular morphology and display a unimodal age peak at ca. 835 Ma. This sequence was possibly deposited in a convergent setting and the detritus were came from the locally distributed syn-collisional igneous rocks. The lower part of the cover sequence (the Xinzhai and Wuye formations and their equivalents) shows a distinct zircon age peak at 815–809 Ma and two subordinate peaks at 2485 Ma and 2018 Ma, suggesting that the basin had gradually transformed into a continental rift basin and received the detritus from the ca. 815 Ma post-collisional magmatic rocks as well as from different Paleoproterozoic source rocks in the northern Yangtze Block. We propose a tectonic evolution model th
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These strata are separated into the basement and cover sequences by a regional angular unconformity. The basement sequence can be subdivided into the lower and the upper parts by the widespread interbedded ca. 840 Ma basalt with pillow structure. In the present work, 234 concordant detrital zircon analyses are obtained from three Tonian sandstone samples in the Fanjingshan district, Guizhou Province. Combined with previous results, a total of 1736 analyses of detrital zircon U-Pb ages derived from 12 formations of Tonian strata in the western Jiangnan Orogen are used to decipher the integrated sedimentary and tectonic histories. The zircons from the lowermost part of the basement sequence (the Yujiagou Formation) show oval morphology and display two Paleoproterozoic age peaks at 2325 Ma and 1845 Ma which are similar with the detrital zircon age peaks from the Late Paleoproterozoic to Early Mesoproterozoic Dongchuan/Dahongshan/Hekou groups, suggesting a passive margin basin in which the sediments were mainly sourced from the southwestern Yangtze Block. However, the zircon age population of the lower part of the basement sequence (the Xiaojiahe, Huixiangping formations and their equivalents) indicates the sedimentary derivation from bidirectional sources (the ca. 870 Ma arc materials in the south and the old detritus from the southwestern Yangtze Block) which is consistent with a back arc setting for the deposition of the sediments. Zircons from the upper part of the basement sequence (the Duyantang Formation and its equivalent) show euhedral and subangular morphology and display a unimodal age peak at ca. 835 Ma. This sequence was possibly deposited in a convergent setting and the detritus were came from the locally distributed syn-collisional igneous rocks. The lower part of the cover sequence (the Xinzhai and Wuye formations and their equivalents) shows a distinct zircon age peak at 815–809 Ma and two subordinate peaks at 2485 Ma and 2018 Ma, suggesting that the basin had gradually transformed into a continental rift basin and received the detritus from the ca. 815 Ma post-collisional magmatic rocks as well as from different Paleoproterozoic source rocks in the northern Yangtze Block. We propose a tectonic evolution model that envisages eruption of ca. 840 Ma basalt in a back arc basin that existed during ca. 870–835 Ma, an angular unconformity was formed during amalgamation of the Yangtze Block and the Cathaysia Block at ca. 835–820 Ma and the rifting of the South China Continent was initiated at ca. 800 Ma. Our study concludes that the South China Continent was formed on the periphery of the Rodinia supercontinent. [Display omitted] •1736 analyses of detrital zircon U-Pb ages were used in this study.•Three episodes (870, 835, 815 Ma) of magmatism had been discovered.•Subduction and back arc extension were developed at 870–835 Ma.•Amalgamation of Yangtze and Cathysia blocks was occurred at 835–820 Ma.•The South China Continent started rifting since 800 Ma.</description><identifier>ISSN: 1674-9871</identifier><identifier>EISSN: 2588-9192</identifier><identifier>DOI: 10.1016/j.gsf.2018.10.009</identifier><language>eng</language><publisher>Oxford: Elsevier B.V</publisher><subject>Age ; Arc deposition ; Back arc basin ; Basalt ; Detrital zircon ; Detritus ; Equivalence ; Evolution ; Fanjingshan ; Formations ; Geological time ; Igneous rocks ; Magma ; Morphology ; Orogeny ; Precambrian ; Provenance ; Radiometric dating ; Sandstone ; Sediments ; Sibao ; Strata ; Tectonics ; Tonian ; Zircon</subject><ispartof>Di xue qian yuan., 2019-09, Vol.10 (5), p.1823-1839</ispartof><rights>2019 China University of Geosciences (Beijing) and Peking University</rights><rights>Copyright Elsevier Science Ltd. 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All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a423t-b73c9af2cdc5125d64272ca79d273cf7e711704cbaafa148ef3c78e4866d75463</citedby><cites>FETCH-LOGICAL-a423t-b73c9af2cdc5125d64272ca79d273cf7e711704cbaafa148ef3c78e4866d75463</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/dxqy-e/dxqy-e.jpg</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.gsf.2018.10.009$$EHTML$$P50$$Gelsevier$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids></links><search><creatorcontrib>Zhang, Jiawei</creatorcontrib><creatorcontrib>Ye, Taiping</creatorcontrib><creatorcontrib>Dai, Yaran</creatorcontrib><creatorcontrib>Chen, Jianshu</creatorcontrib><creatorcontrib>Zhang, Hui</creatorcontrib><creatorcontrib>Dai, Chuangu</creatorcontrib><creatorcontrib>Yuan, Guohua</creatorcontrib><creatorcontrib>Jiang, Kaiyuan</creatorcontrib><title>Provenance and tectonic setting transition as recorded in the Neoproterozoic strata, western Jiangnan Orogen: Implications for South China within Rodinia</title><title>Di xue qian yuan.</title><description>The Neoproterozoic Tonian strata (ca. 870–725 Ma) in the western Jiangnan Orogen archive the records of sedimentary provenance and tectonic setting which can be used to understand the geological evolution of the South China Continent. These strata are separated into the basement and cover sequences by a regional angular unconformity. The basement sequence can be subdivided into the lower and the upper parts by the widespread interbedded ca. 840 Ma basalt with pillow structure. In the present work, 234 concordant detrital zircon analyses are obtained from three Tonian sandstone samples in the Fanjingshan district, Guizhou Province. Combined with previous results, a total of 1736 analyses of detrital zircon U-Pb ages derived from 12 formations of Tonian strata in the western Jiangnan Orogen are used to decipher the integrated sedimentary and tectonic histories. The zircons from the lowermost part of the basement sequence (the Yujiagou Formation) show oval morphology and display two Paleoproterozoic age peaks at 2325 Ma and 1845 Ma which are similar with the detrital zircon age peaks from the Late Paleoproterozoic to Early Mesoproterozoic Dongchuan/Dahongshan/Hekou groups, suggesting a passive margin basin in which the sediments were mainly sourced from the southwestern Yangtze Block. However, the zircon age population of the lower part of the basement sequence (the Xiaojiahe, Huixiangping formations and their equivalents) indicates the sedimentary derivation from bidirectional sources (the ca. 870 Ma arc materials in the south and the old detritus from the southwestern Yangtze Block) which is consistent with a back arc setting for the deposition of the sediments. Zircons from the upper part of the basement sequence (the Duyantang Formation and its equivalent) show euhedral and subangular morphology and display a unimodal age peak at ca. 835 Ma. This sequence was possibly deposited in a convergent setting and the detritus were came from the locally distributed syn-collisional igneous rocks. The lower part of the cover sequence (the Xinzhai and Wuye formations and their equivalents) shows a distinct zircon age peak at 815–809 Ma and two subordinate peaks at 2485 Ma and 2018 Ma, suggesting that the basin had gradually transformed into a continental rift basin and received the detritus from the ca. 815 Ma post-collisional magmatic rocks as well as from different Paleoproterozoic source rocks in the northern Yangtze Block. We propose a tectonic evolution model that envisages eruption of ca. 840 Ma basalt in a back arc basin that existed during ca. 870–835 Ma, an angular unconformity was formed during amalgamation of the Yangtze Block and the Cathaysia Block at ca. 835–820 Ma and the rifting of the South China Continent was initiated at ca. 800 Ma. Our study concludes that the South China Continent was formed on the periphery of the Rodinia supercontinent. [Display omitted] •1736 analyses of detrital zircon U-Pb ages were used in this study.•Three episodes (870, 835, 815 Ma) of magmatism had been discovered.•Subduction and back arc extension were developed at 870–835 Ma.•Amalgamation of Yangtze and Cathysia blocks was occurred at 835–820 Ma.•The South China Continent started rifting since 800 Ma.</description><subject>Age</subject><subject>Arc deposition</subject><subject>Back arc basin</subject><subject>Basalt</subject><subject>Detrital zircon</subject><subject>Detritus</subject><subject>Equivalence</subject><subject>Evolution</subject><subject>Fanjingshan</subject><subject>Formations</subject><subject>Geological time</subject><subject>Igneous rocks</subject><subject>Magma</subject><subject>Morphology</subject><subject>Orogeny</subject><subject>Precambrian</subject><subject>Provenance</subject><subject>Radiometric dating</subject><subject>Sandstone</subject><subject>Sediments</subject><subject>Sibao</subject><subject>Strata</subject><subject>Tectonics</subject><subject>Tonian</subject><subject>Zircon</subject><issn>1674-9871</issn><issn>2588-9192</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNp9UU1vEzEQXSGQiNr-AG6WOHBhg-31rnfhhKICRRVFfJytqT1OHLV2ajsN5Z_wbzurIHHDl5HH773xm9c0LwRfCi6GN9vluvil5GKk-5Lz6UmzkP04tpOY5NNmIQat2mnU4nlzVsqW09F61Jovmj9fc7rHCNEig-hYRVtTDJYVrDXENasZYgk1pMigsIw2ZYeOhcjqBtkXTLucKub0O80kQld4zQ5YqBfZ5wBxTeLsKqc1xrfs4nZ3EyzMcoX5lNn3tK8bttqECOwQKlX2LbkQA5w2zzzcFDz7W0-anx_Of6w-tZdXHy9W7y9bULKr7bXu7AReWmd7IXs3KKmlBT05SS9eoxZCc2WvATwINaLvrB5RjcPgdK-G7qR5ddQ9QPT0XbNN-xxponG_7h4M0lon3nOhCPnyiCTLd3uy-A8qOz4o3Qk5EUocUTanUjJ6s8vhFvKDEdzMcZmtobjMHNfcoriI8-7IQTJ6HzCbYgNSJi7QxqtxKfyH_QgkSZ_i</recordid><startdate>20190901</startdate><enddate>20190901</enddate><creator>Zhang, Jiawei</creator><creator>Ye, Taiping</creator><creator>Dai, Yaran</creator><creator>Chen, Jianshu</creator><creator>Zhang, Hui</creator><creator>Dai, Chuangu</creator><creator>Yuan, Guohua</creator><creator>Jiang, Kaiyuan</creator><general>Elsevier B.V</general><general>Elsevier Science Ltd</general><general>Key Laboratory of Carrying Capacity Assessment for Resources and Environment,Ministry of Land and Resources,Beijing 101149,China</general><general>Chinese Academy of Land and Resources Economics,Beijing 101149,China</general><general>Key Laboratory of Carrying Capacity Assessment for Resources and Environment,Ministry of Land and Resources,Beijing 101149,China%Guizhou Central Laboratory of Geology and Mineral Resources,Bureau of Geology and Mineral Exploration and Development of Guizhou Province,Guiyang 550018,China%Guizhou Geological Survey,Bureau of Geology and Mineral Exploration and Development of Guizhou Province,Guiyang 550081,China%Chinese Academy of Land and Resources Economics,Beijing 101149,China</general><general>Guizhou Geological Survey,Bureau of Geology and Mineral Exploration and Development of Guizhou Province,Guiyang 550081,China</general><scope>6I.</scope><scope>AAFTH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20190901</creationdate><title>Provenance and tectonic setting transition as recorded in the Neoproterozoic strata, western Jiangnan Orogen: Implications for South China within Rodinia</title><author>Zhang, Jiawei ; Ye, Taiping ; Dai, Yaran ; Chen, Jianshu ; Zhang, Hui ; Dai, Chuangu ; Yuan, Guohua ; Jiang, Kaiyuan</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a423t-b73c9af2cdc5125d64272ca79d273cf7e711704cbaafa148ef3c78e4866d75463</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Age</topic><topic>Arc deposition</topic><topic>Back arc basin</topic><topic>Basalt</topic><topic>Detrital zircon</topic><topic>Detritus</topic><topic>Equivalence</topic><topic>Evolution</topic><topic>Fanjingshan</topic><topic>Formations</topic><topic>Geological time</topic><topic>Igneous rocks</topic><topic>Magma</topic><topic>Morphology</topic><topic>Orogeny</topic><topic>Precambrian</topic><topic>Provenance</topic><topic>Radiometric dating</topic><topic>Sandstone</topic><topic>Sediments</topic><topic>Sibao</topic><topic>Strata</topic><topic>Tectonics</topic><topic>Tonian</topic><topic>Zircon</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhang, Jiawei</creatorcontrib><creatorcontrib>Ye, Taiping</creatorcontrib><creatorcontrib>Dai, Yaran</creatorcontrib><creatorcontrib>Chen, Jianshu</creatorcontrib><creatorcontrib>Zhang, Hui</creatorcontrib><creatorcontrib>Dai, Chuangu</creatorcontrib><creatorcontrib>Yuan, Guohua</creatorcontrib><creatorcontrib>Jiang, Kaiyuan</creatorcontrib><collection>ScienceDirect Open Access Titles</collection><collection>Elsevier:ScienceDirect:Open Access</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</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>Di xue qian yuan.</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhang, Jiawei</au><au>Ye, Taiping</au><au>Dai, Yaran</au><au>Chen, Jianshu</au><au>Zhang, Hui</au><au>Dai, Chuangu</au><au>Yuan, Guohua</au><au>Jiang, Kaiyuan</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Provenance and tectonic setting transition as recorded in the Neoproterozoic strata, western Jiangnan Orogen: Implications for South China within Rodinia</atitle><jtitle>Di xue qian yuan.</jtitle><date>2019-09-01</date><risdate>2019</risdate><volume>10</volume><issue>5</issue><spage>1823</spage><epage>1839</epage><pages>1823-1839</pages><issn>1674-9871</issn><eissn>2588-9192</eissn><abstract>The Neoproterozoic Tonian strata (ca. 870–725 Ma) in the western Jiangnan Orogen archive the records of sedimentary provenance and tectonic setting which can be used to understand the geological evolution of the South China Continent. These strata are separated into the basement and cover sequences by a regional angular unconformity. The basement sequence can be subdivided into the lower and the upper parts by the widespread interbedded ca. 840 Ma basalt with pillow structure. In the present work, 234 concordant detrital zircon analyses are obtained from three Tonian sandstone samples in the Fanjingshan district, Guizhou Province. Combined with previous results, a total of 1736 analyses of detrital zircon U-Pb ages derived from 12 formations of Tonian strata in the western Jiangnan Orogen are used to decipher the integrated sedimentary and tectonic histories. The zircons from the lowermost part of the basement sequence (the Yujiagou Formation) show oval morphology and display two Paleoproterozoic age peaks at 2325 Ma and 1845 Ma which are similar with the detrital zircon age peaks from the Late Paleoproterozoic to Early Mesoproterozoic Dongchuan/Dahongshan/Hekou groups, suggesting a passive margin basin in which the sediments were mainly sourced from the southwestern Yangtze Block. However, the zircon age population of the lower part of the basement sequence (the Xiaojiahe, Huixiangping formations and their equivalents) indicates the sedimentary derivation from bidirectional sources (the ca. 870 Ma arc materials in the south and the old detritus from the southwestern Yangtze Block) which is consistent with a back arc setting for the deposition of the sediments. Zircons from the upper part of the basement sequence (the Duyantang Formation and its equivalent) show euhedral and subangular morphology and display a unimodal age peak at ca. 835 Ma. This sequence was possibly deposited in a convergent setting and the detritus were came from the locally distributed syn-collisional igneous rocks. The lower part of the cover sequence (the Xinzhai and Wuye formations and their equivalents) shows a distinct zircon age peak at 815–809 Ma and two subordinate peaks at 2485 Ma and 2018 Ma, suggesting that the basin had gradually transformed into a continental rift basin and received the detritus from the ca. 815 Ma post-collisional magmatic rocks as well as from different Paleoproterozoic source rocks in the northern Yangtze Block. We propose a tectonic evolution model that envisages eruption of ca. 840 Ma basalt in a back arc basin that existed during ca. 870–835 Ma, an angular unconformity was formed during amalgamation of the Yangtze Block and the Cathaysia Block at ca. 835–820 Ma and the rifting of the South China Continent was initiated at ca. 800 Ma. Our study concludes that the South China Continent was formed on the periphery of the Rodinia supercontinent. [Display omitted] •1736 analyses of detrital zircon U-Pb ages were used in this study.•Three episodes (870, 835, 815 Ma) of magmatism had been discovered.•Subduction and back arc extension were developed at 870–835 Ma.•Amalgamation of Yangtze and Cathysia blocks was occurred at 835–820 Ma.•The South China Continent started rifting since 800 Ma.</abstract><cop>Oxford</cop><pub>Elsevier B.V</pub><doi>10.1016/j.gsf.2018.10.009</doi><tpages>17</tpages><oa>free_for_read</oa></addata></record>
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subjects Age
Arc deposition
Back arc basin
Basalt
Detrital zircon
Detritus
Equivalence
Evolution
Fanjingshan
Formations
Geological time
Igneous rocks
Magma
Morphology
Orogeny
Precambrian
Provenance
Radiometric dating
Sandstone
Sediments
Sibao
Strata
Tectonics
Tonian
Zircon
title Provenance and tectonic setting transition as recorded in the Neoproterozoic strata, western Jiangnan Orogen: Implications for South China within Rodinia
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