ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
皖北新元古代贾园组混积岩物源和构造背景的地球化学示踪
  
关键词:provenance  tectonic setting  diamictites  geochemistry  Neoproterozoic  northern Anhui Province
基金项目:国家自然科学基金(编号: 40873015);安徽省高校优秀青年人才基金(编号: 2010SQRL190);宿州学院博士基金(编号: 2009jb04)
作者单位E-mail
孙林华 宿州学院地球科学与工程学院 sunlinh@hotmail.com 
桂和荣 宿州学院地球科学与工程学院  
陈松 宿州学院地球科学与工程学院  
马艳平 宿州学院地球科学与工程学院  
王桂梁 中国矿业大学资源与地球科学学院  
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摘要:
Provenance and Tectonic Setting of the Neoproterozoic Diamictites from Jiayuan Formation in Northern Anhui Province: Evidence from Geochemical Study
      Field observation and petrographic study as well as a systematic analysis of major and trace elements (including rare earth elements) were carried out for diamictites from the Neoproterozoic Jiayuan Formation in northern Anhui Province. The results imply that these diamictites are composed of carbonates and terrigenous de-tritus of variable proportions (1/1.5~1/9) and belong to “mixed sedimentation with gradual facies change”. The concentrations of elements are closely related to the relative concentrations of carbonates and terrigenous detritus, whereas the ratios between La, Th, Zr and Sc are controlled by terrigenous detritus with limited variations, and hence can be used as tracers for the discrimination of provenance of terrigenous detritus and its tectonic back-ground. Geochemical features demonstrate that the terrigenous detritus was mainly derived from the continental arc felsic volcanics, with minor contribution from the old basement. Combined with recent research achievements, the authors hold that the Neoproterozoic sedimentation in northern Anhui Province probably took place between 1.0 and 0.8 Ga, and the sedimentary environment was related to the back arc extension of the southeastern margin of the North China Craton during the convergence of Rodinia supercontinent.
SUN Lin-hua,GUI He-rong,CHEN Song,MA Yan-ping,WANG Gui-liang.2010.Provenance and Tectonic Setting of the Neoproterozoic Diamictites from Jiayuan Formation in Northern Anhui Province: Evidence from Geochemical Study[J].Acta Geoscientica Sinica,31(6):833-842.
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