ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
鄂尔多斯盆地长城系沉积充填格架与源区物质组成
  
关键词:Ordos Basin  Changcheng system  detrital zircon dating  Mesoproterozoic  provenance analysis
基金项目:本文由中国石油长庆油田分公司重大科技专项“鄂尔多斯盆地地震格架大剖面综合解释与基础地质研究”(编号: 2023DZZ02)、中国地质科学院基本科研业务费专项经费(编号: JKYDM2025201)和中国地质调查局地质调查项目“鄂尔多斯东南缘区域基础地质调查”(编号: DD20242779)联合资助。
作者单位E-mail
张雷 成都理工大学沉积地质研究院中国石油长庆油田公司勘探开发研究院低渗透油气田勘探开发国家工程实验室 zhanglei01_cq@petrochina.com.cn 
王永超 中国地质科学院 yongchao@cags.ac.cn 
李钊 中国石油长庆油田公司勘探开发研究院低渗透油气田勘探开发国家工程实验室  
魏丽娟 军事科学院国防工程研究院 376177045@qq.com 
李涵 中国石油长庆油田公司勘探开发研究院低渗透油气田勘探开发国家工程实验室  
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摘要:
Sedimentary Filling Framework and Provenance Composition of the Changcheng System in the Ordos Basin
      The Changcheng System in the Ordos Basin is currently a key target horizon for deep hydrocarbon exploration. However, research on its depositional age, filling framework, and provenance composition remains relatively limited. Based on the latest drilling data and core samples, this study has conducted petrographic analysis, detrital zircon dating, and stratigraphic correlation of the Changcheng System. Regional correlation reveals that the Changcheng System in the Ordos Basin exhibits a distinct “bipartite” lithological character, that is the lower section consists of mafic volcanic rocks while the upper section comprises clastic sedimentary rocks. This filling framework is highly similar to that of the Xionger Rift System. Combined with previous data, our new geochronological results constrain the basal age of the upper sedimentary section to 1 673~1 632 Ma, which aligns with the revised maximum depositional age of the Changcheng System in the Yanliao area. This age interval corresponds to a significant anorogenic magmatic event in the North China Craton, recording prolonged extension following a large igneous province event. The remaining zircons define three primary age peaks at ~1.82 Ga, 2.05 Ga, and 2.5 Ga. These were likely sourced from coeval granitic intrusions in the Yinshan and Taihang Mountains, as well as recycled Paleoproterozoic metasedimentary rocks. A minor contribution may derive from proximal granitoids within the basin.
ZHANG Lei,WANG Yongchao,LI Zhao,WEI Lijuan,LI Han.2026.Sedimentary Filling Framework and Provenance Composition of the Changcheng System in the Ordos Basin[J].Acta Geoscientica Sinica,47(4):715-732.
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