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松辽盆地南部开鲁坳陷姚家组砂岩物源示踪研究

冯绍南 严兆彬 张文文 吴修俣

铀矿地质2024,Vol.40Issue(4):633-647,15.
铀矿地质2024,Vol.40Issue(4):633-647,15.DOI:10.3969/j.issn.1000-0658.2024.40.057

松辽盆地南部开鲁坳陷姚家组砂岩物源示踪研究

Provenance Tracing of Yaojia Formation Sandstone in Kailu Depression,Southern Songliao Basin:Constraints From Petrogeochemistry and Zircon U-Pb Chronology

冯绍南 1严兆彬 1张文文 1吴修俣1

作者信息

  • 1. 东华理工大学 核资源与环境国家重点实验室,江西 南昌 330013
  • 折叠

摘要

Abstract

For the potential prediction and the evaluation of in-situ leachable sandstone type uranium deposit,the source of ore-bearing sand body it is the key factor.In this paper,the microtrace,rare earth elements and zircon chronology of sandstone samples from the Upper Cretaceous Yaojia Formation in the southern margin of Songliao Basin was studied for the tracing the source.The results showed that the content of REE is 100.08×10-6~134.06×10-6,which is characterized by the enrichment of LREE,flat of HREE and moderate negative Eu anomaly.The REE pattern of all samples are highly consistent,indicating that the source of Yaojia Formation came from the same source system.According to ∑REE-La/Yb,Hf-La/Th,Zr/Sc-Th/Sc and Cr/Th-Th/Sc diagrams combined with the microscopic characteristics of sandstone,the source rocks was found to be felsic rocks.U-Pb dating of detrital zircon showed that the concordant ages of the zircons are mainly distributed in three ranges,110~180 Ma,230~280 Ma,1 695~2 171 Ma.With the lithostratigraphic division,characteristics of trace and rare earth elements,age of magmatic rocks and regional tectonic evolution,the sediments of Yaojia Formation was believed to be originated from Ulanhot area in the southern part of the Greater Hinggan Mountains.

关键词

松辽盆地/姚家组/地球化学/锆石年代学/物源分析

Key words

Songliao Basin/Yaojia Formation/geochemistry/zircon chronology/provenance analysis

分类

天文与地球科学

引用本文复制引用

冯绍南,严兆彬,张文文,吴修俣..松辽盆地南部开鲁坳陷姚家组砂岩物源示踪研究[J].铀矿地质,2024,40(4):633-647,15.

基金项目

国家自然科学基金项目(编号:42072009、42062008)资助. (编号:42072009、42062008)

铀矿地质

OACSTPCD

1000-0658

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