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松辽盆地开鲁地区明水组沉积特征及控矿因素分析

柳东良

铀矿地质2026,Vol.42Issue(3):417-429,13.
铀矿地质2026,Vol.42Issue(3):417-429,13.DOI:10.3969/j.issn.1000-0658.2026.42.031

松辽盆地开鲁地区明水组沉积特征及控矿因素分析

Analysis of Sedimentary Characteristics and Ore-controlling Factors of Mingshui Formation in Kailu Area,Songliao Basin

柳东良1

作者信息

  • 1. 核工业二四三大队,内蒙古 赤峰 024000
  • 折叠

摘要

Abstract

To clarify the structural-sedimentary characteristics and uranium metallogenic potential of Mingshui Formation in Kailu area,western Songliao Basin,so as to support regional uranium exploration efforts,this study systematically analyzes the tectonic setting,sedimentary features,and uranium mineralization conditions based on regional geological data and drill core information by field investigations,sampling,geophysical logging,drilling profile logging,and integrated analysis.The results indicated that the sedimentary system of Mingshui Formation in the study area was dominated by terrigenous clastic fluvial-deltaic systems,mainly including braided river,meandering river,and delta facies,with the meandering river facies being the most developed.The regional structural framework forms a complete groundwater recharge-runoff-discharge system.Uranium mineralization was jointly controlled by uranium sources,oxidation zones,and fault structures.The mineralization process can be divided into two stages:the sedimentation and burial stage of pre-metallogenic potential uranium-bearing rock series,and the uplift and mineralization stage of uranium reservoirs during the metallogenic period.Uranium mineralization mainly occurs as tabular or lentiform bodies within the variegated mudstone-sandstone of the first member of the Mingshui Formation,with uranium anomalies and mineralized horizons primarily located in the low-to-high resistivity transition zone.Comprehensive analysis suggests that the first member of Mingshui Formation in Kailu area has significant uranium metallogenic potential,with specific sedimentary zones in the upper and lower reaches of the meandering river being favorable targets for uranium enrichment.

关键词

砂岩型铀矿/沉积体系特征/明水组/开鲁地区/松辽盆地

Key words

sandstone-type uranium deposit/sedimentary system characteristics/Mingshui Formation/Kailu area/Songliao Basin

分类

天文与地球科学

引用本文复制引用

柳东良..松辽盆地开鲁地区明水组沉积特征及控矿因素分析[J].铀矿地质,2026,42(3):417-429,13.

基金项目

中国核工业地质局项目"松辽盆地通辽—大庆地区铀矿资源调查评价与勘查"(编号:202212)和"内蒙古奈曼旗八仙筒—开鲁县建华地区铀矿资源调查评价"(编号:202212-6)联合资助. (编号:202212)

铀矿地质

1000-0658

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