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内蒙古十二吐火山盆地铀矿化特征及成矿预测

吴燕清 林天发 臧亚辉 王天奇 郝晓飞 王常东 董小宇 杨志亮 王之晟 周舰 王洪志 王良玉

铀矿地质2026,Vol.42Issue(1):124-136,13.
铀矿地质2026,Vol.42Issue(1):124-136,13.DOI:10.3969/j.issn.1000-0658.2025.41.009

内蒙古十二吐火山盆地铀矿化特征及成矿预测

Uranium Mineralization Characteristics and Metallogenic Prediction of Shiertu Volcanic Basin in Inner Mongolia

吴燕清 1林天发 1臧亚辉 1王天奇 1郝晓飞 1王常东 1董小宇 1杨志亮 1王之晟 1周舰 1王洪志 1王良玉1

作者信息

  • 1. 核工业二四三大队,内蒙古 赤峰 024006
  • 折叠

摘要

Abstract

Shiertu volcanic basin is located at the southern end of Zhalantun volcanic rock-type uranium mineralization prospective belt in Inner Mongolia.It is confined by the regional NE-trending Huanggangliang-Ulanhot fault and the NW-trending Xilamulun river fault.Mesozoic volcanic eruptions were intense and frequent,providing favorable conditions for uranium mineralization.To analyze the uranium metallogenic conditions and predict prospective metallogenic areas,this paper summarized the uranium mineralization characteristics and analyzed the ore-controlling factors by integrating field geological survey,remote sensing interpretation,and airborne radiometric survey data,as well as drilling and trenching data.The research results show that uranium mineralization in Shiertu volcanic basin mainly occurs along NE-trending FS1 fault and NW-trending FS6 fault,and is often found near secondary NE-trending and NW-trending cover faults,volcanic structures,and subvolcanic dykes,or at their intersections and superimpositions.The host rocks are mainly the rhyolite,rhyolitic welded tuff,and acidic subvolcanic rocks of Manketouebo Formation.A comprehensive analysis suggests that uranium mineralization is mainly controlled by a combination of factors such as faults,acidic volcanic rocks,subvolcanic rocks,volcanic structures,and hydrothermal alteration.Uranium mineralization is closely related to hematitization,fluoritization,silicification,and illitization.The uranium mineralization in Shiertu volcanic basin falls into the medium-low temperature hydrothermal type and can be classified into three subtypes based on the occurring location:altered fracture zones,subvolcanic rocks,and interlayered fracture zones.Based on the summarized ore-controlling factors and exploration indicators,one exploration target area and two prospective mineralization areas were predicted for the next exploration.

关键词

铀矿化特征/控矿因素/成矿预测/十二吐盆地

Key words

uranium mineralization characteristics/ore-controlling factors/metallogenic prediction/Shiertu volcanic basin

分类

天文与地球科学

引用本文复制引用

吴燕清,林天发,臧亚辉,王天奇,郝晓飞,王常东,董小宇,杨志亮,王之晟,周舰,王洪志,王良玉..内蒙古十二吐火山盆地铀矿化特征及成矿预测[J].铀矿地质,2026,42(1):124-136,13.

基金项目

中国核工业地勘基金项目"河北省张北—内蒙古突泉地区铀-多金属矿资源调查评价与勘查"(编号:202312)资助. (编号:202312)

铀矿地质

1000-0658

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