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二连盆地哈达图铀矿床铀成矿特征分析

颜小波 吕永华 郭虎科 张锋

铀矿地质2026,Vol.42Issue(2):218-228,11.
铀矿地质2026,Vol.42Issue(2):218-228,11.DOI:10.3969/j.issn.1000-0658.2026.42.016

二连盆地哈达图铀矿床铀成矿特征分析

Analysis of Uranium Metallogenic Characteristics of Hadatu Uranium Deposit in Erlian Basin,Inner Mongolia

颜小波 1吕永华 1郭虎科 2张锋1

作者信息

  • 1. 核工业二〇八大队,内蒙古 包头 014010
  • 2. 核工业二一六大队,新疆 乌鲁木齐 830011
  • 折叠

摘要

Abstract

Erlian Basin in the middle east of Inner Mongolia is a key exploration area for in-situ leachable sandstone type uranium deposits in northern China.With the innovation of prospecting theory and methods and the transformation of prospecting ideas,breakthroughs have been made in uranium exploration in Erlian Basin,especially the discovery of Hadatu uranium deposit,which has changed the prospecting model of Erlian Basin.In order to further expand the prospecting space in Hadu area,reach the bigger breakthrough in the ancient"Basaiqi"river channel from point to surface,this study made the preliminary analysis of the structural characteristics,stratigraphic characteristics,spatial distribution characteristics of sand body,characteristics of rock geochemical environment,ore body characteristics and ore characteristics of Hadatu uranium deposit.The result considered that Hadatu uranium deposit was a polygenetic sandstone type uranium deposit and the mineralization was controlled by geological factors such as discernible channel microfacies(heart beach and side beach),inversion structure,infiltration of uranium and oxygen-bearing water,underground oil and gas seepage and geochemical reduction barrier in the upper member Formation.The metallogenic ages of Hadatu uranium deposi were 66-30 Ma and 16-8 Ma respectively.

关键词

赛汉组上段/成矿作用/铀成矿特征/哈达图铀矿床/二连盆地

Key words

upper member of Saihan Formation/mineralization/uranium metallogenic characteristics:Hadatu uranium deposit/Erlian Basin

分类

天文与地球科学

引用本文复制引用

颜小波,吕永华,郭虎科,张锋..二连盆地哈达图铀矿床铀成矿特征分析[J].铀矿地质,2026,42(2):218-228,11.

基金项目

中国核工业地质局项目"内蒙古二连盆地及周边铀资源调查评价与勘查"(编号:202202)资助. (编号:202202)

铀矿地质

1000-0658

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