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塔里木盆地库车坳陷日达里克地区库车组下段沉积特征、后生蚀变及与铀成矿关系研究

吕俊维 袁忠 李书海 王元元 杨小强 孙飞 刘念

世界核地质科学2026,Vol.43Issue(2):277-294,18.
世界核地质科学2026,Vol.43Issue(2):277-294,18.DOI:10.3969/j.issn.1672-0636.2026.02.005

塔里木盆地库车坳陷日达里克地区库车组下段沉积特征、后生蚀变及与铀成矿关系研究

Study on the sedimentary and epigenetic alteration characteristics and relation to uranium mineralization in the lower member of Kuqa formation in Ridarik area,Kuqa depression of Tarim basin

吕俊维 1袁忠 1李书海 1王元元 1杨小强 1孙飞 1刘念2

作者信息

  • 1. 核工业二一六大队,新疆 乌鲁木齐 830011
  • 2. 铀资源探采与核遥感全国重点实验室,北京 100029||核工业北京地质研究院,北京 100029
  • 折叠

摘要

Abstract

Ridarik area in Kuqa depression,as an important case of urranium prospecting breakthrough of Neogene at the northern margin of Tarim basin,provided the basis for uranium exploration in Neogene of the whole Tarim basin.In order to better understand the sedimentary characteristics of the lower member of the Kuqa formation in the Ridarik area and the relationship between epigenetic alteration of sand bodies and uranium mineralization and establish a uranium metallogenic model to predict the favorable area.This paper systematically summarizes the characteristics of stratigraphic development in the study area,clarifies the internal relationship between uranium mineralization and sedimentary facies and epigenetic alteration through a large number of field investigations,borehole lithology observation and sample test results and comprehensive analysis.The results show that the fan delta front subfacies are mainly developed in the lower member of Kuqa formation in Ridarik area,and the ore bodies are located in the changing parts of sand body from thick to thin and argillaceous barrier layers being more and thicker.The epigenetic alteration zoning in the area is more obvious,and the ore belt is mostly in the front edge of gray-white belt among the strong clay alteration,which is not easy to identify.Through the statistics analysis of geochemical data,the identification marks of gray-white belt were established,which provide reference for the subsequent exploration of Neogene sandstone-type uranium deposits in Tarim basin.

关键词

砂岩型铀矿/库车组下段/日达里克/库车坳陷/塔里木盆地

Key words

sandstone type uranium deposit/the lower member of the Kuqa group/Ridarik/Kuqa depression/Tarim basin

分类

天文与地球科学

引用本文复制引用

吕俊维,袁忠,李书海,王元元,杨小强,孙飞,刘念..塔里木盆地库车坳陷日达里克地区库车组下段沉积特征、后生蚀变及与铀成矿关系研究[J].世界核地质科学,2026,43(2):277-294,18.

基金项目

中国核工业地质局铀矿地质项目"新疆塔里木盆地北缘温宿-拜城地区铀矿资源调查评价"和"新疆塔里木盆地库尔勒地区铀矿资源调查评价"(编号:202407-1、202507-3)联合资助 Supported jointly by Geological Exploration Project of China Nuclear Geology"Investigation and Assessment of Uranium Resources in the Wensu-Baicheng Area,Northern Tarim Basin,Xinjiang(No.202407-1)"and"Investigation and Assessment of Uranium Resources in the Korla Area,Tarim Basin,Xinjiang(No.202507-3)" (编号:202407-1、202507-3)

世界核地质科学

1672-0636

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