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鄂尔多斯盆地白土井地区环河组灰绿色砂岩成因分析

张字龙 陈乡 王凤岗 程纪星 任志勇 丁波 鲁超 贺锋 张艳

铀矿地质2026,Vol.42Issue(3):347-356,10.
铀矿地质2026,Vol.42Issue(3):347-356,10.DOI:10.3969/j.issn.1000-0658.2026.42.026

鄂尔多斯盆地白土井地区环河组灰绿色砂岩成因分析

Genetic Analysis of Gray-green Sandstone from Huanhe Formation of Baitujing Area,Ordos Basin

张字龙 1陈乡 2王凤岗 1程纪星 1任志勇 3丁波 1鲁超 3贺锋 1张艳1

作者信息

  • 1. 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
  • 2. 核工业北京化工冶金研究院,北京 101149
  • 3. 核工业二〇八大队,内蒙古 包头 014010
  • 折叠

摘要

Abstract

Huanhe Formation of Lower Cretaceous contains thick gray-green sandstones in Baitujing area of Ordos Basin.Studying their genesis is significant for identifying redox zoning and clarifying exploration directions for sandstone-type uranium deposits.This study used macroscopic core observations and scanning electron microscopy analyses to determine the causes of the gray-green coloration in the sandstones of the study area.The results show that the primary chromogenic mineral giving the sandstone its gray-green color is the chlorite,followed by chlorite-smectite mixed layers.Chlorite occurs in three forms:grain coatings,pore linings,and pore fillings,representing different formation stages in the sequence of grain coatings → pore linings → pore fillings.The green color in the sandstone is uniformly and continuously distributed without features of later alteration such as"red core with green edges,"and the edges of purplish-red mud clasts also show no signs of green alteration.The three forms of chlorite closely envelop detrital grains and develop around intergranular pores,with no evidence of iron oxide replacement.Based on sedimentary environment analysis,it was believed that this set of gray-green sandstones was formed in a weakly reducing underwater environment at the delta front,representing a primary sedimentary origin.Therefore,the gray-green sandstones in the study area collectively represent a original reducing zone,and the contact boundary on their western side with red or yellow sandstones can serve as the oxidation front.This recognition has practical significance for guiding uranium exploration in the region.

关键词

绿泥石/灰绿色砂岩/环河组/白土井地区/鄂尔多斯盆地

Key words

chlorite/gray-green sandstone/Huanhe Formation/Baitujing area/Ordos Basin

分类

天文与地球科学

引用本文复制引用

张字龙,陈乡,王凤岗,程纪星,任志勇,丁波,鲁超,贺锋,张艳..鄂尔多斯盆地白土井地区环河组灰绿色砂岩成因分析[J].铀矿地质,2026,42(3):347-356,10.

基金项目

国家重点研发计划项目(编号:2021YFC2902004) (编号:2021YFC2902004)

核工业地质局生产中科研项目(编号:202401-12、ZY2405) (编号:202401-12、ZY2405)

铀资源探采与核遥感全国重点实验室项目(编号:NKLUR-WDZC-2025-04、NKLUR-2024-ZD-001) (编号:NKLUR-WDZC-2025-04、NKLUR-2024-ZD-001)

中核集团青年英才项目(编号:地QNYC2503)联合资助. (编号:地QNYC2503)

铀矿地质

1000-0658

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