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松辽盆地中-新生代构造-沉积演化及其对铀成矿地控制作用

贾立城 李真真 黄笑 邢作昌 田明明

铀矿地质2024,Vol.40Issue(1):90-104,15.
铀矿地质2024,Vol.40Issue(1):90-104,15.DOI:10.3969/j.issn.1000-0658.2024.40.008

松辽盆地中-新生代构造-沉积演化及其对铀成矿地控制作用

Structural-sedimentary Evolution of Mesozoic-Cenozoic and Its Control on Uranium Mineralization in Songliao Basin

贾立城 1李真真 1黄笑 2邢作昌 1田明明1

作者信息

  • 1. 核工业北京地质研究院 中核集团铀资源勘查与评价技术重点实验室,北京 100029
  • 2. 核工业二四三大队,内蒙古 赤峰 024000
  • 折叠

摘要

Abstract

Songliao Basin is a large fault-depression composite sedimentary basin.The composite evolution and filling produced the favorable geological background and metallogenic conditions for uranium mineralization.The structure-filling characteristics of the basin was studied to deepen the understanding of uranium metallogenic mechanism.Based on the study of the structure-filling characteristics of Songliao Basin,this paper summarized the basin-forming dynamics,preliminarily recovered the shapes and features of prototype basin,and identified the structural-sedimentary evolution characteristics and cover types.The study result showed that the basin mainly experienced two stages of basin formation,the Early Cretaceous rift(fault-depression)and the Late Cretaceous depression,resulted in the formation of filling structure of the lower fault and the upper depression,and three sets of favorable formations of upper red and lower black vertically.The Meso-Cenozoic evolution of the basin can be divided into six stages,in which the Paleocene-Eocene(E1-E2)basin developed uplift and denudation under the background of compression,and the deep ore-forming fluid was exuded and reworked on the mineralization with large scale and compromised the main ore-forming period of the basin.

关键词

松辽盆地/构造演化/沉积建造/砂岩型铀矿

Key words

Songliao Basin/structural evolution/sedimentary formation/sandstone-type uranium deposit

分类

天文与地球科学

引用本文复制引用

贾立城,李真真,黄笑,邢作昌,田明明..松辽盆地中-新生代构造-沉积演化及其对铀成矿地控制作用[J].铀矿地质,2024,40(1):90-104,15.

基金项目

中核集团集中研发项目"砂岩型铀矿多重耦合地质成矿作用与时空定位"(编号:中核科发2021-143号)资助. (编号:中核科发2021-143号)

铀矿地质

OACSTPCD

1000-0658

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