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鄂尔多斯盆地西缘惠安堡地区构造地质及铀成矿特征

贾恒 李保侠 荆国强

铀矿地质2012,Vol.28Issue(3):148-151,186,5.
铀矿地质2012,Vol.28Issue(3):148-151,186,5.DOI:10.3969/j.issn.1000-0658.2012.03.004

鄂尔多斯盆地西缘惠安堡地区构造地质及铀成矿特征

Structural Geology and Mineralization of Uranium Deposits in the Huianpu Area, West of Ordos Basin

贾恒 1李保侠 1荆国强1

作者信息

  • 1. 核工业203研究所,陕西咸阳712000
  • 折叠

摘要

Abstract

In the geological investigation of some medium level waste disposal site, environmental isotope and radioactive isotope were applied to study the seepage velocity and age of groundwater, and the connection between deep seated confined water and springs in the disposal site. In addition, the genesis and source of supply of deep seated confined water were also analyzed. Some related hydrogeological characteristics and parameters of the site had been obtained successfully.

关键词

西缘褶断带/逆冲推覆前缘带/早期古氧化/晚期氧化叠加成矿/鄂尔多斯盆地

Key words

hydrogeological characteristics/ isotopes groundwater seepage velocity/ age of groundwater/ water connection

分类

天文与地球科学

引用本文复制引用

贾恒,李保侠,荆国强..鄂尔多斯盆地西缘惠安堡地区构造地质及铀成矿特征[J].铀矿地质,2012,28(3):148-151,186,5.

铀矿地质

OACSCDCSTPCD

1000-0658

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