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中国北东部铀矿化与大地构造活动及演化的关系

王木清

铀矿地质2013,Vol.29Issue(4):193-198,207,7.
铀矿地质2013,Vol.29Issue(4):193-198,207,7.DOI:10.3969/j.issn.1000-0658.2013.04.001

中国北东部铀矿化与大地构造活动及演化的关系

Uranium Mineralization in Northeast China and Its Relation with Tectonic Evolution

王木清1

作者信息

  • 1. 核工业北京地质研究院,北京100029
  • 折叠

摘要

Abstract

Located in the intersection of Eurasian and rim pacific metallogenic belt,Northeast China is favorable for uranium-poly-metall mineralization.The mineralization have been developed in the folding stage of Precambrian basement and Paleozoic geosyncline sediments,reactivation stage of folded basement and Diwa stage.The mineralization is of long time and with various types and produced 4 industrial types.Meso-ceno zoic magmatism,especially the vocalism was well developed in Northeast China,and correspondingly,hydrothermal dominated uranium mineralization,especially vocalism related mineralization was formed in the area with important significance.

关键词

地洼/构造活化/铀矿化/铀源层(体)

Key words

Diwa/ tectonic activation/ uranium mineralization/ source rocks of uranium

分类

天文与地球科学

引用本文复制引用

王木清..中国北东部铀矿化与大地构造活动及演化的关系[J].铀矿地质,2013,29(4):193-198,207,7.

铀矿地质

OACSCD

1000-0658

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